title: Vary Peri

text:
Vary Peri (), also called Sweets Fairy or Magical Wizard Cake Fairy is a 2012 Korean-Chinese Cel Shaded 3D animated series based on character created by InfinityOne Comics Entertainment, animated by Alpha Group Company in China & CJ E&M in South Korea. It was produced by Anthony Chen, directed by Han Feng and written by Lu Lingyi, Wang Wei and Ming Riye. It first aired on the Chinese channel Golden Eagle Television and the Cable channel JiaJia Kids from 10 November 2012 to 18 February 2013 with a total of 40 Episodes.

Vary Peri is officially based on the toys of the same name which utilizes a pop-up function when pressed. The overall theme of the series is Desserts and Sweets, as shown to the main characters and the setting. The series is very notable for copying various concepts from Spin Master and Sega Sammy Holdings's toy franchise Zoobles, particularly the Japanese/Korean Version.

Story
The Sweetsheart Kingdom () is a magical world filled with various sweets and pastries, inhabited by animal people who are good patisseries and cooks experting on each dessert. The kingdom's only Princess, Mousse Bibi is soon going to ascend to the throne as the new Queen, however all she cared on her life is to taste various kinds of cakes and sweets. One day, Lyan, her royal adviser, set up a plan by making her suffer Ageusia. As she is shocked that she can no longer taste anything, he told her that the only way to cure her condition is to search for the legendary magic called Delicious Miracle (). She immediately left the castle and venture outside, not knowing to her that Lyan is doing this to eradicate her.

Upon her arrival at the town called Cake Village (), she first met a denizen of the village named Mocha Dennis, who is very obsessed on his looks. Though the meeting between both him and Bibi is unsettling. She is also unaware that she possesses a hidden potential that would help her search for the legendary magic and be the key on changing the fate of the Sweetsheart Kingdom once and for all!

Characters

Cake Fairies
Mousse Bibi ()
Voiced by: Deng Hong
A Female Strawberry Mousse Cake Rabbit, Mousse Bibi is the Princess of the Sweetsheart Kingdom. She is very dimwitted yet kindhearted girl who likes to think big and has a playful and lively personality. Bibi also loves to eat sweets and watch anime, and she is very good on making tea but is very bad on baking. She rarely gets along with Mocha Dennis, though in the end she finally appreciates him as a friend. Her star sign is Gemini.

Bibi is supposed to ascend to the throne and become Queen until Lyan decided to make her suffer Aguesia, forcing her to go to the Cake Village to search for the Delicious Miracle, the only magic that can cure her. She also possess an unusual ability when she eats a dessert that is blessed with the Delicious Miracle, allowing her to transform into her Fairy Form in order to do purification magic. She is also the first person to unlock her Cake Fairy abilities. By the end of the series, she finally became Queen after her sense of taste returned.

Mocha Dennis ()
Voiced by: Liu Pei
A Male Mocha Cupcake Bear (Although his design is similar to a panda), Mocha Dennis is Bibi's first friend she met in the Cake Village and the cousin of Parfait Chacha. He cares a lot about his image and is a neat freak, usually does things in a leisurely way. He is also very strong willed though has a fear on bugs. Dennis is an expert patisserie and usually teaches Bibi how to bake properly. He rarely gets along with Bibi though he starts to develop some feelings to her. His star sign is Libra.

He first met Bibi at episode 1 alongside Parfait Chacha, though the meeting is very unexpected for the both of them. is the second person to unlock his Cake Fairy abilities in episode 3. He is also in suspicion regarding Lyan's action until he found out his true motives.

Vanilla Ellie ()
Voiced by: Liao Chunyu
A Female Vanilla Mille Crepe Cake Sheep, Vanilla Ellie is Bibi's best friend in Cake Village. She is weakly willed, but she is also has a romantic personality and is a very nice girl. Ellie also loves reading the Horoscope and usually makes stuffed animals (though they look a bit bad, Bibi loves them). Her star sign is Virgo.

Bibi met her at episode 3 and first thought she's a monster all thanks to Angel spreading false rumors about her. After a while, the two reconcile and got along well as they both became best friends. She is the fifth person to unlock her Cake Fairy abilities.

Blueberry Angel ()
Voiced by: Zhao Na
A Female Blueberry Cupcake Peacock, Blueberry Angel is the owner and manager of the pastry shop "Blue Berry". She is very proud, smart, always bossy regarding her work and also a bit of tomboyish due her attitude. Angel can be a bit cold-hearted and strict sometimes, usually has a huge ambition to become the best patisserie in the Sweetsheart Kingdom. She bakes cakes as a hobby, often some of them are blessed with Delicious Miracle, and treats Tia as her best friend. She also admires Lyne due to his baking skills until the reveal and she is allergic to grass pollen. Her star sign is Capricorn.

She and Tia first met Bibi at Episode 1, mistaking her as a thief who wants to take away one of her decorated masterpiece. Angel also witnessed Bibi's fairy form for the first time, thinking she is a monster and became cold to her. She then become friends with her in Episode 4. Angel is the third person to unlock her Cake Fairy abilities.

Orange Tia ()
Voiced by: Zu Liqing
A Female Orange Pudding Cake Deer Fawn, Orange Tia is Angel's close friend. She is very studious and usually more mature than the others, though she can have a very sharp tongue. She is also very calm and is very prepared on some situations and loves to read a lot of books, often being called a nerd sometimes. When she's stuck in a situation, she comes up with ideas. Tia is also a very good specialist on desserts and worked with Angel together in some of their creations. She owns an heirloom crown at her house and has a cousin named Niva, a very mischievous cat. Her star sign is Scorpio.

She and Angel first met Bibi at Episode 1, thinking she's a thief who wants to take away one of Angel's decorated masterpiece. Tia also witnessed Bibi's fairy form for the first time, and knew that she has hidden abilities that she can discover. Tia is the seventh person to unlock her Cake Fairy abilities.

Parfait Chacha ()
Voiced by: Li Jing
A Female Green Tea Cake Dog, Parfait Chacha is a noblewoman living in the Cake Village and also Mocha Dennis's cousin. She is a very playful girl who is very spoiled on things, especially her engagement with Dennis. She is also very haughty, ambitious and really motivated in which she will do everything to get Dennis's attention. She also hates Bibi due to the fact he focuses on her more than she does, but later in the final episode, they became friends. Her star sign is Pisces.

She first met Bibi at episode 1 alongside Dennis, though the meeting between him and Bibi broke her heart. After Episode 34, her parents went bankrupt and decided to move away from Cake Village, leaving her behind. She now currently lives with Peach, working for a living. She is the sixth person to unlock her Cake Fairy abilities.

Strawberry Jessie ()
Voiced by: Li Jing
A Female Strawberry Pudding Cake Hen Chick, Strawtberry Jessie is an herbalist living in the outskirts of Cake Village. She is very timid, shy and laid back, usually living alone before she met Bibi. Jessie is also dislikes both Durians and Lightning but has a liking on egg rolls. Her star sign is Aquarius.

Bibi first met her in Episode 5 and befriended her despite her being an outcast. Later on, she and her friends learned that she is the guardian of the Vanilla Valley, which is a place filled with various kinds of herbs. Her ancestors and family guarded the valley for centuries before she's given the task. She is the fourth person to unlock her Cake Fairy abilities.

Tiramisu Cavan ()
Voiced by: Zhao Ran
A Male Tiramisu Penguin, Tiramisu Cavan is Cake Village's genius gadgeteer. He is a very nice person who usually focuses on inventing things and likes to study mechanical things. He has bad eyesight and usually rely on his glasses to see. Cavan usually gets along with Tia but he is best friends with Peach. His star sign is Taurus.

Bibi and her friends first met him at Episode 14, who is building several theme park rides for everyone in Cake Village. His dream is to build a "Dream Paradise" for everyone. He is the ninth person to unlock his Cake Fairy abilities.

Honey Peach ()
Voiced by: Li Jing
A Female Honey Cake Bee, Honey Peach is the village's resident honey expert. She is very workaholic, kind to people, and a tomboy, where she raises them to make honey. She is also very caring to small animals and hates to see her prized honey bees to get hurt. She is best friends with Tiramisu Cavan and share a relationship together. Her star sign is Sagittarius.

Bibi first met her in Episode 16 and she and Cavan became best friends in Episode 17. She is the eight person to unlock her Cake Fairy abilities.

Ice Cream Sarah ()
Voiced by: Zu Liqing
A Female Ice Cream Cake Panda, Ice Cream Sara is a newcomer in the Cake Village who specializes on dried fruits. She is very full of enthusiasm and is optimistic and passionate on her work, especially her job but she can get a little homesick. On her first appearance, she makes friends with Bibi and later with the rest of the crew. Her star sign is Leo.

Bibi first met her in Episode 21 as she found out she arrived in Cake Village, mistaken it for her hometown: the Ice Cream Village. Lyne found out about this and used this to his schemes but failed. She is the last person to unlock her Cake Fairy abilities.

Side Characters
Chief Nicolas ()
Voiced by: Zhao Ran
A Male King Chef Elephant and the Mayor of the Cake Village, he always appears through a hot air balloon to greet Bibi and her friends.

Crepe Gugu ()
Voiced by: Zhao Na
A Female Orange Cream Puff dog, Crepe Gugu is the twin sister of Vanilla Gigi as well as Chacha's assistants. She usually behave nicely in front of Chacha though often the two argue sometimes. Usually the two always agrees on Chacha's ideas and always go for them.

Vanilla Gigi ()
Voiced by: Liao Chunyu
A Female Vanilla Cream Puff dog, Vanilla Gigi is the twin sister of Crepe Gugu as well as Chacha's assistants. She usually behave nicely in front of Chacha though often the two argue sometimes. Usually the two always agrees on Chacha's ideas and always go for them.

Cherry Dandan ()
Voiced by: Deng Hong
A young female Cherry Cake squirrel, Cherry Dandan is the best friend of both Gugu and Gigi. She usually tags along both of them and likes to play with the two sisters.

Aunt Anna ()
Voiced by: Liao Chunyu
A Female Orange Herb Tea dog, she is Parfait Chacha's mother. She is very well dressed, and she and her husband tend to be very anxious for their daughter's well-being, but especially her.

Uncle Jeff ()
Voiced by: Liu Pei
A Brown Herb Tea dog who is Parfait ChaCha's father.

Niva ()
Voiced by: Zhao Na
A Female Strawberry cat, Niva is Tia's cousin. She is very mischievous thought sometimes well behaved.

Antagonists
Lyan ()
Voiced by: Zhao Ran
A male Bagel lion, Lyan is Mousse Bibi's royal adviser and the series's main antagonist. He is nice and very supportive, however he has a very dark and evil side and will do anything to eradicate the Princess. On his stay in the Cake Village, he wears his special disguise in order for the others not to recognize him. His star sign is Aries.

He is usually jealous when he first heard Bibi is gonna ascend to the throne and wants it for himself. Because of this, he made a cake that would make her suffer Ageusia and the one telling her to search for the Delicious Miracle for his personal goal. However, in the finale, he finally changed his ways after Bibi talked to him.

Episodes
There were 40 episodes in total, running from 12 November 2012 - 13 February 2013.

 Welcome to the Sweetsheart Kingdom!
 The Big Bake-off
 When Bibi met Ellie
 When Bibi and Angel were Rivals
 Jessie Comes to Visit
 A Trip to Vanilla Valley
 Ellie in Distress
 Cake Fairies at Sea
 Firefly Follies
 Double Cousin
 Down on the Sweetsheart Farm
 Chacha's Big Diet
 Ellie and the Little Blackbird
 Dr. Cavan the Smart Cookie
 Beatin' the Heat
 A Buzzy Day at the Cake Village
 Peach and Cavan Save the Day
 A Taste of Christmas
 The Lucky Color Cake
 I've Been Toothached!
 Sarah the Little Ice Cream Panda
 A Frutti Tutti Adventure
 Ellie's Unlucky Fortune
 A Secret Recipe Revealed
 Niva: Tia's Little Cousin
 Birthday Bashers
 Dennis' (Not so) Ordinary Day
 Gugu and Gigi Hangout
 Jessie's the Most Important One
 Not your Ordinary Lyan! (part 1)
 Not your Ordinary Lyan! (part 2)
 Ambassador Bibi
 A Piece of Problem Pie
 Chacha the Little Beekeeper
 Hypno Style
 The Lost Time Capsule
 A Catastrophe at the Cake Village
 The Search for the Light of Hope
 The Big and Magical Sweetsheart Kingdom Cake
 It's Transformation Time!

See also
Zoobles

References

General
 https://web.archive.org/web/20121231221014/http://comic.letv.com/zt/cakesweet/index.shtml

Specific

External links
 Official Website

2012 Chinese television series debuts
2013 Chinese television series endings
2010s animated television series
Mandarin-language television shows
Cel-shaded animation
Chinese children's animated adventure television series
Chinese children's animated comedy television series
Computer-animated television series


title: Hochstein School of Music & Dance

text:
The Hochstein School (formerly Hochstein School of Music & Dance) is an all ages school of music and dance in Rochester, New York The school was founded in 1920.

History
David Hochstein was a world-renowned violinist from Rochester. When he was killed in World War I's Battle of Argonne in October 1918, elites such as George Eastman and Emily Sibley Watson joined with other citizens of Rochester in forming the "David Hochstein Music School Settlement". The school was chartered by the State of New York in 1920.

In 1976, Hochstein became the first non-degree granting school to be accredited by the National Association of Schools of Music.

Facilities
The school was originally opened in the Hochstein's family home on Joseph Avenue for 250 students. By 1928, the school had begun to outgrow this facility. Funds are raised by interested citizens for a new site to be constructed on 12 Hoeltzer Street.  The school remained here until 1975, when in need of more space, it is moved to the former Central Presbyterian Church on Plymouth Avenue. In 1978, the building was purchased for $1, "considered to be an appropriate fee in light of the long tradition of the importance of music in that house of worship."

Hochstein's Performance Hall is the former sanctuary of the Central Presbyterian Church and has been fully renovated as a theater. It hosts student performances as well as concerts from outside groups. Once a week, live concerts are broadcast from the Performance Hall as part of WXXO's "Live from Hochstein" concert series.

References

External links

1920 establishments in New York (state)
Dance in New York (state)
Dance schools in the United States
Education in Rochester, New York
Educational institutions established in 1920
Music of Rochester, New York
Music schools in New York (state)


title: Nokia 106

text:
Nokia 106 is a feature phone release on November 2013. Two more iteration were release in 2018 and 2023. Original model is discontinued.

Specification for the original Nokia 106 (2013)

It has FM (headset required) and a speaking clock. It does not support any connectivity option like GPRS, EDGE, or Bluetooth.

References

External links

Nokia official website (active) https://www.nokia.com/phones/en_int/nokia-106
Nokia official website (deprecated) http://www.nokia.com/global/products/phone/106/
GCMArena specification (active): https://www.gsmarena.com/nokia_106-5635.php

106
Mobile phones introduced in 2013
Mobile phones with user-replaceable battery


The 2010 Huntingdonshire District Council election took place on 6 May 2010 to elect members of Huntingdonshire District Council in Cambridgeshire, England. One third of the council was up for election and the Conservative Party stayed in overall control of the council.

After the election, the composition of the council was:
Conservative 37
Liberal Democrats 12
UK Independence Party 2
Independent 1

Background
After the last election in 2008 the Conservatives continued to run the council with 38 councillors, while the Liberal Democrats had 12 and there were 2 independents. However, in July 2009 the UK Independence Party won their first seat on the council after Peter Reeve won a by-election for Ramsey ward, taking the seat from the Liberal Democrats. He was then joined by the other Ramsey councillor, Andy Monk, who had been elected at another by-election in April 2009 as a Conservative, but defected to the UK Independence Party in January 2010.

Meanwhile, the Liberal Democrats gained a seat from the Conservatives in another by-election in Fenstanton in February 2010. These changes meant that going into the 2010 election there were 36 Conservative, 12 Liberal Democrat, 2 UK Independence Party and 2 independent councillors.

Election result
The Conservatives increased their majority on the council by 1 to have a majority of 22 seats on the council.

Ward results

References

2010 English local elections
May 2010 events in the United Kingdom
2010
2010s in Cambridgeshire


title: Feng Jifeng

text:
Feng Jifeng is a Chinese oncologist at Jiangsu Cancer Hospital and Nanjing Medical University, both located in Nanjing, China. He specializes in the diagnosis and treatment of malignant tumors such as lung cancer, breast cancer, and lymphoma. He has a special interest in aspects of biotherapy and the correlation between dosage of chemotherapeutics and their curative effect and toxicity.
He currently holds the following positions:
Director of national pharmaceutical clinical trial institute in Jiangsu Cancer Hospital
Chief physician of Jiangsu Cancer Hospital
Director of Quality Control Centre of Jiangsu Medical Oncology and Chinese Medical Association
Vice director of Chinese Society of Clinical Cancer Chemotherapy of Chinese Anti-Cancer Association
Editor-in-chief of the Journal of International Translational Medicine

References

Medical journal editors
Living people
Chinese oncologists
Year of birth missing (living people)
Place of birth missing (living people)
Writers from Nanjing
21st-century Chinese science writers
20th-century Chinese physicians
21st-century Chinese physicians
Physicians from Jiangsu


title: Margaret Qualley

text:
Sarah Margaret Qualley (born October 23, 1994) is an American actress. A daughter of actress Andie MacDowell, she trained as a ballerina in her youth. She made her acting debut in the 2013 drama film Palo Alto and gained recognition for her supporting role in the HBO drama series The Leftovers (2014–2017).

Qualley subsequently appeared in films such as The Nice Guys (2016), Death Note (2017), and Once Upon a Time in Hollywood (2019), and performed a voice role in the video game Death Stranding (2019). She received critical acclaim and nominations for the Primetime Emmy Award for playing Ann Reinking in the FX biographical miniseries Fosse/Verdon (2019) and the title role in the Netflix drama miniseries Maid (2021).

Early life and education
Sarah Margaret Qualley was born in Kalispell, Montana. She is the daughter of actress and model Andie MacDowell, and former model Paul Qualley. She has an older brother, Justin, and an older sister, actress and singer Rainey Qualley.

The Qualley siblings spent their early years on a ranch in Missoula, Montana, moving to Asheville, North Carolina, when Margaret was four. Qualley's parents separated when she was five years old, and she subsequently split her time equally between them. For many years, her parents lived just  apart. Her family home with MacDowell is in North Carolina, where they have extended family nearby.

As a teenager growing up in Asheville, North Carolina, she and her sister were both debutantes, and Qualley made her debut at the Bal des débutantes in Paris. She left home at 14 to board at the North Carolina School of the Arts, where she studied dance. She trained as a ballerina, earning an apprenticeship at the American Ballet Theatre and studying at New York's Professional Children's School. However, at the age of 16, following an offer to become an apprentice with the North Carolina Dance Theater company, Qualley decided to quit dance. In order to stay in New York, she began working as a model. Of this period, Qualley says: "I wrote to my mom saying: 'Look, I don't think I want to be a dancer any more so I'm going to quit ballet and stay here. I will have this and this income next week.' I laid it out in a way that she couldn't say no because I was so organized." Qualley later changed her focus to acting and attended London's Royal Academy of Dramatic Art summer program. Qualley attended New York University but left after a semester for acting roles.

Career

Modeling
In 2011, at age 16, Qualley made her modeling debut during New York Fashion Week, walking for Alberta Ferretti. She modeled during Paris Fashion Week Spring/Summer 2012 for Valentino and Chanel. She again walked for Chanel during their Fall/Winter 2012 show. Qualley has appeared on the covers and editorials of Evening Standard, Jolie, Teen Vogue, Paper, Elle, W, Hunger, Porter, Document Journal, AnOther, Interview, Vogue (including Vogue Russia and China), Vanity Fair, Nylon, V, The Cut, and C. She has appeared in advertising campaigns for Kenzo, Ralph Lauren, Kate Spade, and Celine. Qualley has also appeared in numerous campaigns for Chanel, for which is she is a house ambassador.

Acting

Qualley first appeared on screen in 2013 playing a small part in Gia Coppola's film Palo Alto. She received the part because she happened to be on set visiting her then-boyfriend, Nat Wolff. In June 2013, Qualley was cast as a series regular in the HBO television series The Leftovers. Qualley reprised her role as Jill Garvey for the subsequent second and third seasons of the HBO drama series The Leftovers in 2015 and 2017, respectively. In 2015, Qualley appeared in the short promotional film L'Américaine for American fashion label Tory Burch. In 2016, Qualley appeared as the central character in a Spike Jonze-directed commercial for KENZO World; choreographed by Ryan Heffington, Qualley improvised much of the dance routine using her training in classical ballet. Qualley next appeared in Shane Black's 2016 comedy The Nice Guys starring Ryan Gosling and Russell Crowe.

In April 2016, Qualley was announced to have joined the cast of Shawn Christensen's The Vanishing of Sidney Hall. Qualley and her sister Rainey appeared in the music video for Soko's 2017 single "Sweet Sound of Ignorance". The film premiered at the 2017 Sundance Film Festival, alongside another film of hers, Novitiate. In Novitiate, Qualley stars as Sister Cathleen, a young woman who begins to question her faith as she trains to be a nun. The film was released on October 27, 2017. That same year, Qualley starred in Death Note, directed by Adam Wingard.

In 2018, Qualley appeared in Donnybrook, directed by Tim Sutton and co-starring Jamie Bell and Frank Grillo. The film had its premiere at the 2018 Toronto International Film Festival. In 2019, Qualley starred in the Netflix science-fiction film IO. The film was directed by Jonathan Helpert and it was released on January 18, 2019. She played Sam Walden, a teenager surviving as one of the last people on an abandoned post-cataclysmic Earth, who is racing to find a cure for her poisoned home world before the last shuttle off the planet to the distant human space colony leaves her stranded.

Also in 2019, Qualley portrayed the role of Mary Dalton in Rashid Johnson's HBO adaption of Native Son. In 2019, Qualley also portrayed actress and dancer Ann Reinking in the FX miniseries Fosse/Verdon, for which she received nominations for a Primetime Emmy Award for Outstanding Supporting Actress in a Limited Series or Movie and a Critics' Choice Television Award for Best Supporting Actress in a Movie/Miniseries. She then appeared in Quentin Tarantino's epic comedy-drama film Once Upon a Time in Hollywood (2019), playing a member of the Manson Family named Pussycat. For the film, Qualley was nominated along with the rest of the cast for a Screen Actors Guild Award for Outstanding Performance by a Cast in a Motion Picture.

She also starred in Seberg (2019) opposite Kristen Stewart and Jack O'Connell. directed by Benedict Andrews.  On May 29, 2019, it was revealed that Qualley would be playing "Mama" in Hideo Kojima's PlayStation 4 game Death Stranding. She also played the character of Lockne, Mama's twin sister, in the game. In 2020, Qualley starred in Wake Up, a short film directed by Olivia Wilde, and in the feature My Salinger Year, opposite Sigourney Weaver and directed by Philippe Falardeau, which had its world premiere at the Berlin International Film Festival in February 2020. In 2021, Qualley starred in the miniseries Maid based upon Stephanie Land's memoir for Netflix. For her performance she received nominations for the Golden Globe Award for Best Actress – Miniseries or Television Film and the Screen Actors Guild Award for Outstanding Performance by a Female Actor in a Miniseries or Television Movie.

Qualley starred in psychological thriller A Head Full of Ghosts directed by Scott Cooper; and in Stars at Noon (2022) opposite Joe Alwyn directed by Claire Denis. In 2023 she executive produced and starred in the erotic thriller Sanctuary opposite Christopher Abbott.

She is set to star in the Yorgos Lanthimos directed surrealist fantasy film Poor Things starring Emma Stone and Mark Ruffalo which will premiere at the Venice International Film Festival. She also acted in Ethan Coen's comedy road film Drive-Away Dolls alongside Geraldine Viswanathan which will be released in February 2024.

Personal life
As of November 2019, Qualley lives in New York. Qualley formerly lived in Los Angeles with her sister Rainey, with whom she shares a dog named Books. Qualley describes her sister as "my idol, my best friend in the whole world".

Qualley was briefly romantically linked to Pete Davidson in 2019. She began dating actor Shia LaBeouf in 2020 after they co-starred in Rainey's music video "Love Me Like You Hate Me". Qualley and LaBeouf's relationship ended in January 2021 following controversies surrounding LaBeouf, including his ex-girlfriend and singer FKA Twigs's lawsuit against him for sexual battery and assault. In September 2021, Qualley told Harper's Bazaar that she believed FKA Twigs's allegations. In May 2022, Qualley announced her engagement to musician Jack Antonoff. They married on August 19, 2023 in a restaurant in Beach Haven, New Jersey, where Antonoff spent time as a kid.

Qualley is the subject of the 2023 song "Margaret" by Lana Del Rey from her album Did You Know That There's a Tunnel Under Ocean Blvd. She speaks on the track "Taco Truck x VB" from the same album.

Filmography

Film

Television

Video games

Music videos

Short videos

Awards and nominations

References

External links

1994 births
21st-century American actresses
Actresses from North Carolina
Actresses from Montana
American film actresses
American female dancers
American dancers
American television actresses
Debutantes of le Bal des débutantes
Living people
Female models from Montana
Female models from North Carolina
New York University alumni
People from Asheville, North Carolina
Place of birth missing (living people)
IMG Models models
American people of English descent
American people of French descent
American people of Irish descent
American people of Scottish descent
American people of Welsh descent


title: Masters W35 high jump world record progression

text:
This is the progression of world record improvements of the high jump W35 division of Masters athletics.

Key

References

Masters Athletics High Jump list

Masters athletics world record progressions
High jump


title: Masters W40 high jump world record progression

text:
This is the progression of world record improvements of the high jump W40 division of Masters athletics.

Key

References

Masters Athletics High Jump list

Masters athletics world record progressions
High jump


title: Masters W45 high jump world record progression

text:
This is the progression of world record improvements of the high jump W45 division of Masters athletics.

Key

References

Masters Athletics High Jump list

Masters athletics world record progressions
High jump


title: C. S. Fondy a.s.

text:
C.S. Fondy a.s. comprises three mutual funds that were previously managed by CS Fund, Inc., an investment company: namely, the C.S. Capital Gains Fund, the C.S. Energetics Fund, and the C.S. Regular Dividend Fund. Since 1998, the Funds have been managed by AKRO Investment Company, Inc. under the names AKRO Progressive Companies Fund, AKRO Global Equities Fund and AKRO Balanced Fund.

C. S. Funds management
Until February 1997, C. S. Funds were managed by the C. S. Fund, Inc., an investment company controlled by a larger number of investors associated with the so-called Motoinvest group.

After the receivership of Agrobanka in September 1996, the group decided to urgently sell off all their assets and leave the market; in the context the owners of the C. S. Fund, Inc. decided to sell the company as well. This occurred in February 1997 when the C. S. Fund, Inc. was sold to a Cyprus-based company Austell Enterprises Ltd. Two changes of owners followed: Austell sold S. C. Fund, Inc. to a Czech company Crassus, Ltd. who later sold it to a Russian company Kos-Mos. The new management of C. S. Fund, Inc., appointed by the Russian owner, then stripped C. S. Funds of its assets.

Subsequently, the management of C. S. Funds was transferred to AKRO Investment Company by decision of the Ministry of Finance, which manages it up to now.

C. S. Funds assets stripping
C. S. funds were stripped of their assets shortly after the C. S. Fund, Inc. came into the possession of Russian company Kos-Mos. C.S. Funds were taken over in a state where the majority of their assets were in bank accounts of the individual C. S. Funds in the form of cash due to the anticipated opening of the fund and expectations of equity markets decline.

The Board of Directors, shareholders and fund management learned about the changing of the owner on March 3, 1997, when Prague notary Robert Hochman certified Moscow's KosMos, Ltd. as the new owner of C. S. Funds, represented by Nikolai Trofimov.

Company representatives of KosMos Ltd. had the same notary register three Czech citizens as the new statutory representative of the C. S. Funds. One of them, at that time, twenty one years old, unemployed young man Vaclav Franta from Chrastava near Liberec got the right to sign a power of attorney to carry out transactions of the company. Later that day he took full advantage of it: he came to a Pilsen bank where the money of the funds was deposited and demonstrated his newly acquired power of attorney from representatives of KosMos Ltd. and instructed to transfer 1.23 billion CZK, which were the entire assets of C. S. Funds, on behalf of the British Swirlglen Ltd to purchase virtually worthless shares of the company Poultry Příšovice, which even were not publicly traded.

The money traveled through the brokerage company Umana (the trade was mediated by Umana brokers Josef Matoulek and Vladislav Naď) to Prague bank Girocredit to an account of the company Swirlglen. From there they were supposed to be transferred abroad. Girocredit considered the operation to be so suspicious that they asked for an investigation by the Financial Analytical Department of the Ministry of Finance (FAÚ MF), which alone had the right to suspend the transfers.

However, the director of FAÚ MF Jiří Kudlík allowed the transfer of the money abroad on March 11, 1997 after being visited by two representatives of the company Swirlglen.[12] Thus on March 12, 1997 virtually all of the property of C.S. Funds definitely disappeared in accounts in Switzerland, Liechtenstein, Gibraltar and USA.

Investigation and its results
The shareholders of C.S. Funds were not content with the loss of their money and made a series of compensation claims. In January 2001, a judge of the Municipal Court in Prague Hana Hubáčková adjudged sentences ranging from 5 to 10 years over the four men involved in the billions being stolen from the C.S. Funds. However, in September 2003, a judge of the High Court in Prague Pavel Zelenka returned the case to the Municipal Court with the requirement of evidence completion. His main complaint was that the Municipal Court used as evidence Russian interrogation of Trofimov, which the advocates of the defendants were not allowed to participate in.

In March 2002, the clients of C. S. Funds won the dispute with the Pilsen bank which, as a depository for the funds, was not supposed to carry out the suspicious transaction.

Since mid 1999, the executives of Crassus company, Petr Müller and Jaromír Florián, were prosecuted because by a few financial transactions they created worthless shares of Poultry Příšovice a.s., which were sold to KosMos, Ltd. for more than a billion CZK.

At the end of February 2003, an important verdict in the case of C. S. Funds stripping of assets was made. Judge of the District Court for Prague 4 Hronová decided that the Treasury must compensate one of the shareholders of the C. S. Funds, Zdeňek Řepka from Hradce Králové, 88k CZK plus the cost of the legal proceedings. The verdict meant good news primarily for the other C. S. Funds shareholders. It was in fact the first ever compensation controversy which the Treasury lost.

In October 2007, the police suggested to the prosecutors that Pavel Tykač should be accused of the stripping of assets of C.S. Funds as well. Tykač was allowed a retrial in early 2013. This was suggested by the Chief Public Prosecutor's Office in Prague in 2012 based on the allegations of businessman Frantisek Bušek (formerly Chobota) and his companions Klaus Schimmelpfennig and Oscar Gerlach that Tykač was responsible for the C. S. Funds stripping of assets. They submitted the minutes of an alleged meeting in Kufstein, Austria, where they were supposed to be negotiating the division of the stolen money. The argument of these people was extremely challenged when the presented minutes of the alleged meeting proved to be clearly forged. According to forensic experts, the creator of the minutes, which were supposed to be created in 1997, used Calibri font which was created a few years later (designed in 2003 and expanded for every day use in 2007), which clearly indicates the very antedating of the record. They themselves refused to testify either out of fear of being prosecuted, or as witnesses they testified to something else, when according to the evidence the C. S. Funds money ended up in the accounts of persons other than Pavel Tykač.

Tykač himself stated from the beginning that already in 2011 Bušek blackmailed him that if he did not pay 500mil CZK, he would produce evidence against him and accuse him of C. S. Funds assets stripping. The statement was not proven to be true yet but the fact is that the renewed prosecution Tykač was accompanied by a number of other substandard conditions and steps which have become the subject of discussion in professional circles and also drew attention to the systemic weaknesses of the monitoring activity of the prosecutors (in this case the prosecutor repeatedly disregarded the binding findings of the High and Supreme court). The prosecutor's office eventually stopped the prosecuting of Tykač in December 2015 after nearly three years of renewed investigation.

Another person talked about in connection with C. S. Funds assets stripping at least since 2004, but never accused of it, is the controversial financier Petr Sisák. His former girlfriend Lucie Lunde (formerly Václavíková) and also the sentenced Josef Matoulek pointed out Sisák and people surrounding him. Demonstrably the people from his surroundings were connected with the case: Sisák's father-in-law Jaromír Florián (at the time the executive director and shareholder of Crassus, Ltd., which sold the C.S. Funds to the Russian KosMos) or Sisák's longtime collaborator Peter Müller (along with Jaromír Florián he was the Managing Director and Shareholder of Crassus. Previously, he was involved, among other things, with Sisák's wife Věra and his father-in-law Florián in the first Silesian capital company, which among other things has previously owned a significant stake in poultry plants Příšovice, factual predecessors of Poultry Příšovice). The convicted in the case Matoulek described Sisák with Florián and Vasil Mohorita, Florián's half-brother and former chairman of SSM, as the main masterminds behind the C. S. Funds assets stripping.

Finally, the already mentioned Bušek, Schimmelpfennig and Gerlach or their collaborator Gunnar Kühn, the former CEO of Swirlglen, via which the stolen money traveled abroad, were never accused in this case even though they admitted the participation in the fraud.

Compensation
The forced Administrator of C. S. Funds with the help of hired lawyers and detective agencies managed to track down a significant part of the stolen money and get about 200mil CZK back. AKRO received another 650mil for the funds from the sale of compensation claims against the Pilsen bank.

In 2012, AKRO recovered an additional amount of almost 2.1 billion CZK in compensation for damage from the state. The verdict was subsequently overturned by the Supreme Court, but since in the meantime the state had already paid the compensation amount to AKRO and AKRO refused to return the amount paid, the state currently seeks return of the money by legal actions arising from unjust enrichment. In case the lawsuit ended in favor of AKRO and AKRO would not be required to return the money, the acquired amount for the damage compensation, of which a considerable part consists of high interest rates, would reach 2.9 billion CZK. Thus it would significantly exceeded the original amount of the caused damage. The whole affair can paradoxically end very favourably for the shareholders of former C. S. Funds.

References

Financial services companies of the Czech Republic
1991 establishments in Czechoslovakia


title: Masters W50 high jump world record progression

text:
This is the progression of world record improvements of the high jump W50 division of Masters athletics.

Key

References

Masters Athletics High Jump list

Masters athletics world record progressions
High jump


title: Masters W55 high jump world record progression

text:
This is the progression of world record improvements of the high jump W55 division of Masters athletics.

Key

References

Masters Athletics High Jump list

Masters athletics world record progressions
High


title: San Angelo Group

text:
The San Angelo Group is a geologic group in Texas. It preserves fossils dating back to the Permian period.

See also

 List of fossiliferous stratigraphic units in Texas
 Paleontology in Texas

References

Geologic groups of Texas
Permian System of North America


title: Masters W60 high jump world record progression

text:
This is the progression of world record improvements of the high jump W60 division of Masters athletics. Also see Masters women high jump world record progression.

Key

References

Masters Athletics High Jump list

Masters athletics world record progressions
High


title: Masters W65 high jump world record progression

text:
This is the progression of world record improvements of the high jump W65 division of Masters athletics.

Key

References

Masters Athletics High Jump list

Masters athletics world record progressions
High


title: Wolfe City Group

text:
The Wolfe City Group is a geologic group in Texas. It preserves fossils dating back to the Cretaceous period.

See also

 List of fossiliferous stratigraphic units in Texas
 Paleontology in Texas

References

Geologic groups of Texas
Cretaceous System of North America


title: 1920 LSU Tigers football team

text:
The 1920 LSU Tigers football team represented Louisiana State University (LSU) in the 1920 college football season.

Schedule

References

LSU
LSU Tigers football seasons
LSU Tigers football


title: Glen Rose Group

text:
The Glen Rose Group is a geologic group in Texas. It preserves fossils dating back to the Cretaceous period.

See also

 List of fossiliferous stratigraphic units in Texas
 Paleontology in Texas

References

Geologic groups of Texas
Cretaceous System of North America


title: Tornillo Group

text:
The Tornillo Group is a geologic group in Texas. It contains fossils dating back to the Cretaceous period.

See also

 List of fossiliferous stratigraphic units in Texas
 Paleontology in Texas

References

Geologic groups of Texas
Cretaceous System of North America


title: Port of Galveston immigration

text:
The immigrant inspection station at the Port of Galveston, in Galveston, Texas, was the gateway for tens of thousands of immigrants to the Southwest of the United States. Galveston was one of the largest cities in Texas until the hurricane of 1900 devastated the city

The Galveston station opened in 1906. Although not as familiar as Ellis Island, Galveston is known for an influx of Jewish immigrants from Europe during this period, the Galveston Movement. Immigrants from all over the world entered the United States through Galveston, including Central and South America, Asia, and Europe.

The station in Galveston was built on  Pelican Island. “When the federal government replaced state administrations in processing immigrants at the turn of the century, efforts began to redirect the flow of immigration from the Northeast to Texas. Pelican Island became federal property, and the government constructed an immigration center and quarantine station there." Quarantine centers already existed at other stations as well, because of the idea that immigrants brought with them diseases that could spread to the American people. After an outbreak of yellow fever, the quarantine station on Pelican Island was set up to ensure the disease did not reach the US population. The quarantine center was based on the one at Ellis Island, but was not as large or efficient.

Although known as “The Ellis Island of the West”, Galveston processed fewer immigrants than Ellis Island, but was at one time one of the largest immigration stations in the west. "Between 1906 and 1914 nearly 50,000 immigrants arrived at Galveston, including Bohemians, Moravians, Galicians, Australians, Romanians, Swiss, English, Poles Italians, Dutch, and some 10,000 Jews."

Many were Jewish. Eventually, “between 1907 and 1914, approximately ten thousand Jews entered the United States through the port of Galveston, Texas.” There was a push for Jewish immigrants to enter the United States through Galveston rather than Ellis Island because “the vast majority of Jewish immigrants remained in the ghettos of New York“. A project of the Jewish Immigrants' Information Bureau, the London-based Jewish Territorial Organization, and Jewish philanthropists such as Jacob Schiff to stop the concentration of Jewish immigrants in the congested industrial cities of the northeastern United States landed them in Texas instead, and helped them to find  jobs in the west.

The Jewish population had concerns that anti-Semitism had led to rejections of Jewish immigrants at ports of entry, but Galveston immigration officials were no exception.

The immigration station was damaged by storms in 1915 and 1916. It was then moved to 21st Street. World War I greatly reduced the number of immigrants entering through the Port of Galveston. The center was eventually demolished in 1972. However, the impact of the Jewish immigrant population in the Southwest, was due in large part to the Galveston station.

See also
Galveston Movement

Footnotes

References
Adam Krout, Silent Travelers: Germs, Genes and the “Immigrant Menace” (New York: Harper Collins, 1994)
Bernard Marinbach, Galveston: Ellis Island of the West. (New York: State University of New York Press, 1983)
Diana J. Kleiner, "GALVESTON COUNTY," Handbook of Texas Online (http://www.tshaonline.org/handbook/online/articles/hcg02), accessed September 30, 2013. Published by the Texas State Historical Association.

History of Galveston, Texas
History of immigration to the United States
 Antisemitism in the United States
 United States immigration law
Jews and Judaism in Texas
Jews and Judaism in Galveston, Texas


title: Masters W70 high jump world record progression

text:
This is the progression of world record improvements of the high jump W70 division of Masters athletics.

Key

References

Masters Athletics High Jump list

Masters athletics world record progressions
High


title: Ellenburger Group

text:
The Ellenburger Group is a geologic group in Texas. It preserves fossils dating back to the Ordovician period.

See also

 List of fossiliferous stratigraphic units in Texas
 Paleontology in Texas

References

Geologic groups of Texas
Ordovician System of North America


title: Montoya Group

text:
The Montoya Group is a group of geologic formations in westernmost Texas and southern New Mexico. It preserves fossils dating back to the late Ordovician period.

Description
The group consists mostly of dolomite but with some limestone and a basal sandstone. The total thickness is about . The group overlies the El Paso Formation and is overlain by the Fusselman Formation or Percha Formation, with both contacts difficult to define in some exposure areas. Biostratigraphy of the group is consistent with deposition in the Cincinnatian.

The group is divided into the Cable Canyon Sandstone, Upham Dolomite, Aleman Formation, and Cutter Formation These are treated as members in most of southern New Mexico, where the Montoya is relatively thin and remains at formation rank.

The Cable Canyon Sandstone is present in the northern exposures of the group and lies unconformably on the El Paso Formation. In the southern exposures, the Cable Canyon Sandstone is not present and the Upham Dolomite has a thin basal quartz sandstone.

The bulk of the Upham Dolomite is skeletal packstone and grainstone arising from dolomitization of a crinoidal calcarenite. Hardgrounds are found throughout the unit.

The Aleman Formation has up to 70% chert, in the form of thin continuous beds of sponge spicules within calcisiltite beds or of diagenetic lenses of chert nodules within skeletal wackestone or packstone. The continuous chert beds appear to have been laid down in cool water, while the packstone was deposited in warmer water.

The Cutter Formation is mostly bioturbated tidal flat carbonate mudstone or dolomite.

The contact with the underlying El Paso Formation is an unconformity corresponding to a hiatus of about 30 million years. In the Franklin Mountains, the upper El Paso Formation shows pronounced karst weathering. In other locations, the contact is sharp.

The group is interpreted as having been deposited within 30 degrees of the equator on the subtidal zone of a passive continental margin during the transition to late Ordovician glaciation. The presence of abundant chert and phosphate minerals in the group is attributed to upwelling along the continental margin, possibly triggered by glaciation.

Fossils
The Cable Canyon Sandstone contains trace fossils (Skolithos). The Upham Formation is rich in fossils, including brachiopods, bryozoans, corals, crinoids, gastropods, nautiloids, and receptaculids. The gastropod Maclurites is particularly prominent. The Aleman Formation is dominated by brachiopods, with some gastropods and tentaculites but few crinoids or bryozoans. The Cutter Formation contains abundant thin packstone beds with numerous brachiopods, bryozoans, and crinoids.

Economic geology
The formation has the potential to be an important natural gas reservoir in southern New Mexico, using horizontal drilling with hydrofacturing, with successful drilling reported by 2004.

History of investigation
The name was first used by G.B. Richardson in 2008, who did not explain the origin of the name or designate a type section. The formation was promoted to group rank by Kelley and Silver in 1952, who divided the group into the Cable Canyon sandstone, Upham dolomite, Aleman formation, and Cutter formation in the Franklin Mountains, but the Montoya remains a formation in southern New Mexico, where its subunits are too thin to be mappable at the usual 1:24,000 scale.

See also

 List of fossiliferous stratigraphic units in Texas
 Paleontology in Texas

Footnotes

References

 Poole, F.G., Stewart, J.H., Palmer, A.R., Sandberg, C.A., Madrid, R.J., Ross, R.J., Jr., Hintze, L.F., Miller, M.M., and Wrucke, C.T., 1992, Latest Precambrian to latest Devonian time; development of a continental margin, Chapter 2, IN Burchfiel, B.C., Lipman, P.W., and Zoback, M.L., eds., The Cordilleran Orogen; conterminous United States: Geological Society of America, The Geology of North America, The Decade of North American Geology (DNAG), v. G-3, p. 9-56.

Geologic groups of Texas
Limestone formations of the United States
Ordovician System of North America


"When Yankee Doodle Learns to "Parlez Vous Français"" is a World War I song published by A.J. Stasny Music Co.  Based on estimates of sales, a performance of the song by Arthur Fields in 1918 was ranked #8 in the United States when it was featured on his Oh! Frenchy album, released by Victor. The lyrics playfully present American soldiers learning French so that they may flirt with women while in France.

The lyrics and cover art are in the public domain.

Composition
The song was published in 1917 by A.J. Stasny Music Co. in New York City. It features music by Ed Nelson and words by Will Hart.

Performances and commercial success

Anna Chandler, Julia Dika, and Lew Seymour performed the song and were highlighted on sheet music variants.

It was recorded by Arthur Fields.

The song appeared in the 1948 movie When My Baby Smiles at Me.

References

Bibliography
Nelson, Ed G., and Will Hart. When Yankee Doodle Learns to "Parlez Vous Français". New York: A.J. Stasny Music Co, 1917.

External links
WORLD WAR 1 SONGS AND AMERICAN PATRIOTIC MUSIC
When Yankee Doodle learns to parlez vous francais
Song MP3 and sheet music cover found at the Illinois Digital Archive

Songs about language
Songs of World War I
Songs about France
1917 songs


title: Masters W75 high jump world record progression

text:
This is the progression of world record improvements of the high jump W75 division of Masters athletics.

Key

References

Masters Athletics High Jump list

Masters athletics world record progressions


title: Dearborne Limestone

text:
The Dearborne Limestone is a geologic formation in Montana. It preserves fossils dating back to the Cambrian period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Limestone formations of the United States
Cambrian Montana


title: Meagher Formation

text:
The Meagher Formation is a geologic formation in Montana made up of limestone. It preserves fossils dating back to the Cambrian period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Cambrian Montana
Cambrian southern paleotropical deposits


title: Pagoda Formation

text:
The Pagoda Formation is a geologic formation in Montana. It preserves fossils dating back to the Cambrian period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Cambrian Montana
Cambrian southern paleotemperate deposits
Cambrian southern paleotropical deposits


title: Masters W80 high jump world record progression

text:
This is the progression of world record improvements of the high jump W80 division of Masters athletics.

Key

References

Masters athletics world record progressions
High


title: Pentagon Formation

text:
The Pentagon Formation is a geologic formation in Montana. It preserves fossils dating back to the Cambrian period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Cambrian Montana
Cambrian southern paleotropical deposits


title: Pilgrim Formation

text:
The Pilgrim Formation is a geologic formation in Montana. It preserves fossils dating back to the Cambrian period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Cambrian Montana
Cambrian southern paleotropical deposits


title: Snowy Range Formation

text:
The Snowy Range Formation is a geologic formation in Montana. It preserves fossils dating back to the Cambrian period. It contains characteristic flat pebble conglomerate which sometimes show distinctive red rims

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Cambrian Montana
Cambrian geology of Wyoming
Cambrian southern paleotropical deposits


title: Wolsey Shale

text:
The Wolsey Shale is a geologic formation in Montana. It preserves fossils dating back to the Cambrian period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Cambrian Montana
Cambrian southern paleotropical deposits


title: Listed buildings in Toft, Cheshire

text:
Toft is a civil parish in Cheshire East, England. It contains eight buildings that are recorded in the National Heritage List for England as designated listed buildings.  Of these, one is listed at Grade II*, the middle of the three grades, and the others are at Grade II.  The major building in the parish is Toft Hall; this, its stable block and a bridge on the approach road are listed.  The rest of the parish is rural, and the other listed buildings are houses, a church and a milepost.

Key

Buildings

References

Citations

Sources

Listed buildings in the Borough of Cheshire East
Lists of listed buildings in Cheshire


Visa requirements for East Timorese citizens are administrative entry restrictions by the authorities of other states placed on citizens of East Timor. As of 2 July 2019, East Timorese citizens had visa-free or visa on arrival access to 94 countries and territories, ranking the East Timorese passport 56th in terms of travel freedom according to the Henley Passport Index.

East Timor signed a mutual visa waiver agreement with the European Union on 26 May 2015.

Visa requirements map

Visa requirements

See also

 Visa policy of East Timor
 East Timorese passport
 Foreign relations of East Timor

References and Notes
References

Notes

East Timor
Foreign relations of East Timor


title: Allan Mountain Limestone

text:
The Allan Mountain Limestone is a geologic formation in Montana. It preserves fossils dating back to the Carboniferous period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Limestone formations of the United States
Carboniferous Montana
Carboniferous southern paleotropical deposits


title: Sappington Formation

text:
The Sappington Formation is a geologic formation in Montana. It preserves fossils dating back to the Carboniferous period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Carboniferous geology of Utah
Devonian southern paleotropical deposits
Carboniferous southern paleotropical deposits


title: Amsden Formation

text:
The Amsden Formation is a geologic formation in Montana. It preserves fossils dating back to the Carboniferous period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Carboniferous Montana
Carboniferous geology of Wyoming
Carboniferous southern paleotropical deposits


title: Big Snowy Formation

text:
The Big Snowy Formation is a geologic formation in Montana. It preserves fossils dating back to the Carboniferous period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Carboniferous Montana


title: Cameron Creek Formation

text:
The Cameron Creek Formation is a geologic formation in Montana. It preserves fossils dating back to the Carboniferous period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Carboniferous Montana


title: Castle Reef Dolomite

text:
The Castle Reef Dolomite is a geologic formation in Montana. It preserves fossils dating back to the Carboniferous period. Castle Reef is the type locality.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Carboniferous Montana


title: Heath Shale

text:
The Heath Shale is a geologic formation in Montana. It preserves fossils dating back to the Carboniferous period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Shale formations of the United States
Carboniferous Montana


title: Lodgepole Limestone

text:
The Lodgepole Limestone is a geologic formation in Montana, United States. It preserves fossils dating back to the Carboniferous period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Limestone formations of the United States
Carboniferous Idaho
Carboniferous Montana
Carboniferous geology of Utah
Carboniferous southern paleotropical deposits


title: Egyptian Hope Party

text:
The Egyptian Hope Party () is a political party in Egypt created by former members of the Constitution Party. The party plans to run in the 2015 Egyptian parliamentary election.

References

External links
Egyptian Hope Party website

Political parties in Egypt
Political parties established in 2014
2014 establishments in Egypt
Pragmatism


title: Benton Shale

text:
The Benton Shale (also Benton Formation or Benton Group) is a geologic formation name historically used in Montana, Wyoming, North Dakota, South Dakota, Colorado, Kansas, and Nebraska. In the "mile high" plains in the center of the continent, the named layers preserve marine fossils from the Late Cretaceous Period. The term Benton Limestone has also been used to refer to the chalky portions of the strata, especially the beds of the strata presently classified as Greenhorn Limestone, particularly the Fencepost limestone.

Naming and status
The name was applied by Meek, F.B. and Hayden, F.V. in 1862 to the gray marine shales, often chalky in the middle layers, lying above the terrestrial Dakota Sandstone and usually below the massive limestones at the base of the Niobrara Chalk. The name was taken from the type outcrop at Fort Benton, today a small city in Montana on the Upper Missouri River.

Today, the Benton classification is obsolete in some regions, having been replaced by the ascending sequence Graneros Shale/Belle Fourche Shale, Greenhorn Limestone, and Carlile Shale. However, many old publications used the name. And the use of the Benton Group name continues in the Front Range where the Graneros Shale, Greenhorn Limestone, Carlile Shale, and Codell Sandstone may be recognized as member units.

In the lower Missouri River, west of Yankton, South Dakota, the distinction between the Benton and the Niobrara is very clear. This is near Meek and Hayden's type location for the Niobrara, the Niobrara River. On the shores of Lewis and Clark Lake between Yankton and the Niobrara River, high bluffs of near white Fort Hays Limestone are perched above the top of the gray shales that Meek and Hayden named "Fort Benton". However, at their Fort Benton type location for the Benton Group, the Fort Hays Limestone layer is hardly distinct from the Benton Shale and is identifiable only by its major change in fossil species.

The Mancos Shale of the Colorado Plateau correlates with the Colorado Shale, and the Tokay Tongue of the lower Mancos is the synonym for the Benton Shale.

Bentonite
There are many thin beds of volcanic ash in the unit that have devitrified into mostly montmorillonite. Taking its name from the formation, this material is called bentonite. Iron sulfide in the bentonite seams converts to rust when exposed to air resulting in orange lines across exposures of Benton shale and chalk.

Gallery

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Shale formations of the United States
Cretaceous Colorado
Cretaceous Montana
Cretaceous geology of Wyoming
Cretaceous geology of North Dakota
Cretaceous geology of South Dakota
Cretaceous geology of Nebraska


title: Blackleaf Formation

text:
The Blackleaf Formation is a geologic formation in Montana. It preserves fossils dating back to the Albian to Cenomanian stages of the Cretaceous period.

Description
The formation comprises an isolated, sinuous sandstone body sitting within and crosscutting a succession of three mudrock units. The lowermost mudstone is greater than 35 cm in thickness, light greenish grey and weakly calcareous. This unit exhibits extensive dark reddish grey mottling over its uppermost portion. Additionally, carbonate nodules as much as 4.5 cm in diameter form a discontinuous layer of 20–25 cm below the sharp upper contact of the unit. A dark greenish-grey claystone succeeds vertically. This 25 cm thick unit is calcareous with a platy structure and grades upwards into a greenish grey blocky mudstone with some organics. This third unit encloses the upper portion of the sedimentary structure and bears a sharp, irregular contact with an overlying burrowed dark red claystone. The lithology of the structure contrasts sharply with the surrounding host mudrock and facilitates recognition of the structure in the field.

The lower, bone-bearing portion consists of 25–30 cm of medium to fine, calcareous greenish-grey sandstone, moderately sorted with abundant plagioclase and other volcanogenic grains. Small (3–6 mm), rounded mud clasts are common in the coarser basal portion. This structureless unit fines upwards with an increasing clay content. A thin, 1–2 cm thick, grey claystone separates this lower sand- stone from an upper fine sandstone. The bedding parallels that of the host mudrocks. Reduced clay content, grey colour and larger (approx. 10 mm), platy mud clasts distinguish this unit from the otherwise similar, lower sandstone. A thin (less than 1 cm) rim of tan claystone with abundant calcite veins separates the lower portion of the structure from the host mudrocks.

Fossil content
The following fossils were reported from the formation:

Reptiles
 Oryctodromeus cubicularis
 Bernissartia sp.
 Glyptops sp.
 Ankylosauridae indet.
 Chelydridae indet.
 Dromaeosauridae indet.
 Goniopholididae indet.
 Hadrosauridae indet.
 Testudines indet.
 Tyrannosauridae indet.

Fish
 Neopterygii indet.

Flora
 Araliaephyllum westonii
 cf. Aralia wellingtonia
 Araliopsoides cf. cretacea
 cf. Aspidophyllum trilobatum
 cf. Ficus ovatifolia
 cf. Celastrophyllum sp.
 Cinnamomoides sp.
 Nymphaeites sp.
 Platanophyllum sp.
 cf. Protophyllum sp.

See also
 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Bibliography

Geologic formations of Montana
Cretaceous System of North America
Cretaceous Montana
Albian Stage
Cenomanian Stage
Mudstone formations
Sandstone formations
Shale formations
Siltstone formations
Deltaic deposits
Fluvial deposits
Lacustrine deposits
Ooliferous formations
Paleontology in Montana


title: Marias River Shale

text:
The Marias River Shale is a geologic formation in Montana. It preserves fossils dating back to the Cretaceous period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Shale formations of the United States
Cretaceous Montana


title: Montana Formation

text:
The Montana Formation is a geologic formation in Montana. It preserves fossils dating back to the Cretaceous period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Cretaceous Montana


title: Shell Creek Shale

text:
The Shell Creek Shale is a geologic formation in Montana. It preserves fossils dating back to the Cretaceous period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Shale formations of the United States
Cretaceous Montana


title: Thermopolis Shale

text:
The Thermopolis Shale is a geologic formation which formed in west-central North America in the Albian age of the Late Cretaceous period. Surface outcroppings occur in central Canada, and the U.S. states of Montana and Wyoming. The rock formation was laid down over about 7 million years by sediment flowing into the Western Interior Seaway. The formation's boundaries and members are not well-defined by geologists, which has led to different definitions of the formation. Some geologists conclude the formation should not have a designation independent of the formations above and below it. A range of invertebrate and small and large vertebrate fossils and coprolites are found in the formation.

Geological history
The Western Interior Seaway was an inland sea that existed from the Late Jurassic (161.2 ± 4.0 to 145.5 ± 4.0 million years ago [Ma]) to the end of the Paleogene (66 to 23.03 Ma). It existed in the middle of North America, extending from the Arctic Ocean to the Gulf of Mexico. It was roughly  long and  wide. The seaway was relatively shallow, with a maximum depth estimated at .

A foreland basin existed just to the east of the Sevier orogenic belt, which was inundated by the Western Interior Seaway. A forearc on the western side of the basin made this deeper than the eastern side, encouraging the build-up of sediment and, in time, sedimentary rock. Erosion of the Western Cordillera also contributed to the build-up of sedimentary rock on the western edge of the basin, while the more low-lying area to the east provided much less. Changes in the amount, type, rate, and other aspects of the sedimentation were caused by uplift, subsidence, sea level changes, and other factors. The water in the basin made at least two major advances and one major retreat during the Cretaceous, adding complexity to the rock and permitting the creation of riverine, marsh, and estuarine rock in addition to the principal shallow and deep marine rock.

Dating of bentonite and palynological evidence indicate that the Lower Thermopolis Member was deposited between 100.3 and 98.5 Ma. A study of Inoceramidae bivalves confirmed a Late Albian age. Deposition of the upper three members of the Thermopolis Shale occurred over approximately 7 million years.

Identification
The Thermopolis Shale was first identified in 1914 by geologist Ferdinand F. Hintze, Jr. He called it the "Lower Benton Shale", and included the Mowry Shale in the same formation. Hintze described three members: The basal "rusty beds", a lower shale, a  thick "Muddy Sand" (muddy sandstone), and an upper shale member. (The fourth member of the "Lower Benton Shale" was the Mowry Shale.)

The Thermopolis Shale was first named by geologist Charles T. Lupton in 1916. Lupton described the rocks as a formation lying conformably atop the Cloverly Formation, and conformably underlying the Mowry Shale. The Thermopolis Shale was the basal of four formations making up the Colorado Group. He described the Thermopolis Shale as Late Cretaceous in age, generally dark in color, from  thick, and with sandstone lenses common. At least one member of the Thermopolis Shale was also noted, a "muddy sand" layer about  thick. No type locality was identified, but the formation was named for the town of Thermopolis in Hot Springs County, Wyoming—where, nearby, outcroppings of the shale were well exposed. Lupton's division of the Thermopolis Shale was adopted by the United States Geological Survey and used for the next 50 years.

The stratigraphic history of the Thermopolis Shale was first outlined by geologist Don L. Eicher in 1962.

About the formation
The Thermopolis Shale belongs to both the Colorado Group and Dakota Formation. Both historically and currently, the stratigraphic units in these groups, and in the Thermopolis Shale, have been unclear, and the nomenclature used by geologists is not standardized. The identification of beds, members, and formations and their names have changed over time as well.

The Thermopolis Shale is said by Eicher to overlie the Cloverly Formation, although Rice, Porter et al., and Lash that in Montana and Wyoming the Kootenai Formation is geologically equivalent to the Cloverly Formation and thus conclude that the Thermopolis Shale overlies the Kootenai Formation.  There is disagreement as to the stratigraphic definition of the basal member of the Thermopolis Shale, however. Eicher has argued that the "rusty beds" division is clearly distinguishable in many ways from the Cloverly Formation, and thus belongs to the Thermopolis Shale. Seeland and Brauch assigned the "rusty beds" to the Cloverly Formation in 1975, an assessment concurred with by Finn in 2010. Porter et al., however, classified the "rusty beds" as part of the Fall River Sandstone in 1997.

What constitutes the upper boundary of the Thermopolis Shale is disputed, making it difficult to identify what overlays the Thermopolis Shale. In 1922, Collier identified the beds below the Mowry Shale as the Nefsy shale member of the Graneros Shale. This left the Thermopolis Shale underlying the Graneros Shale. But Rubey assigned these rocks to the Mowry Shale in 1931, so that now the Thermopolis Shale underlay the Mowry Shale. Eicher redefined these beds in 1960 as the Shell Creek Shale, separating them from the Mowry Shale. This effectively put the Thermopolis Shale below the Muddy Sandstone Formation. In 1998, Porter et al. identified the Shell Creek Shale as the upper member of the Thermopolis Shale, a position with which Lash agreed in 2011.

Depending on the definition of the shale, and the location, the Thermopolis Shale varies widely in thickness. Chester N. Darton estimated the size of the formation at  (including the "rusty beds") in 1906. In 1914, Hintze described the formation as  deep. Hewett and Lupton reported in 1917 that the shale (including the "rusty beds") to be  thick in the Bighorn Basin, while Finn (not including the "rusty beds" reported a thickness in the same area of . On the Wind River Indian Reservation of Wyoming, using the inclusive definition, it was reported to be a more robust  thick. It is only  thick in the Shirley Basin of southwest central Wyoming.

Generally speaking, the Thermopolis Shale consists of a dark gray to black shale, with thin layers of bentonite, sandy claystone, and siltstone interspersed throughout the shale. Depending on the stratigraphic definition of the formation, a gray, thinly-bedded sandstone member exists between the upper and lower members.

Members
For the purposes of this article, the definition of the Thermopolis Shale used by Porter et al.  and Lash will be used, recognizing (as Condon does) that there is scientific disagreement about this issue. Using this definition, there are four members of the Thermopolis Shale:

The "rusty beds" Member—This basal member of the Thermopolis Shale was first described by Nelson H. Darton in 1904, who noted the sandy nature of this shale and its rusty brown color. The color was attributed to the presence of iron, and Darton coined the term "rusty series" in 1906. The first geologist to use the term "rusty beds", however, was Chester W. Washburne in 1908. These rocks were laid down as the level of the Western Interior Seaway began a major rise. Erosion of the lacustrine Kootenai Formation occurred, creating a nonconformity as the new "rusty beds" rock was laid down. In some places, the entire upper Himes Member of the Cloverly Formation had eroded, allowing the "rusty beds" to lie disconformably on the medial Little Sheep Member. The "rusty beds" consist of thin layers of reddish-brown sandstone between  thick, separated by leaves of black shale between  thick. The basal beds of the "rusty beds" are probably estuarine or deltaic in nature. The member was estimated as between  and  in thickness. The "rusty beds" member is geologically equivalent to the Fall River Sandstone, Greybull Sandstone, and some members of the Dakota Formation.
Lower Thermopolis Member—This member of the Thermopolis Shale was first briefly described by Darton in 1904, and more completely by Washburne in 1908. The member has remained unnamed or only informally named, usually being only referred to as the Lower Thermopolis Member. These rocks were deposited as the northern and southern portions of the Western Interior seaway linked together, and represents deposition during the maximum "transgression" (rise in sea level) of the Western Interior Seaway. The transition from the "rusty beds" to the Lower Thermopolis Member is gradational, probably due to erosion or flooding. The Lower Thermopolis Member was described by Washburne and Harshman as carbon-rich black shale with occasional sandstone lenses in its lower portion, and E.N. Harshman noted it was fissile. Porter et al., however, described the rock in 1993 as mudstone or siltstone, implying a lack of fissility. The Lower Thermopolis Member is geologically equivalent to the Skull Creek Shale.

Muddy Sandstone Member—This member of the Thermopolis Shale was first briefly described by Darton in 1904, and much more completely by Hintze in 1914. Hintze described it as a widespread almost white sandstone member,  thick, with small, uniform, poorly cemented grains. Hintze called this member the "Muddy sand", after the terminology used by oil and gas drillers in Wyoming. It remained informally known as the "Muddy sand" into the 1960s, despite widespread acknowledgement among geologists that it was significant and widely occurring and worthy of a formal name. By 1972, the member had received the formal name "Muddy Sandstone Member". The Muddy Sandstone began to be laid down during a period when water levels in the Western Interior Seaway dropped, and this deposition continued once sea levels rose again. An erosional unconformity occurred while the sea receded, over which estuarine and fluvial deposits were laid down as the Muddy Sandstone. Thus, in some areas contact with the overlying Muddy Sandstone is sharp and unconformable, while in others it is conformable and gradational. Deposition of the Muddy Sandstone continued around the foreland basin's margins, while the Upper Thermopolis Member was laid down conformably above the Muddy Sandstone in the basin's interior. The Muddy Sandstone consists of a number of thin beds of fine-grained, silty sandstone of buff, brownish-grey, or grey color. It is shaly, contains carbon flecks and pyrite crystals, and when weathered is either buff or grey. Some beds exhibit ripple marks. The sandstone is interbedded with thin beds of shale, siltstone, and (occasionally) bentonite. Lupton estimated the Muddy Sandstone's thickness at  in thickness, although Porter et al. have pointed out that it varies widely in thickness from place to place. David Seeland and Early Brauch have concluded that is because pre-Laramide geologic structures or topography probably governed the distribution of Muddy Sandstone deposits. The Muddy Sandstone Member is geologically equivalent to the Birdhead Sandstone.
Upper Thermopolis Member—This member of the Thermopolis Shale was first briefly described by Darton in 1904, and more completely by Washburne in 1908. Norman Mills was the first to use the term "Upper Thermopolis" in 1956, although the member remained formally unnamed. The Upper Thermopolis Member was laid down conformably atop the Muddy Sandstone in the foreland basin's interior during the latter part of the Western Interior Seaway's second transgression. Washburne described the member as consisting of bluish-black shale, interbedded very occasionally with beds of volcanic ash and bentonite in the upper part. Lupton argued for two distinct divisions in the member: Lower beds of soft, black shale about  thick, and upper beds of hard shale with sandstone lenses about  thick. Harshman has provided evidence that the upper beds are a transitional zone leading to the Mowry Shale. He observed that the upper beds consist primarily of thin, limy, silty sandstone and silty shale beds interbedded with dense, siliceous Mowry Shale with the occasional bed of silty lignite. The sandstone beds exhibit mud cracks and root tubes which indicate a paludal (marsh deposited) origin. The differences between the upper and lower beds led Harshman to conclude that some of the sandier beds near the base of the Upper Thermopolis Member may belong to the Muddy Sandstone Member. Seeland and Brauch also found extensive evidence of gradational contact with the overlying Mowry Shale. The Muddy Sandstone Member is geologically equivalent to the Shell Creek Shale.

Surface outcroppings of the Thermopolis Shale occur in central Canada, and the U.S. states of Montana and Wyoming. Marine-deposited rock thins toward the west, while nonmarine-deposited rock thins toward the east. The marine-deposited rock is primarily shale, with some limestone, sandstone, and siltstone. The nonmarine rock is primarily sandstone, with some coal, shale, "black" or carbonaceous shale, and siltstone.

Fossil record
The Thermopolis Shale is unusually rich in marine vertebrate fossils, consisting primarily of skeletal material, teeth, and coprolites.

A particularly rich marine vertebrate fossil zone exists in the lower beds of the Upper Thermopolis Member. Marine crocodile, plesiosaur (primarily Edgarosaurus muddi), ray (primarily Pseudohypolophus and an unidentified species), sawfish (primarily Onchopristis), and turtle (primarily Baenidae and Glyptops) remains, as well as whole coprolites, are abundant. Hybodont shark (primarily Meristodonoides), ganoid-scaled and teleost fish, and invertebrate fossil ammonoids (primarily Baculites) are also found.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References
Notes

Citations

Bibliography

Shale formations of the United States
Cretaceous Montana


title: Jefferson Formation

text:
The Jefferson Formation is a geologic formation in Montana. It preserves fossils dating back to the Devonian period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Devonian Montana
Devonian Idaho
Devonian southern paleotropical deposits


title: Three Forks Shale

text:
The Three Forks Shale is a geologic formation in Montana and North Dakota. It preserves fossils dating back to the Devonian period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Devonian Montana
Devonian southern paleotropical deposits


title: Ellis Formation

text:
The Ellis Formation is a geologic formation of the Ellis Group in Montana.

It preserves fossils dating back to the Jurassic period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Jurassic Montana


title: Hepburn's Mesa Formation

text:
The Hepburn's Mesa Formation is a geologic formation in Montana. It preserves fossils dating back to the Neogene period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Neogene Montana


title: Madison Valley Formation

text:
The Madison Valley Formation is a geologic formation in Montana. It preserves fossils dating back to the Neogene period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Neogene Montana


title: Sixmile Creek Formation

text:
The Sixmile Creek Formation is a geologic formation in Montana. It preserves fossils dating back to the Neogene period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Neogene Montana


title: Deep River Formation

text:
The Deep River Formation is a geologic formation in Montana. It preserves fossils dating back to the Neogene period.

Fauna

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Neogene Montana


title: Flaxville Gravels

text:
The Flaxville Gravels is a geologic formation in Montana. It preserves fossils dating back to the Neogene period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Geologic formations of Montana
Neogene stratigraphic units of North America


title: Bear Formation

text:
The Bear Formation is a geologic formation in Montana. It preserves fossils dating back to the Paleogene period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Paleogene Montana


title: Climbing Arrow Formation

text:
The Climbing Arrow Formation is a geologic formation in Montana. It preserves fossils dating back to the Paleogene period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Paleogene Montana


title: Cook Ranch Formation

text:
The Cook Ranch Formation is a geologic formation in Montana. It preserves fossils dating back to the Paleogene period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Paleogene Montana


title: Dell Beds Formation

text:
The Dell Beds Formation is a geologic formation in Montana. It preserves fossils dating back to the Paleogene period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Paleogene Montana


title: Dunbar Creek Formation

text:
The Dunbar Creek Formation is a geologic formation in Montana. It preserves fossils dating back to the Paleogene period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Paleogene Montana


title: Visa requirements for Myanmar citizens

text:
Visa requirements for Myanmar citizens are administrative entry restrictions by the authorities of other states placed on citizens of Myanmar. As of 28 September 2019, Myanmar citizens had visa-free or visa on arrival access to 46 countries and territories, ranking the Myanmar passport 95th in terms of travel freedom according to the Henley Passport Index. Myanmar is also a part of ASEAN and has visa-free access to all other ASEAN states besides Malaysia.

Recent changes
On 6 September 2017, India has announced e-visa for citizens of Myanmar.

Visa requirements map

Visa requirements

See also

Visa policy of Myanmar
Myanmar passport
Foreign relations of Myanmar

References

Notes

Myanmar
Foreign relations of Myanmar


title: Lebo Member

text:
The Lebo Member is a geologic member of the Fort Union Formation in Montana and Wyoming. It preserves fossils dating back to the Paleogene period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Paleogene Montana
Paleogene geology of Wyoming


title: Melville Formation

text:
The Melville Formation is a geologic formation in Montana. It preserves fossils dating back to the Paleogene period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Paleogene Montana


title: Passamari Formation

text:
The Passamari Formation is a geologic formation in Montana. It preserves fossils dating back to the Paleogene period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Paleogene Montana


title: Polecat Bench Formation

text:
The Polecat Bench Formation is a geologic formation in Montana. It preserves fossils dating back to the Paleogene period. The polyglyphanodontian lizard Chamops is known from this formation.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Paleogene Montana
Paleogene geology of Wyoming
Thanetian Stage
Ypresian Stage


title: Renova Formation

text:
The Renova Formation is a geologic formation in Montana. It preserves fossils dating back to the Paleogene period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Paleogene Montana


title: Sage Creek Formation

text:
The Sage Creek Formation is a geologic formation in Montana. It preserves fossils dating back to the Paleogene period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Paleogene Montana


title: Toston Formation

text:
The Toston Formation is a geologic formation in Montana. It preserves fossils dating back to the Paleogene period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Paleogene Montana


title: Tullock Formation

text:
The Tullock Formation is a geologic formation in Montana. It preserves fossils dating back to the Paleogene period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Geologic formations of the United States
Paleogene Montana
Puercan


title: Park City Formation

text:
The Park City Formation is a geologic formation in Montana and Utah. It preserves fossils dating back to the Permian period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Permian geology of Montana
Permian Idaho
Permian geology of Utah


title: Shedhorn Formation

text:
The Shedhorn Formation is a geologic formation in Montana. It preserves fossils dating back to the Permian period.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Permian geology of Montana


title: J. C. Daly

text:
J. C. Daly (1846-1932) was a lawyer, a California politician and a farmer in Ventura County, California.  He was an authority on water rights and agricultural laws.

Personal
Daly was born in Rochester, New York, on May 13, 1846, and was educated at Niagara College, New York. He was married to Mary Ann Burke in Utica, New York; she died about 1932. They had three children, Joseph B. of San Fernando, California, William F. of Ventura, California, and Kate (Mrs. T.J. Donovan).

The family came to California in 1883 and settled in Los Angeles in 1887, then moved to Ventura County in 1889.

Daly died at age 86 at the home of his son, William, in the Mound district of Ventura, on December 8, 1932.  Funeral services were at Mission San Buenaventura, with burial in Ventura Cemetery.

Vocation

Legal
In Los Angeles, Daly was elected city attorney in 1886 and reelected in 1887. In 1896 he served as justice of the peace in Ventura County. In 1898 he was California port commissioner in San Francisco, and in 1902 he was assistant California attorney general. In politics, he was at one time a Republican and later a Democrat.

He was for many years an associate counsel for the Southern Pacific Railway. Daly was also an authority on water rights and farming laws.

Land development and farming
In 1905 Daly purchased on behalf of the Adams-Phillips Company a half interest in the former 2,500-acre Dixie Thompson rancho east of Ventura, which had the largest plantation of lima beans in the world, with a seafront of nearly five miles. The west end of the rancho was to be divided into tracts for resale.

As president of the Fruit Growers Association, in February 1908 he addressed a letter to U.S. Secretary of Agriculture James Wilson supporting the use of sulphurization in preserving fruit. He wrote:

Governments exercising paternal supervision, such as Germany, have attempted to limit the amount of sulphur dioxide in our dried fruits, which legislation, we have contended, was to prevent the light, beautiful and appetizing California dried fruits coming in competition with the dark-colored and poor-tasting fruit produced and sold in that country.

In 1916 Daly was noted to be a "prominent" bean grower.

References and notes

Los Angeles City Attorneys
1846 births
1932 deaths
Burials in Ventura County, California
California Democrats
California Republicans
19th century in Los Angeles


title: Dinwoody Formation

text:
The Dinwoody Formation is a geologic formation in the western United States (Idaho, Montana, Utah, Wyoming). It preserves fossils dating back to the Triassic period (Induan stage).

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Triassic geology of Nevada
Triassic geology of Utah
Triassic geology of Wyoming


title: Thaynes Limestone

text:
The Thaynes Formation is a geologic formation in Montana and Idaho, United States. It was recently elevated to group status, as the Thaynes Group.

It preserves fossils dating back to the Triassic period, such as Ammonoidea, Actinopterygii, Actinistia, Conodonta, Gastropoda, Nautiloidea, Ichthyosauria, and others. A diverse fauna known as the Paris biota has been described from the Thaynes Formation.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana
 Paleontology in Idaho

References

Triassic geology of Montana
Triassic Idaho
Triassic geology of Utah
Triassic geology of Wyoming


title: Blacktail Deer Creek Formation

text:
The Blacktail Deer Creek Formation is a geologic formation in Montana. It preserves fossils.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Cretaceous Montana


title: Greyson Shale

text:
The Greyson Shale is a geologic formation in Montana. It preserves fossils.

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Geologic formations of Montana


title: Wiota Gravels

text:
The Wiota Gravels is a geologic formation in Montana. It preserves fossils dating to the Pleistocene .

See also

 List of fossiliferous stratigraphic units in Montana
 Paleontology in Montana

References

Geologic formations of Montana


title: Caçarelhos e Angueira

text:
Caçarelhos e Angueira is a civil parish in the municipality of Vimioso, Portugal. It was formed in 2013 by the merger of the former parishes Caçarelhos and Angueira. The population in 2011 was 335, in an area of 53.16 km².

References

Freguesias of Vimioso


title: Jesús Quintero

text:
Jesús Rodríguez Quintero (18 August 1940 – 3 October 2022) was a Spanish journalist, editor and presenter of Spanish programs in radio and television, known in the media as Jesús Quintero.

Biography
Quintero was born in San Juan del Puerto, Huelva, Spain, on 18 August 1940. He was introduced into the theatrical world and from there jumped to RNE (Radio Nacional de España) in 1973, which began a long career as a presenter. His first program was Studio 15-18, presented with Marisol Valle. It was a great success and the star program in the attempted normalization of public radio programming that passed from dictatorship to a new period.

Quintero's flagship program, with schemes that would revolutionize the media was El hombre de la roulot (Man of Roulotte) and El loco de la colina (The fool on the hill), which made him a social phenomenon even outside Spain, Argentina or Uruguay.

Quintero also appeared as a lecturer in the teaching world, such as when he delivered the conference Journalism and Commitment on 17 October 2002 at the Faculty of Communication Sciences of the University of Málaga, on his tenth anniversary. After this speech, he unveiled a plaque to baptize one of the classrooms of the center with his name, sign of respect and admiration that produces the journalist.

Quintero was producer of the singer Soledad Bravo and guitarist Paco de Lucía.

Quintero was author of the books Trece noches (Thirteen nights) (1999) with Antonio Gala, Cuerda de presos (Prisoners Rope) (1997) and Jesús Quintero: entrevista (Jesús Quintero: Interview) (2007).

Quintero died on 3 October 2022, at the age of 82.

In radio
 Música de los cinco continentes (Music from five continents)
 Círculo internacional (International circle)
 Estudio 15/18 (Studio 15/18)
 A 120
 Ciudades (Cities)
 El hombre de la Roulotte (Man of Roulotte)
 Tres a las tres (Three to three)
 Andalucía Viva (Andalucía alive)
 El loco de la colina (The fool on the hill) (1981–1986), RNE and Cadena Ser
 El lobo estepario (Steppenwolf), 1992, Onda Cero
 Entre dos luces (Between two lights), 2002

In television
 El perro verde (The green dog), 1988, in TVE
 Qué sabe nadie (Does anyone know), 1990–1991, in Canal Sur
 Trece noches (Thirteen nights), 1991–1992, in Canal Sur
 La boca del lobo (The mouth of the wolf), 1992–1993, in Antena 3
 Cuerda de presos (Chain gang), 1995–1996, in Antena 3
 El Vagamundo, 1999–2002, in Canal Sur
 Ratones coloraos, 2002–2004, in Canal Sur
 El loco de la colina (The fool on the hill), 2006, in TVE
 La noche de Quintero (The night of Quintero), 2007, in TVE
 Ratones coloraos, 2007–2009, in Canal Sur, Telemadrid and 7 Región de Murcia
 El mundo de Jesús Quintero (The world of Jesús Quintero), summer 2008, in Canal Sur
 El gatopardo, 2010–20??, in Canal Sur
 La noche del loco (The night of the crazy)
 El sol, la sal y el son in Canal Sur
 El loco soy yo (I'm crazy) in Canal Sur
 Un loco en América in Telemundo

Awards
 National Communication Media Award (2006)
 Television presenter of the year (2006)
 Golden antenna for his program, El Vagamundo (2003)
 Premio Ondas (2001)
 Award Best interviewer of the Millennium
 Award Andaluz of the 2000 year Award King of Spain'' of journalism (1990)
 Premio Ondas Internacional (1990)
 Medal of Andalucía
 Knight of Argamasilla de Alba
 Award for the most innovative radio done

References

1940 births
2022 deaths
Spanish editors
Spanish journalists
Spanish television directors
Spanish television presenters
Spanish radio presenters
People from the Province of Huelva


title: Edoardo Bencivenga

text:
Edoardo Bencivenga (Naples, ? – Rome, June 6, 1934) was an Italian film director; Bencivegna started in 1907 filming his first short film Raffaello e la Fornarina , in his career he made over 60 films, the last one in 1922.

Filmography
 Raffaello e la Fornarina – short film (1907)
 L'uomo dalla testa dura (1908)
 Raffaello Sanzio e la fornarina (1909)
 L'ignota – short film (1910) –
 Il serpe – short film (1910)
 Il barone Lagarde – short film (1910) –
 Maria Bricca (1910)
 I cavalieri della morte – short film (1910) –
 L'innocente (1911)
 Pietà di mamma – short film (1911)
 Il processo Clémenceau (1912)
 Se fossi Re! – short film (1912)
 La nave – short film (1912) – come Eduardo Bencivenga
 Il fischio della sirena – short film (1912)
 Il ragno – short film (1913)
 Cuor di poeta – short film (1913)
 L'epopea napoleonica (1914)
 Fata Morgana – short film (1914)
 La du Barry (1914)
 DuBarry (1915)
 L'onore di morire (1915)
 Cuore ed arte (1915)
 Il dubbio – short film (1915)
 Savoia, urrah! – short film (1915)
 Guerra redentrice (1915)
 Alla bajonetta!.. (1915) – as Eduardo Bencivenga
 Eroismo di madre – cortometraggio (1915)
 Il sacrificio del nonno – short film (1915)
 Il ridicolo (1916)
 Don Giovanni (1916)
 Trama sventata (1916)
 Il nemico occulto (1916)
 Il medaglione – short film (1916)
 Ferréol (1916)
 L'anello di Pierrot (1917)
 La figlia di Jorio (1917)
 Pazzia contagiosa – short film (1917)
 Le due orfanelle (1918)
 P.L.M. ossia l'assassinio della Paris-Lyon-Mediterranée (1918)
 Mariute (1918)
 L'orgoglio (1918)
 Voca e canta – short film (1918)
 L'ira (1918)
 Fiamme avvolgenti (1918)
 L'invidia (1919)
 Sullivan (1919)
 Il cieco (1919)
 La piovra (1919)
 La leggenda dei tre fiori (1919)
 La lussuria (1919)
 L'onore della famiglia (1919)
 La morte civile (1919)
 La colpa vendica la colpa (1919)
 Il cuore di Roma (1919)
 La donna dai capelli d'oro (1920)
 La follia del giuoco (1920)
 Fino alla tenebra (1920)
 Il marito perduto (1920)
 La donna, il diavolo, il tempo (1921)
 La moglie di sua eccellenza (1921)
 Il figlio di Coralie (1921)
 Hermione (1921)
 Dionisia (1921)
 Il dubbio (1921)
 Non è resurrezione senza morte (1922)

References

1934 deaths
Italian film directors
Silent film directors
Year of birth missing


title: Herbert Henry Gowen

text:
Herbert Henry Gowen (1864–1960) was an Anglican missionary and orientalist who wrote on the history of China and Japan and was long associated with the University of Washington.

Early life and education
Herbert Gowen was born in Yarmouth, England and earned a B.A. degree from St. Augustine's College in 1886. He was ordained a deacon in the Church of England the same year.

Career

Missionary work
Following his ordination, Gowen left to Hawaii at the invitation of Alfred Willis, then the Anglican bishop of Honolulu. Willis was away when Gowen arrived, but he was greeted by a group of Chinese Christians from Kohala and led a service the following Sunday in what is considered the "beginning of St. Peter's Church, Honolulu".

Gowen helped found the Chinese mission school in Honolulu, Hawaii where, among the students, was Sun Yat-sen. Gowen remained in Honolulu for four years, serving as the curate of the Cathedral of Saint Andrew, and as chaplain to the Hawaiian Royal Family. From 1890 to 1897 Gowen served in Canada, as curate of Holy Trinity Cathedral and as rector of St. Barnabas Church in New Westminster, British Columbia. He left Canada to continue on to the United States, serving as rector of Seattle's Protestant Episcopal Trinity Church and establishing St. Peter's Japanese Mission.

University of Washington
In 1909 Gowen became the founding chair of the University of Washington's Department of Oriental Subjects, a post he would hold until 1929. Gowen continued to teach at the University of Washington until 1938, and would continue to be affiliated with the university until 1945.

Personal life
Gowen was a polyglot and read, in addition to English, Arabic, Chinese, Hebrew, Japanese, and Sanskrit.

In 1977 Condon Hall at the University of Washington was renamed Gowen Hall in Gowen's honor.

Bibliography
 Five Foreigners in Japan (1936)
 A History of Indian Literature from Vedic Times to the Present Day (1931)
 An Outline History of Japan (1926)
 Asia: A Short History from the Earliest Times to the Present Day (1926)
 The Napoleon of the Pacific, Kamehameha the Great (1919)
 Church Work in British Columbia: Being a Memoir of the Episcopate of Acton Windeyer Sillitoe (1899)

Notes

References

1864 births
1960 deaths
University of Washington faculty
Anglican missionaries in Japan
British expatriates in the Hawaiian Kingdom
British expatriates in Canada
British expatriates in the United States
People from Great Yarmouth