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HomeBusiness Products & ServicesWhy People Think Companies Are A Good Idea
Why People Think Companies Are A Good Idea
January 21, 2018 Business Products & Services Comments Off on Why People Think Companies Are A Good Idea
Tips for Identifying the Best Chairman
Many firms or organizations and even groups endeavor to develop their best to become their best chairmen. The point of concern is however if the chairman will in cooperate the resourcefulness in the rest of the team so as to realize betterment for the group.Or will the chairman simply lead on his own expertise?
The team forms the most sensitive integral part of any organization group or firm.Firms, companies or institutions are formed of teams.This means that the chairman plays a very vital role in the overall productiveness of the organization. Consequently, chairmen should be selected in a very careful way, considering the overall implication in the firms productiveness and efficiency. The chairman will play a big role in ensuring that the company succeeds or fails. Consequently, it becomes needful to measure the effectiveness of a chairman from time to time. If this is practiced, it will ensure that the chairman doesn't become redundant.
The best chairman will be defined by several factors. The best chairman will demonstrate the following qualities.
The best chairman should be energetic. A continual percolation of a chairman's energy should be instantly felt at different levels of the hierarchy, ensuring that the feeling is at every level of the hierarchy.
A chairman should be good at prioritizing. Projects should be carried out in the order of their priority. The chairman is the focus of the subordinates. They will make fun of a chairman who is not confident and well-focused.
The best chairman will be effective in communication like Hussain al Nowais. Misunderstandings are avoided by the effective communication of the best chairman. Without clarity, it is hard to solve issues in a good manner.
See also Lessons Learned from Years with Services
Again, the best chairman will his team and also keenly listen to all members. This makes the team members to own the group. This is well going for the team since the sense of ownership by all team members will make them to want to improve the team.
The form of leadership that the best chairman will use it the democratic leadership. Deriving work from the team members requires democratic leadership.This good leader will share his authority and leadership with team members without micromanaging.
The best chairman will praise the work of his team mates. Any team feels blessed to have a chairman who gives credit to the deserving members. The best chairman will never absorb praise when the team wins but will give it to the team members.This will help the team members to stay productive and encouraged.
The team will derive its cohesion from the chairman.
Why not learn more about Finances?
On Realtors: My Thoughts Explained


CHARLESTON, S.C. – What started as a pitcher's duel turned into teams trading blow-for-blow before Radford stole a 6-5 Friday night win from the Charleston Southern baseball team in 11 innings at CSU Ballpark.
CSU (8-16, 0-4 Big South) starter Jaret Bennett and Radford (8-13, 2-2 Big South) each tossed five scoreless innings before both offenses collected their first hits of the night and scored six combined runs – three for both in each half of the sixth.
Radford scored their first two runs on a one-out Spencer Horwitz two-run homer then added another on J.D. Mundy's solo longball. CSU responded though with three runs on two Radford errors and their first two knocks. CSU scored on a fielder's choice and throwing error for a 3-1 deficit before Blakeney cracked the hit column and drove-in two for a 3-3 tie after six frames.
The Highlanders hit a third home run off Bennett, the final one off the bat of Matt Roth for a 5-3 lead through the top of the seventh. CSU had another answer as sophomore shortstop Josh Asbill launched his first career home run to right field getting Bennett off the hook and tying the game once again.
Radford's Cameron Fritz and CSU's Tyler Weekley matched zeros down the stretch with Fritz tossing 4.0 scoreless frames and striking out eight Buccaneer batters for the win while Weekley took the hard-luck loss tossing 4.2 innings of relief allowing just the one earned run in the 11th inning.
Radford got on the board first behind Horwitz' long fly to right then Mundy sent a solo shot to right center for a 3-0 Highlander lead through six.
Charleston Southern responded with their own three-spot as Brooks Bryan reached on an error and Josh Asbill got plunked for the second time for two-on and none down. Another Radford error brought in the first run then Blakeney sent a ball back up the middle for two runs and 3-3 tie.
Radford responded with two more in the seventh on their third home run –this time a two-run blast from Roth made it 5-3 at the seventh-inning stretch.
Asbill had a response of his own as his third time reaching safely came via a two-run shot to right – his first collegiate home run and a 5-5 tie after seven.
Weekley and Fritz traded zeros before the Highlanders pushed across the go-ahead single in the 11th on Roth's two-out single.
The Bucs fell for the first time in extra innings Friday moving to 2-1 on the season. The 11-inning affair was also the second for CSU over the past three contests taking a 7-6 win at Savannah State in 12 innings Tuesday.
Jason Miller collected another three-hit day –his third of the 2019 season.
Josh Asbill hit his first career home run in the seventh inning and he became the 10th different Buccaneer with a two-RBI performance on the season.
Both Asbill and Brooks Bryan scored twice Friday night making up four the five Buccaneer tallies.
The five no-hit innings from both sides marked the furthest into a game CSU or their opponent reached the hit column as the game started as a pitcher's duel.
CSU and Radford continue their weekend series with game two set for 4 p.m. Saturday from CSU Ballpark.


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Q: Curve fitting: How to optimize x_value model for curve fitting in python I am trying to fit an exponential curve into my data. However, I am having some trouble defining the x_value model properly in order to have a representative curve-fit to the data. I would think that the approach I used in preparing the DataFrame dataTable, is not optimal in the subsequent steps. I tried using arange() function to define x_line, but I wasn't successful. I would appreciate some help. See the table, the sample code I used, and the output.
Table

Code
import os
import pandas as pd
import seaborn as sns
import numpy as np
import matplotlib.pyplot as plt
from numpy import exp
from scipy.optimize import curve_fit

# file path
folder = '...'
fileTable = os.listdir(folder)

for i in fileTable:
    if i.endswith('.csv'):
        df = pd.read_csv(i, index_col=None)

# creat a new table
series_df = df.loc[:, df.columns.str.startswith('s')]
time_df = df.loc[:, df.columns.str.startswith('timeframe')]
df_new = [series_df, time_df]
newTable = pd.concat(df_new, axis =1)

dataTable = newTable.melt('timeframe', var_name='Series', value_name='length').dropna()
x, y = dataTable['timeframe'], dataTable['length']

# plot the data
plt.figure(figsize=(5,5))
ax1 = sns.scatterplot(data=dataTable, x=x, y=y, hue = 'Series')

# define a function for an exponential curve
def exponential(x, a, b, c):
    return a*(1-exp(-x / b)) + c

popt, _ = curve_fit(exponential, x, y)
a, b, c = popt
x_line = x
y_line = exponential(x, a, b, c)

# plot the fit on top of the raw data
axs = ax1.twinx()
ax2 =sns.lineplot(data=dataTable, x=x, y=y_line, color='green', alpha=1, ax=axs)
ax2.lines[0].set_linestyle('--')

Output

A: below data table in numerical format. Thanks.

s1
s2
s3
s4
s5
timeframe

0
0
0
0
0
0

2.3
3
1.4
1.5
2.6
5

3.6
4.3
3.7
3.3
3.4
10

4.5
5.4
4.5
4.4
4.4
15

5.3
6.3
5
5.2
5
20

5.5
5.2
5.6
5.3
25

5.8
6
6
5.9
30

6.7
6.4
6.3
6.1
35

7.4
6.3
6.8
6.3
40

7.3
6.7
6.9
6.7
45

7.4
6.9
7.3
6.
50

8
7.1
7.4
7
55

7.8
7.8
7.6

60

7.5

7.6

65

7.3

7.5

70

75

A: Below  this is more a comment than a definitive answer to the question.
I used another software than your software to fit the function y = a + b * exp( c * x) to your data.
See below the results with the data files S1 , S2 , S3 , S4 and S5 independently.
Then the five files where merged leading to a data of 60 points. The result of fitting to the exponential function is given at the bottom of next page.

I see no inconsistency.
So I suggest to first merge the five partial files into a unique file. Then import this big data file into a new session of your software for the nonlinear regression in order to avoid confusion with the previous calculus.
Nonlinear regression involves an iterative process. To start the process some "guessed" values of the unknown parameters are required. Possibly your software initiate the process with values not good enough. The values found above can be used as good initial values for a better relability.
NOTE :
For my above calculus I used the next very simple method :

Ref. : https://fr.scribd.com/doc/14674814/Regressions-et-equations-integrales .
One could improve a bit the accuracy with a post-treatment by nonlinear regression initiated with the above values of the parameters.
IN ADDITION : See below how the original data files were merged.
The "Merged data files" can be used as input to any nonlinear regression software.
The "Data ranked in increasing order of x" can be used as input to the method of fitting shown above.

redpajama_set_name: RedPajamaStackExchange


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Missouri River Drainage Basin Landform Origins Research Project is a 21st century Expedition of Discovery
About the "thick ice sheet that melted fast" geomorphology paradigm
Missouri River drainage basin landform origins research project, overview essay
Understanding the "Thick Ice Sheet that Melted Fast" Paradigm
Yellowstone River-North Fork Shoshone River drainage divide area landform origins east of Yellowstone National Park, Wyoming, USA
June 20, 2012 · Lamar River, Shoshone River, Wyoming, Yellowstone National Park, Yellowstone River
Eric Clausen Website: http://geomorphology… At present I am a professor emeritus having taught geology at Minot State University (North Dakota, USA) from 1968 until 1997. I was trained in geology at Columbia University and the University of Wyoming where my studies emphasized regional geomorphology. For many years I have pursued a research interest that developed when as result of geologic field work and interpretation of large mosaics of detailed North American topographic maps I discovered significant evidence previous investigators had ignored. Over a period of many years, after studying such anomalous evidence, I was forced to develop a fundamentally different interpretation of North American geomorphic history than that which is generally accepted. Geomorphology is the study of landforms and my interest as a geomorphology researcher is in determining the origin of large drainage systems, such as the Missouri River drainage basin in North America. The Missouri River drainage basin consists of thousands of smaller drainage basins, each of which has a history my essays (website posts) are trying to unravel. What I try to do is reconstruct the landscape the way it looked prior to the present day drainage system. I then try to determine how the present day drainage system evolved. While conducting my Missouri River drainage basin landform origins study I also developed an interest in scientific paradigms, especially in how scientific paradigms develop and how they are replaced. The Missouri River drainage basin landform origins project at geomorphologyresearch.com has been completed and I am currently creating a catalog of Philadelphia, PA area erosional landforms, which can be found at phillylandforms.info For off site questions and discussions about either project I can be contacted at eric2clausen@gmail.com
This essay uses topographic map evidence to interpret landform origins in the region between the Yellowstone River and the North Fork Shoshone River east of Yellowstone National Park along the Absaroka Range crest ridge in Wyoming. The Yellowstone River flows in a north-northwest direction to Yellowstone Lake and then in a northwest, northeast, north and northwest direction to the Yellowstone National Park north boundary and the west and north-northwest oriented Lamar River is an important Yellowstone River tributary. The North Fork Shoshone River originates as a southwest and south oriented stream south of the Lamar River headwaters and then turns to flow in a southeast and east direction to join the northeast oriented South Fork Shoshone River and to form the northeast oriented Shoshone River. Mountain passes or through valleys link Lamar River and Yellowstone River tributary valleys with North Fork Shoshone River tributary valleys. These mountain passes or through valleys are interpreted to be remnants of south oriented flood flow channels that once crossed the region. At that time the Absaroka Range did not stand high above surrounding areas and floodwaters could freely flow across what is today a major mountain range. Floodwaters were derived from the western margin of the thick North American ice sheet and were flowing in south and southeast directions from western Canada to and across the Yellowstone National Park region. Ice sheet related crustal warping raised the Absaroka Range and Yellowstone Plateau as floodwaters flowed across them. At the same time headward erosion of the deep Yellowstone River in Montana (north of the study region) from space in the deep "hole" the ice sheet had occupied and which was being opened up by ice sheet melting systematically beheaded south and southeast oriented flood flow channels in sequence from east to west. Floodwaters on north ends of beheaded flood flow channels reversed flow direction to create the north oriented drainage routes seen today and often captured south and southeast oriented floodwaters from west of the actively eroding Yellowstone River valley head. Barbed tributaries to north oriented Yellowstone River valley segments provide further evidence of these massive flood flow reversals.
The following interpretation of detailed topographic map evidence is one of a series of essays describing similar evidence for all major drainage divides contained within the Missouri River drainage basin and for all major drainage divides with adjacent drainage basins. The research project is interpreting evidence in the context of a previously unexplored deep glacial erosion paradigm, which is fundamentally different from most commonly accepted North American glacial history interpretations. Project essays are listed on the sidebar category list under their appropriate Missouri River tributary drainage basin, Missouri River segment drainage basin (by state), and/or state in which the Missouri River drainage basin is located.
The purpose of this essay is to use topographic map interpretation methods to explore Yellowstone River-North Fork Shoshone River drainage divide area landform origins east of Yellowstone National Park, which is located in northwest Wyoming. Map interpretation methods can be used to unravel many geomorphic events leading up to formation of present-day drainage routes and development of other landform features. While each detailed topographic map feature provides detailed evidence to be explained, the solution must be consistent with explanations for adjacent area map evidence as well as solutions to big picture map evidence puzzles. I invite readers to improve upon my solutions and/or to propose alternate solutions that better explain evidence and are also consistent with adjacent map area and big-picture evidence. Readers may do so either by making comments here or by writing and publishing their own essays and then by leaving a link to those essays in a comment here.
This essay is also exploring a new geomorphology paradigm in which erosional landforms are interpreted as evidence left by immense glacial melt water floods. Implied in that interpretation is the immense floods were derived from a thick North American ice sheet that created a deep "hole" in the North American continent and also melted fast. The previously unexplored paradigm being tested in this and other Missouri River drainage basin landform origins research project essays is a thick North American ice sheet, comparable in thickness to the Antarctic ice sheet, occupied the North American region usually recognized to have been glaciated, and through its weight and erosive actions created a deep North American "hole". The southwestern rim of that deep "hole" is today preserved in the high Rocky Mountains. The ice sheet through its weight and deep erosion (and perhaps deposition along major south-oriented melt water flow routes) caused significant crustal warping and tectonic change, through its action of melting fast produced immense floods that flowed across the continent, and through its action of melting fast systematically opened up space in the ice sheet created "hole" so headward erosion of newly developed north-oriented drainage systems captured immense south-oriented melt water floods and diverted immense melt water floods north into space the ice sheet had once occupied.
If this previously unexplored paradigm is correct the geographic region explored by this essay should contain evidence of immense floods that were captured by headward erosion of new valley systems so as to cause the floods to flow in a different direction. Ability of this previously unexplored paradigm to explain Yellowstone River-North Fork Shoshone River drainage divide area landform evidence east of Yellowstone National Park, Wyoming will be regarded as evidence supporting the "thick ice sheet that melted fast" paradigm.
Yellowstone River-North Fork Shoshone River drainage divide area location map
Figure 1: Yellowstone River-North Fork Shoshone River drainage divide area location map (select and click on maps to enlarge). National Geographic Society map digitally presented using National Geographic Society TOPO software.
Figure 1 provides a location map for the Yellowstone River-North Fork Shoshone River drainage divide area east of Yellowstone National Park and illustrates a region of northern Wyoming with Yellowstone National Park located in the northwest corner of Wyoming in the south half with Montana being located north of Wyoming. The Yellowstone River originates south of the southeast corner of Yellowstone National Park and flows in a north-northwest direction to Yellowstone Lake and then to Canyon, Wyoming. From Canyon the Yellowstone River flows in a northeast, north, and northwest direction to Gardiner, Montana and then in a northwest, north-northeast, and east-northeast direction to Big Timber, Montana. From Big Timber the Yellowstone River flows in an east-southeast and northeast direction to the north edge of figure 1 (east half) and north and east of figure 1 the northeast oriented Yellowstone River eventually joins the Missouri River. The northwest oriented Lamar River is an important Yellowstone River tributary in the northeast quadrant of Yellowstone National Park. The North Fork Shoshone River originates just east of Sylvan Pass (east of Yellowstone Lake) and flows in an east direction to Buffalo Bill Reservoir where it joins the north-northeast oriented South Fork Shoshone River to form the northeast oriented Shoshone River, which then joins the north and north-northeast oriented Bighorn River, which in turn joins the Yellowstone River near Bighorn, Montana (near north edge of figure 1). The Yellowstone River-Shoshone River drainage divide area east of Yellowstone National Park investigated in this essay begins with Lamar River-North Fork Shoshone River drainage divide area north of Sylvan Pass and extends southward to the drainage divide between the north-northeast oriented Yellowstone River headwaters and the north-northeast oriented South Fork Shoshone River and is located along the crest of the high Absaroka Range.
Today drainage systems seen in figure 1 are oriented in a north direction, however most north and northwest oriented drainage routes seen in figure 1 originated as south and southeast oriented flood flow channels. Floodwaters were derived from the western margin of a thick North American ice sheet and were flowing in south and southeast directions from western Canada across Montana into and across Wyoming. At that time the deep glacial erosion was creating a deep "hole" in the continent under the ice sheet and ice sheet related crustal warping was raising mountain ranges and high plateau areas along the ice sheet rim and elsewhere on the continent. The region seen in figure 1 could be considered to part of the deep "hole's" deeply eroded southwest rim and mountain ranges and other high areas (e.g. Yellowstone Plateau) seen in figure 1 were being uplifted as immense south and southeast oriented melt water floods flowed across them. Headward erosion of what was then a much deeper northeast and east oriented Yellowstone River valley from space in the deep "hole" being opened up by ice sheet melting captured the south and southeast oriented melt water floods and diverted floodwaters into the south end of the deep "hole" and then initially in a south direction to Gulf of Mexico, although as ice sheet melting continued new northeast and north oriented flood flow routes across the ice sheet floor opened up. Floodwaters on north and northwest ends of flood flow routes beheaded by the northeast and east oriented Yellowstone River valley headward erosion in Montana reversed flow direction to create what are today north oriented Yellowstone River tributary drainage systems and the north oriented Yellowstone River headwaters drainage system seen near the west edge of figure 1. Flood flow channels were beheaded in sequence from east to west and often newly reversed flood flow channels captured floodwaters from yet to be beheaded flood flow channels further to the west. Also aiding in the flood flow reversal process was crustal warping that was raising mountain ranges as floodwaters flowed across them. While this brief description gives a very generalized picture of how the figure 1 drainage system evolved there were many additional complexities and each valley segment has a story to tell. Detailed maps shown in this essay illustrate a few of those stories, although again in a very abbreviated form.
Detailed location map for Yellowstone River-North Fork Shoshone River drainage divide area
Figure 2: Detailed location map Yellowstone River-North Fork Shoshone River drainage divide area. United States Geological Survey map digitally presented using National Geographic Society TOPO software.
Figure 2 provides a detailed location map for the Yellowstone River–North Fork Shoshone River drainage divide area east of Yellowstone National Park. A region in eastern Yellowstone National Park is shown with the red-brown color in the west half of figure 2. The Yellowstone River originates in the Thorofare Plateau area south and east of the southeast corner of Yellowstone National Park and flows in a north-northwest direction to Yellowstone Lake. North of Yellowstone Lake the Yellowstone River flows in a northwest direction from Fishing Village (at north end of the lake) to Canyon Junction and then in a northeast and north direction to the north edge of figure 2. The Lamar River (labeled "River" in figure 2) originates near the Yellowstone National Park easternmost extension (near Lamar Mountain) and flows in a north, southwest, and west direction before turning to flow in a north-northwest direction to the north edge of figure 2 and joins the Yellowstone River north of figure 2. Note numerous southwest oriented streams flowing to the north-northwest oriented Yellowstone River and to Yellowstone Lake as barbed tributaries. These barbed tributaries provide evidence the Yellowstone River valley south of Yellowstone Lake probably originated as a south oriented drainage route and was subsequently reversed to form the north-northwest drainage route seen today. The highway from Yellowstone Lake to Buffalo Bill Reservoir (west of Cody, Wyoming) follows the North Fork Shoshone River valley from Pahaska to Buffalo Bill Reservoir where the east oriented North Fork is joined by the northeast oriented South Fork to form the northeast oriented Shoshone River, which then flows to the northeast corner of figure 2. East oriented tributaries forming the North Fork include Jones Creek, Crow Creek, and Middle Creek. Northeast oriented Eagle Creek joins the North Fork east of Pahaska. Note how the southwest and south oriented North Fork Shoshone River headwaters flow to the southeast and east oriented North Fork Shoshone River at Pahaska and drain the region directly south of the Lamar River headwaters. While not obvious from figure 2 the Yellowstone River-North Fork Shoshone River drainage divide is the crest of the high Absaroka Mountains and is today a high mountain region. In spite of this mountain topography many of the North Fork Shoshone River tributaries are aligned with Yellowstone River tributaries, but flow in opposite directions. For example the northeast oriented Eagle Creek drainage route is aligned with an unnamed southwest oriented Yellowstone River tributary (Howell Creek). This alignment suggests the drainage routes originated as a southwest oriented flood flow channel that was dismembered as crustal warping raised the Absaroka Mountains and as headward erosion of the deep northeast oriented Eagle Creek valley beheaded the south-southwest oriented flood flow. This and other similar alignments are illustrated and discussed in the topographic maps illustrated below.
Pelican Creek-Jones Creek drainage divide area
Figure 3: Pelican Creek-Jones Creek drainage divide area. United States Geological Survey map digitally presented using National Geographic Society TOPO software.
Figure 3 provides a topographic map of the Pelican Creek-Jones Creek drainage divide area. The northeast shore of Yellowstone Lake can be seen just east of the south half of the west edge of figure 3. The Yellowstone River-North Fork Shoshone River drainage divide serves as the Yellowstone National Park eastern boundary in figure 3 and is shown with a labeled dashed line extending from near the northeast corner of figure 3 to the south center edge of figure 3. Pelican Creek is the south, southwest, and west oriented stream (labeled "Creek") flowing from the north edge of figure 3 (west half) to the west center edge of figure 3 and west of figure 3 turns to flow in a south direction to enter Yellowstone Lake. Raven Creek is the southwest oriented Pelican Creek tributary flowing from the north center edge of figure 3. Mist Creek is a northeast oriented stream flowing from Mist Creek Pass to the north edge of figure 3 (east of center) and south and east of Mist Creek is northeast and north-northeast oriented Cold Creek. North of figure 3 Mist Creek joins Cold Creek, which turns to flow in a north direction to the north-northwest oriented Lamar River. East oriented streams east of the Park boundary flow to the east edge of figure 3 and from north to south these east oriented streams are Bear, Jones, and Crow Creeks. East of figure 3 Bear, Jones, and Crow Creeks flow to the south oriented North Fork Shoshone River headwaters, which then turn to flow in a southeast and east direction at Pahaska. Note how several labeled and unlabeled passes cross the Yellowstone River-North Fork Shoshone River drainage divide. These include Crow Creek Pass, which links the east oriented Crow Creek valley with the southwest and west oriented Cub Creek valley, and Jones Pass, which links the east oriented Jones Creek valley with the southwest and northwest oriented Bear Creek valley. The map contour interval for figure 3 is 50 meters and, depending on where one measures, these passes are from 100 to 300 meters deep. Even deeper unlabeled passes can be seen near Stonecup Lake linking the Jones Creek headwaters with a northwest oriented Pelican Creek tributary and near Frost Lake linking the southeast oriented Bear Creek valley with a north oriented Cold Creek tributary valley. The pass near Stonecup Lake has an elevation of between 2800 and 2850 meters. Mount Chittenden to the west rises to 3103 meters while Cathedral Peak to the northeast rises to 3280 meters suggesting the pass is at least 250 meters deep. The pass near Frost Lake also has an elevation of between 2800 and 2850 meters. Pyramid Peak to the west rises to 3201 meters while unnamed peaks east of figure 3 rise to more than 3250 meters suggesting the pass is at least 350 meters deep. These passes are water-eroded features and were eroded by southeast and east oriented flood flow moving to the actively eroding east oriented North Fork Shoshone River valley and its tributary valleys. Headward erosion of a deeper south oriented valley on the present day north oriented Yellowstone River alignment beheaded and reversed flood routes across Crow and Jones Passes and perhaps the Stonecup Lake pass while southeast oriented flood flow continued to move across the pass near Frost Lakes. Flood flow across the Frost Lake pass ended when flood flow in the Yellowstone National Park area was beheaded and reversed to create the north oriented Yellowstone River drainage system, which included the north-northwest oriented Lamar River drainage basin.
Detailed map of Lamar River-Bear Creek drainage divide area
Figure 4: Detailed topographic map of the Lamar River-Bear Creek drainage divide area. United States Geological Survey map digitally presented using National Geographic Society TOPO software.
Figure 4 provides a detailed topographic map of the Lamar River-Bear Creek drainage divide area seen in less detail in figure 3 above. The Lamar River-North Fork Shoshone River drainage divide serves as the Yellowstone National Park eastern boundary and is shown with well-marked line extending from the east edge of figure 4 (north half) to the south edge of figure 4 (west half). Areas north and west of the drainage divide drain to the north-northwest oriented Lamar River. Areas south and east of the drainage divide drain to the North Fork Shoshone River. Bear Creek flows in a northeast direction across section 12 (just east of the Park boundary) and then turns to flow in an east and southeast direction to the south edge of figure 4 (near southeast corner) and south of figure 4 joins the south, southeast, and east oriented North Fork Shoshone River. The unnamed southeast oriented stream flowing to the east edge of figure 4 flows to southwest oriented North Fork Shoshone River, which then turns to flow in a south direction before turning again to flow in a southeast and east direction. The north oriented stream originating west of Frost Lake north of figure 4 joins Cold Creek, which then flows in a north direction to join the north-northwest oriented Lamar River. Note how a well-defined north-to-south oriented through valley (near center of figure 4) links the north-oriented stream valley with the southeast oriented Bear Creek valley. The map contour interval for figure 4 is 40 feet and the through valley floor elevation at the drainage divide is between 9200 and 9240 feet. Pyramid Peak to the east rises to more than 10,480 feet. The Lamar River-North Fork Shoshone River drainage divide near the east edge of figure 4 rises to more than 10,440 feet and further east rises even higher. These elevations suggest the north-to-south oriented through valley is approximately 1200 feet deep. The through valley is a water-eroded valley and was eroded by south oriented flood flow moving from the present day north-northwest oriented Lamar River valley to the southeast oriented Bear Creek valley and then to the south oriented North Fork Shoshone River valley. Headward erosion of the deep east and southeast oriented North Fork Shoshone River probably captured the south oriented flood flow and diverted the floodwaters in an east direction to deeper south oriented flood flow channels in the present day north oriented Big Horn Basin. Reversals of flood flow in the Big Horn Basin were followed by reversals of flood flow in the Yellowstone National Park region and created the north oriented drainage systems seen today and the Lamar River-North Fork Shoshone River drainage divide seen in figure 4.
Clear Creek-Middle Creek drainage divide area
Figure 5: Clear Creek-Middle Creek drainage divide area. United States Geological Survey map digitally presented using National Geographic Society TOPO software.
Figure 5 illustrates the Clear Creek-Middle Creek drainage divide area south and slightly east of figure 3 and includes a significant overlap area with figure 3. The Yellowstone National Park east boundary is shown with a dashed line and extends in a south-southeast direction from the north edge of figure 5 (west of center) to Hoyt Peak (just north of highway near center of figure 5) and then in an east-northeast direction almost to the east edge of figure 5, but turns in a south direction as a straight line before turning in a southwest direction to Plenty Coups Peak (near south edge of figure 5, east of center). North of Hoyt Peak the Yellowstone River-North Fork Shoshone River drainage divide serves as the Yellowstone National Park boundary. South of Hoyt Peak the drainage divide continues in a south and southeast direction to Sylvan Pass, Top Notch Peak, Mount Langford, and Plenty Coups Peak. The Yellowstone Lake eastern shore is seen along the west edge of figure 5. From south to north named streams flowing to Yellowstone Lake are southwest oriented Columbine Creek; northwest, southwest, and northwest oriented Clear Creek; and southwest oriented Cub Creek. East oriented streams flowing to the east edge of figure 5 are North Fork Shoshone River tributaries and from south to north are east oriented Cabin Creek, east-northeast oriented Middle Creek, and east oriented Crow Creek. Sylvan Pass near the center of figure 5 is a through valley linking the northwest and southwest oriented Clear Creek valley with the east-northeast oriented Middle Creek valley, which east of figure 5 drains to the southeast and east oriented North Fork Shoshone River valley (see figure 2). The map contour for figure 5 is 50 meters and the Sylvan Pass elevation at the drainage divide is between 2550 and 2600 meters. Hoyt Peak to the north rises to more than 3150 meters and Top Notch Peak to the south rises to more 3121 meters suggesting Sylvan Pass is approximately 500 meters deep. Sylvan Pass is a water-eroded valley and was eroded by southeast oriented flood flow moving from the present day north oriented Yellowstone River drainage basin to the east-northeast oriented Middle Creek valley, which had eroded headward from the actively eroding North Fork Shoshone River valley to capture south and southeast oriented flood flow moving across the region. At that time floodwaters were flowing on a surface equivalent in elevations to the highest points now seen in figure 5, although the region has probably been significantly uplifted since.
Detailed map of Clear Creek-Middle Creek drainage divide area
Figure 6: Detailed map of Clear Creek-Middle Creek drainage divide area. United States Geological Survey map digitally presented using National Geographic Society TOPO software.
Figure 6 illustrates a detailed topographic map of the Clear Creek-Middle Creek drainage divide area seen in less detail in figure 5. The Yellowstone National Park east boundary is the well-marked line extending in a southeast and south direction from the north edge of figure 6 (west of center) to Avalanche Peak and Hoyt Peak and then in a northeast and east direction to near the northeast corner of figure 6. Sylvan Pass is near the center of figure 6. Clear Creek flows in a northwest and east direction from Sylvan Pass to the west edge of figure 6 (near northwest corner). Top Notch Peak is located south and west of Sylvan Pass and Middle Creek originates on the southeast side of Top Notch Creek as a southeast oriented stream, but then turns to flow in a northeast and east-northeast direction to the east edge of figure 6 (north of center). A southeast oriented tributary flows from near Sylvan Pass to northeast oriented Middle Creek. Sylvan Pass is an impressive through valley eroded across the Absaroka Mountains crest ridge. The map contour interval for figure 6 is 40 feet and the Sylvan Pass elevation is between 8500 and 8550 feet. Hoyt Peak to the north rises to more than 10,480 feet while Top Notch Peak to the south rises to more than 10,200 feet suggesting Sylvan Pass is approximately 1650 feet deep. While lakes and cirques seen in figure 6 (north side of Top Notch Peak) suggest the region was glaciated at some point in time the Sylvan Pass through valley is a water-eroded feature and was eroded by southeast oriented flood flow moving to the northeast and east-northeast oriented Middle Creek valley, which had eroded headward from the North Fork Shoshone River valley, and which had probably eroded headward from deep south oriented flood flow channels in the present day north oriented Big Horn Basin. The Sylvan Pass through valley was eroded as crustal warping raised the Absaroka Range and for a time the concentrated flood flow was able to erode the water gap deeper and deeper. However headward erosion of what was probably a south oriented flood flow channel on the present day north oriented Yellowstone River alignment beheaded and reversed the southeast oriented flood flow channel to create the northwest and west oriented Clear Creek drainage route and to create the Clear Creek-Middle Creek drainage divide at Sylvan Pass. Glaciation of the region occurred after all melt water flood flow across the region had ended.
Middle Creek-Beaverdam Creek drainage divide area
Figure 7: Middle Creek-Beaverdam Creek drainage divide area. United States Geological Survey map digitally presented using National Geographic Society TOPO software.
Figure 7 illustrates the Middle Creek-Beaverdam Creek drainage divide area south and east of figure 5 and includes a significant overlap area with figure 5. The Yellowstone National Park east boundary is shown with a dashed line extending in a southwest direction from the north edge of figure 7 (near northeast corner) to Plenty Coups Peak and then in a south direction to Atkins Peak, Mount Schultz, and the south edge of figure 7. The Yellowstone Lake Southeast Arm straddles the west edge of figure 7. The north-northwest oriented Yellowstone River enters the Southeast Arm south of figure 7. Mount Langford is located near the center of figure 7. Beaverdam Creek originates on the southeast side of Mount Langford and flows in a south and southwest direction to enter the Yellowstone Lake Southeast Arm just south of the south edge of figure 7. Rocky Creek is a south-southwest oriented Beaverdam Creek tributary. Sylvan Pass is located near the north center edge of figure 7 and Top Notch Peak is located south and west of Sylvan Pass. Middle Creek originates south and east of Top Notch Peak and flows in a northeast direction to the north edge of figure 7 (east half). A north-northeast oriented Middle Creek tributary originates east of Mount Langford and joins Middle Creek near the north edge of figure 7 (east half). Note how there is a deep notch, gap, or pass between Mount Langford and Plenty Coups Peak linking the north-northeast oriented Middle Creek tributary valley with the south and southwest oriented Beaverdam Creek valley. The map contour interval for figure 7 is 50 meters and the pass elevation is between 2950 and 3000 meters. Mount Langford rises to more than 3250 meters and Plenty Coups Peak rises to 3334 meters suggesting the pass is at least 325 meters deep. While located today on what is a high mountain ridge the pass is a remnant of what was once a water-eroded valley and was eroded by south-southwest oriented flood flow moving to a south oriented flood flow channel on the present day north oriented Yellowstone River alignment. Headward erosion of the much deeper northeast oriented Middle Creek valley from the North Fork Shoshone River valley beheaded and reversed the south-southwest oriented flood flow channel to create the north-northeast oriented Middle Creek tributary drainage route and to create the Middle Creek-Beaverdam Creek drainage divide.
Detailed map of Middle Creek-Beaverdam Creek drainage divide area
Figure 8: Detailed map of Middle Creek-Beaverdam Creek drainage divide area. United States Geological Survey map digitally presented using National Geographic Society TOPO software.
Figure 8 illustrates a detailed topographic map of the Middle Creek-Beaverdam Creek drainage divide area seen in less detail in figure 7. The Yellowstone National Park eastern boundary is shown with a well-marked line in the east half of figure 8. Beaverdam Creek originates near the center of figure 8 and flows in a south direction to the south edge of figure 8 (west of center). The north-northeast oriented stream flowing to the north edge of figure 8 (east of center) is a Middle Creek tributary. Note the gap or pass linking the north-northeast oriented Middle Creek tributary valley with the south oriented Beaverdam Creek valley. Mount Langford is to the northwest of the pass and Plenty Coups Peak is to the southeast. The map contour interval for figure 8 is 40 feet and the pass elevation is between 9680 and 9720 feet. Mount Langford reaches an elevation of more than 10,760 feet while Plenty Coups Peak reaches an elevation of 10,940 feet suggesting the pass is approximately 1100 feet deep. The northeast side of the pass appears to be a cirque suggesting glaciation has altered valley shapes. What is important to remember is the valleys seen in figure 8 were eroded by water and any glacial erosion occurred after all flood flow across the region in figure 8 had ended. The pass was eroded by south-southwest oriented flood flow moving from the present day north-northeast oriented Middle Creek tributary valley alignment to the south and southwest oriented Beaverdam Creek valley and then to a south oriented flood flow channel on the present day north oriented Yellowstone River alignment. At that time south oriented floodwaters were eroding diverging and converging flood flow channels into a surface equivalent in elevation to the high mountain ridges seen in figure 8. Headward erosion of the much deeper northeast oriented Middle Creek valley (north of figure 8) beheaded the south-southwest oriented flood flow channel between Mount Langford and Plenty Coups Peak. Floodwaters on the north-northeast end of the flood flow channel reversed flow direction to create the north-northeast oriented Middle Creek tributary drainage route.
Eagle Creek-Howell Creek drainage divide area
Figure 9: Eagle Creek-Howell Creek drainage divide area. United States Geological Survey map digitally presented using National Geographic Society TOPO software.
Figure 9 illustrates the Eagle Creek-Howell Creek drainage divide area east and south of the figure 7 and includes a significant overlap area with figure 7. The Yellowstone National Park eastern boundary is shown with a dashed line that extends in a south direction from the north edge of figure 9 (west half) to Mount Humphreys and then in an east direction to Eagle Peak and finally in a south direction (as a straight line) to the south center edge of figure 9, The Yellowstone River flows in a north-northwest direction across the southwest corner of figure 9. Beaverdam Creek flows in a southwest direction across the northwest corner of figure 9. Mountain Creek flows in a west-southwest direction from the southeast quadrant of figure 9 to join the Yellowstone River south of figure 9. Howell Creek is a south and south-southwest oriented tributary originating near Eagle Pass and joining Mountain Creek near the south edge of figure 9 (west half). Eagle Creek is a northeast oriented stream originating north of Eagle Peak and flowing to the north center edge of figure 9. North of figure 9 Eagle Creek continues to flow in a northeast direction to join a southeast oriented segment of the North Fork Shoshone River. Note the northeast and north oriented Eagle Creek tributary located north of Eagle Pass. Eagle Pass is a north-to-south oriented through valley linking the north oriented Eagle Creek tributary valley with the south and south-southwest oriented Howell Creek valley. The map contour interval for figure 9 is 50 meters and the Eagle Pass elevation is between 2900 and 2950 meters. Eagle Peak to the west rises to 3462 meters and the unnamed mountain to the east rises to 3299 meters suggesting that Eagle Pass is at least 350 meters deep. Eagle Pass is another example of a water-eroded valley, which was eroded by a south oriented flood flow channel moving floodwaters to a south oriented flood flow channel on the present day north oriented Yellowstone River alignment. Headward erosion of the much deeper northeast oriented Eagle Creek valley from the southeast oriented North Fork Shoshone River valley beheaded the south oriented flood flow channel. Floodwaters on the north end of the beheaded flood flow channel reversed flow direction to create the north oriented Eagle Creek tributary drainage route. Prior to eroding the south-southwest oriented flood flow channel floodwaters flowed on a surface equivalent in elevation to the highest points seen in figure 9, although the region has probably been significantly uplifted by ice sheet related crustal warping since that time.
Detailed map of Eagle Creek-Howell Creek drainage divide area
Figure 10: Detailed map of Eagle Creek-Howell Creek drainage divide area. United States Geological Survey map digitally presented using National Geographic Society TOPO software.
Figure 10 provides a detailed topographic map of the Eagle Creek-Howell Creek drainage divide area seen in less detail in figure 9. Eagle Pass is located near the center of figure 10. The Yellowstone National Park east boundary extends in an east-southeast and east-northeast direction from Mount Humphreys near the west edge of figure 10 to Eagle Pass and then in a south direction to the south center edge of figure 10. Howell Creek is the south oriented stream originating near Eagle Pass and flowing to the south center edge of figure 10. The northeast oriented stream in section 36 near the northwest corner of figure 10 is Eagle Creek, which north of figure 10 joins the southeast and east oriented North Fork Shoshone River. The northeast oriented stream originating in section 6 and flowing to the north center edge of figure 10 north of figure 10 flows in a north direction to join northeast oriented Eagle Creek. Note the west and northwest oriented tributary to that northeast and north oriented Eagle Creek tributary in sections 4 and 5, which is located directly north of Eagle Pass. While it is a significant climb from either direction to reach Eagle Pass, Eagle Pass is a remnant of what was once a north-to-south oriented flood flow channel moving floodwaters to a south oriented flood flow channel on the present day north oriented Yellowstone River alignment. The map contour interval for figure 10 is 40 feet and the Eagle Pass elevation is 9628 feet. Eagle Peak to the west rises to more than 11,320 feet and the unnamed mountain to the east rises to 11,497 feet. These elevations suggest Eagle Pass is as much as 1,690 feet deep. Small ice masses can be seen on north sides of the higher mountain peaks and north facing valley heads have cirque shapes suggesting glaciation, which occurred after flood flow across the region had ended, has further modified valleys heads, especially north facing valley heads. Valleys seen in figure 10 are water-eroded valleys and while glaciation has steepened valley walls the primary erosion agent that produced the landscape seen in figure 10 was water with immense south oriented melt water floods responsible for much of the erosion.
Additional information and sources of maps studied
This essay has provided only a sample of the detailed topographic map evidence supporting the flood erosion interpretation. Many additional illustrations could be provided. Readers are encouraged to look at mosaics of detailed topographic maps to see the abundance of available data. Maps used in this study were created and published by the United States Geologic Survey and can be obtained directly from the United States Geological Survey and/or from dealers offering United States Geological Survey maps. Hard copy maps can also be observed at United States Geological Survey map depositories, which are located throughout the United States and elsewhere. Illustrations used here were created using National Geographic Society TOPO software and digital map data. TOPO software and map data can be obtained from the National Geographic Society and/or dealers offering National Geographic Society digital map data.
Absaroka Range · Landform origins · Sylvan Pass · topographic map interpretation
Links to open access published papers related to this website
Philadelphia, PA landform descriptions are found at phillylandforms.info
Evidence for south-oriented drainage in the present day Gallatin, Madison, and Jefferson River drainage basins
Evidence investigated that led to the Missouri River drainage basin landform origins research project
South Platte River-Plum Creek drainage divide area landform origins in the Rampart Range, Colorado, USA
Cherry Creek-Plum Creek drainage divide area landform origins in Douglas County, Colorado, USA
Kiowa Creek-Bijou Creek drainage divide area landform origins on the Colorado Piedmont, USA
Bijou Creek-Beaver Creek drainage divide area landform origins in Adams, Arapahoe, Elbert, and Washington Counties, Colorado, USA
Beaver Creek-Arikaree River drainage divide area landform origins in Arapahoe, Elbert, Lincoln, and Washington Counties, Colorado, USA
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Evolution of the New Hampshire Drainage Network
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Hazel Branch valley in Linn County, Kansas
Information about web site author, Eric Clausen
South Fork Flathead River-Blackfoot River drainage divide area landform origins, western Montana, USA
The Method of Multiple Working Hypotheses: Is It A Chimera?
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redpajama_set_name: RedPajamaCommonCrawl


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text:
Q: How to Use Hive parsing multiple nested JSON arrays {
    "base": {
        "code": "xm",
        "name": "project"
    },
    "list": [{
        "ACode": "cp1",
        "AName": "Product1",
        "BList": [{
            "BCode": "gn1",
            "BName": "Feature1"
        }, {
            "BCode": "gn2",
            "BName": "Feature2"
        }]
    }, {
        "ACode": "cp2",
        "AName": "Product2",
        "BList": [{
            "BCode": "gn1",
            "BName": "Feature1"
        }]
    }]
}

JSON like this, want to get this
| code | name    | ACode | Aname    | Bcode | Bname    |
| ---- | ------- | ----- | -------- | ----- | -------- |
| xm   | project | cp1   | Product1 | gn1   | Feature1 |
| xm   | project | cp1   | Product1 | gn2   | Feature2 |
| xm   | project | cp2   | Product2 | gn1   | Feature1 |

I try Use this
SELECT
    code
  , name
  , get_json_object(t.list, '$.[*].ACode')          AS ACode
  , get_json_object(t.list, '$.[*].AName')          AS AName
  , get_json_object(t.list, '$.[*].BList[*].BCode') AS BCode
  , get_json_object(t.list, '$.[*].BList[*].BName') AS BName
FROM
    (
        SELECT
            get_json_object(t.value, '$.base.code') AS code
          , get_json_object(t.value, '$.base.name') AS name
          , get_json_object(t.value, '$.list')      AS list
        FROM
            (
                SELECT
                    '{"base":{"code":"xm","name":"project"},"list":[{"ACode":"cp1","AName":"Product1","BList":[{"BCode":"gn1","BName":"Feature1"},{"BCode":"gn2","BName":"Feature2"}]},{"ACode":"cp2","AName":"Product2","BList":[{"BCode":"gn1","BName":"Feature1"}]}]}' as value
            )
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get this
xm  project ["cp1","cp2"]   ["Product1","Product2"] ["gn1","gn2","gn1"] ["Feature1","Feature2","Feature1"]

BUT I find it will generate six row.Seems to have a Cartesian product.
And I try use split(string, "\},\{"),but this will split the inner layer at the same time.SO I hope to get help.

A: I solve it!!
SELECT
    code
  , name
  , ai.ACode
  , ai.AName
  , p.BCode
  , p.BName
FROM
    (
        SELECT
            get_json_object(t.value, '$.base.code') AS code
          , get_json_object(t.value, '$.base.name') AS name
          , get_json_object(t.value, '$.list')      AS list
        FROM
            (
                SELECT
                    '{"base":{"code":"xm","name":"project"},"list":[{"ACode":"cp1","AName":"Product1","BList":[{"BCode":"gn1","BName":"Feature1"},{"BCode":"gn2","BName":"Feature2"}]},{"ACode":"cp2","AName":"Product2","BList":[{"BCode":"gn1","BName":"Feature1"}]}]}' as value
            )
            t
    )
    t
    lateral view explode(split(regexp_replace(regexp_extract(list,'^\\[(.+)\\]$',1),'\\}\\]\\}\\,\\{', '\\}\\]\\}\\|\\|\\{'),'\\|\\|')) list as a
    lateral view json_tuple(a,'ACode','AName','BList') ai as ACode
  , AName
  , BList
  lateral view explode(split(regexp_replace(regexp_extract(BList,'^\\[(.+)\\]$',1),'\\}\\,\\{', '\\}\\|\\|\\{'),'\\|\\|')) BList as b
  lateral view json_tuple(b,'BCode','BName') p as BCode
  , BName


text:
Legend of Loreley Siren of the River Rhine
Rhinemaidens by Hans Makart (Wikimedia Commons)
The Loreley is a siren legend of the River Rhine in Germany. She is a ghostly vision with a heart grown as stone cold as the waters flowing below her. The Loreley is also the name of a rock bluff over looking the river, it was named for this siren.
The sound of the gurgling water echoes off the rocks which line the shores of the Rhine giving this section of the river an enchanted feeling. The gurgling river creates a humming sound which when heard can be mistaken for that of a soft ghostly voice. It is an essential part of the mystic behind the legend of the Loreley (Lorelei). She is often depicted as a siren or mermaid and there is a tale that is told of her.
It is a tale which has with the passing of time grown into a legend. It is a tale of a ghostly woman who beckons sailors to come closer to her and to the rocks on which sits. If they do they are doomed to lose their ship to the craggy coast and their lives to the cold waters that surround it.
I was in early elementary school when my new grade teacher singled me out from the rest of the class. I was always very shy so having a teacher direct their attention to me was an event that I dreaded.
I remember him looking at me and my feeling very dismayed knowing what was to follow. His steadfast look in my direction let me know in no uncertain terms that he was going to focus all his attention directly on me.
He asked if my name was Lorelei and when I nodded, he asked if I had heard the legend of the Loreley. I shook my head no and he began to tell myself and my fellow students the magical tale of the river Rhine and of a beautiful woman who would later transform into a ghostly siren there. It is funny because I do not recall the teacher's name or exactly what grade I was in at the time. I was quite impressed with the tale however and loved the thought that I might somehow have a magical ghostly mermaid lady connected to me.
The rock hill known as the Loreley sits on the east shore of the Rhine river within the Rhine Gorge.The Rhine Gorge is a section of the river which is historically recognized as a treacherous waterway to maneuver through. The channel is lined with rocky hills and the waters hide dangerous rocks and strong undercurrents.
The Rhine's history of luring men to their death by capsizing their ships was forever romanticized when in 1801 Clemens Brentano wrote "Zu Bacharach am Rheine" the ballad of the Lore Ley. The River Rhine was forever romanticized by the image of a siren forever destined to call from the bluffs to the passing ships.
The Haunting Song of the Loreley
Clemens Brentano's Zu Bacharach am Rheine told a poetic tale of the river Rhine involving a woman named Lore Ley. Lore Ley is a beautiful woman, but when betrayed by her lover she extracts her revenge on all men. She is accused by the clergy of bewitching and murdering
men and as such she is sentenced to death.
As Lore Ley is lead away she beseeches to once more look down over the river Rhine. Allowed to climb the rock to look down upon the river she throws herself down into the Rhine and to her death.
Her tale is one of enchantment, romance, disappointment, and heartbreak. The sound of the waters of the Rhine echoing throughout the gorge increase the romantic mystical theme of the lovely siren Lore Ley singing upon the rocks. From that day onward the rocks echo her song.
Heinrich Heine Poem: Die Loreley. Heinrich Heine brings the image of Lorelei to life even further within his poem Die Loreley. In her death Loreley becomes a ghostly siren and within her death lie the death of many men. She sits high upon the rock softly singing a song which lures passing seamen toward her and into the unyielding rock upon which she sits. Siren, ghost, or mermaid, the Loreley through time becomes a legend which flows as deep as the Rhine itself.
The Ballad of the Lore Ley by Clemens Brentano
Her name is forever destined to remain connected to this river and the rock which bears her name. From the barren rock of Loreley the image of a woman is formed. From the haunted waters where ships of yesteryear pass her voice rings out into the sky over the river Rhine.
Heinrich Heine: The Poem of Loreley Translated
Her portrayal is one of beauty seduction and sorrow. Enticing as a creature of the deep oceans can be the folklore behind her being lives on today. The tale of the legendary Loreley has also remained with me since I first heard of her.
Lorelei is the English spelling of Loreley (German) and today both names carry the meaning of siren, mermaid, or water nymph. This popular television show The Gilmore Girls increased the awareness and use of this name.
The Rhine River and the Loreley rocks are quite a popular destination for tourists. A simple Google search will bear you more information on travel and tours to this destination.
As a child I lived within walking distance to a lake so my siblings and I would often go there to swim throughout the summer months. After learning the tale of the siren of the River Rhine I would pretend to be a mermaid as we swam at that local beach. A mermaid seemed a friendlier image than that of a woman who fell to her death into a watery grave. Today in my mind's image I now see the ghostly girl the legend actually portrays online you will also find me by my screen name Ladymermaid.
Magical Glass Potion Bottles and Jars
Tiny Fairy Elf Party Dessert Treats
The Legend of the Black Unicorn
Old Wives Tales and Inspirational Old Country Proverbs


This collection of gowns explore couture and gave an opportunity to practice craftsmanship. Inspired by extravagant and heavily embellished bridal trends. Made using luxe silk, French lace and Swarovski materials.
Thank you for your inquiry. I'll be in touch shortly to discuss how we can bring you idea to life!


TThe UPAREL custom arm sleeves are made of tough non-woven antibacterial 83% polyester and 17% spandex material yet have a thick high quality feel. They have excellent sun protective qualities. The only USA manufacturer to offer Certified UPF 50+ protection.
LOVE the sleeves! My son received them as a birthday gift and he wore them the next day to a game. Most of his teammates have now ordered and they love them, too! Great gift!


text:
13 health systems opening hospitals
Posted on September 9, 2020 by henrykotula	• Posted in Capital Expenditure, Health System, Hospital, Hospital Construction, Hospital Expansion	• Leave a comment
https://www.beckershospitalreview.com/capital/13-health-systems-opening-hospitals.html?utm_medium=email
The following health systems have opened hospitals, advanced proposals to build them or announced plans for them in the last two weeks:
1. UT Health San Antonio to build $400M+ hospital
University of Texas Health San Antonio plans to build a 144-bed specialty and research hospital.
2. Conway Medical Center plans new 50-bed hospital
Conway (S.C.) Medical Center plans to build a hospital in South Carolina's Carolina Forest area, the organization announced Sept. 8.
3. Tidelands Health plans new hospital in South Carolina
Tidelands Health plans to build a hospital in South Carolina's Horry County, the Georgetown, S.C.-based organization said Sept. 8.
4. Atrium Health fights to open hospital in North Carolina county
Charlotte, N.C.-based Atrium Health is still fighting to open a $147 million, 30-bed hospital in Mecklenburg County.
5. Abrazo Health to open Arizona hospital this fall
Phoenix-based Abrazo Health plans to open a hospital in Surprise, Ariz., this fall.
6. McLaren Healthcare boosts funding by $150M for Lansing health campus
After increasing its investment by $150 million, Grand Blanc, Mich.-based McLaren Health Care said it will spend $600 million on its new health campus in the state's capital of Lansing. The new campus will include a new 262-bed McLaren Orthopedic Hospital.
7. Ballad Health plans 2021 reopening for hospital closed 7 years
Johnson City, Tenn.-based Ballad Health plans to reopen a hospital in Virginia that has been closed since October 2013.
8. Ascension reopens Florida hospital ravaged by hurricane in 2018
Ascension Sacred Heart has reopened its hospital in Panama City, Fla., about two years after Hurricane Michael damaged the facility.
9. MarinHealth opens $535M hospital
MarinHealth in Greenbrae, Calif., has opened a new $535 million hospital.
10. HonorHealth to open 70-bed hospital in September
HonorHealth plans to open a 70-bed Phoenix hospital in September.
11. St. Louis University Hospital opens $550M hospital
SSM Health St. Louis University Hospital opened its $550 million facility to patients. The new facility is called the Grand New SSM Health St. Louis University Hospital.
12. Ascension Saint Thomas can build hospital in Tennessee county, beating out Vanderbilt
Ascension Saint Thomas has won approval to build a hospital in Tennesee's Murfreesboro County, beating out a proposal from Vanderbilt University Medical Center.
13. Trustees approve OSU's $1.79B hospital
Ohio State University's board of trustees unanimously approved this week its new $1.79 billion inpatient hospital.
← First Sign of Civilization
Where furloughs stand at 92 hospitals, health systems →


Atta girl, California. This week Governor Brown signed a law making it illegal for children under age 18 to use tanning beds. No doctor note, no parent note, or any other paperwork necessary. It's a real ban and it's the strictest law in our nation. While 30 some other states have laws limiting indoor tanning use by minors, no other state has banned the use of indoor tanning for minors entirely. Although many professional groups have urged for a tanning bed ban, it has taken some time to get this trend started. Only 49 states to go.
A study back in 2002 surveyed kids from all 50 states to determine (risky) behaviors increasing the odds of skin cancer. The findings were fairly grim. Over 80% of teens reported having a sunburn in the prior year and over 1/3 of them had experienced 3 or more burns. We know one bad sunburn in childhood dramatically increases the likelihood of a skin cancer later in life. Further, one out of every 4 teen girls between 15 and 18 years of age reported indoor tanning bed use. And worse, as teens get older, they use indoor tanning more: the rate of indoor tanning doubles between age 12 and 17. The reality is, teens won't prioritize skin health so you may have to help. Some suggest using the argument for preserving beauty ("Sun damage gives you wrinkles") is more powerful than using the argument for preserving life ("Sun damage may give you a skin cancer that kills you").
Thing is, 65% of melanoma skin cancers can be attributed to UV radiation exposure from the sun. Further, we know early excessive sun exposure in life (even at young ages) dramatically increases the likelihood of developing a skin cancer later in life. A burn early in life can have lasting effects.
Using a tanning bed increases your risk for developing a melanoma by 75% in one study. Although other organizations like the WHO quote a one time tanning bed-use as a 15% increase risk of developing a melanoma. A 15% increase risk of getting a cancer with one 30-minute activity! Tell your teen.
Over 2 million teens use indoor tanning in the US every year.
Consequently, melanoma rates are rising here, increasing each and every year since 1992 when I left high school. Young, white women are leading the charge for the increase in our numbers. Although melanoma is only the 5th most common cancer, it is by far the deadliest.
The UVA radiation from at tanning bed is 10-15 times stronger than that from the sun in the middle of the day! UV radiation (UVR) is harmful because damages skin and evidence supports a strong causal relationship between sunlight exposure and skin cancer. In particular, there is a heightened risk of melanoma for those with increased childhood sun-exposure. UVR is made up of UVA and UVB waves of light. Remember this: UVB light is the light that Burns, and UVA light is the light that causes your skin to Age (wrinkle).
You don't have to live in California to live the good life. Make your home a little more California today. Ban indoor-tanning for your children forever.
Dear WSS, Thank you for posting this amazing and moving video, and sharing the great news. May there never be the word "sunburn" in another child's life. Well, we can dream, can't we?
What an amazing video. I hope and pray that this and others like it will make it to all the children and parents out there and that they will really listen. Cancer of any type is nothing to mess with and melanomas are one of the worse. USE your sunscreen, it can save your life.
Why has the medical community not connected the vitamin D deficiency with the shift to a low-fat diet? The article also mentions a few other vitamins that are usually low, along with D. Interestingly, these are all fat-soluable vitamins. Add to this our increase in diabetes over the past 30 years. When you eat fats and proteins along with sugars and carbs, they keep your blood sugar regulated. In you have low-fat milk in your sugar-laden breakfast cereal, you've got a problem. Good fats (not trans fats) turn into our hormones, so why recommend lowering them? As soon as we rid ourselves of the low-fat mentality, we'll see an overall improvement in our health.


A "dump truck" in rafting occurs when all of the passengers in a raft are "dumped" out during a rapid. There are a few points to consider in determining what constitutes an actual "dump truck", the main factor being whether all of the paddlers fall out of the raft. If even one paddler stays in the raft, then it is not considered a "dump truck". Another key question is whether the raft guide falls out of the raft as well as the guests. Some rafters consider it to be a true "dump truck" only if the guide stays in the raft, much like the driver of a dump truck who empties his cargo, but obviously remains in the truck while doing so. Others consider it a "dump truck" only when the guide also falls out along with his guests, leaving the raft completely empty.
Check out this series of photos of a "dump truck" where the guide falls out with their guests http://www.youtube.com/watch?v=zBFK-LD4_fU and another where the guide dumps out his entire crew, but stays in the raft http://www.youtube.com/watch?v=BwqdUHPeJw8. This final video claims to be a "dump truck" in the title, but is not because all paddlers do not leave the raft http://www.youtube.com/watch?v=vZfssXKOn6o.


RSVP for นิทรรศการ "เมื่อเวลาทำหน้าที่อย่างซื่อสัตย์เสมอ" to add comments!
"When Time Always Carries Its Duty Faithfully"
Resentments bring sorrow every time they come up; deeply planted memories gloom the mind. All these plights are constructed by us who create cages of rage to enclose ourselves. When time silently progresses, enduringly; the rage and pain have silted.
Reflecting from episodes in her life is a didactic mechanism to guide mindfulness. Jiratchaya decides to confront her plights by stepping into the discomfort feelings planted deep in her heart and emancipates herself from enraged subconscious. By letting go and forgiving oneself and others, the mind lighten and calmed.
The artist relays these feelings through her new exhibition "When Time Always Carries Its Duty Faithfully".
Dark black lines and weights cutting through white pure spaces in different shapes and forms will allow viewers to unfurl their imagination alongside the artist on the liberation of emancipated mind.
Additionally, we would like to invite everyone to discuss with and congratulate the artist at the Opening Reception on Saturday 7th October 2017, from 6 pm to 9 pm.
• The exhibition is on view from: 7th October to 18th November 2017.
• Opening Reception : Saturday 7th October 2017 at 6 – 9 pm.


text:
using Atata;

namespace AtataSamples.SalesforceLightning
{
    using _ = ComboboxPage;

    [Url("lightning:combobox/example")]
    public class ComboboxPage : Page<_>
    {
        public enum Progress
        {
            New,
            InProgress,
            Finished
        }

        [FindByName("progress")]
        [CloseAlertBox(TriggerEvents.AfterSet)]
        public SLCombobox<_> StringBasedCombobox { get; private set; }

        [FindByName("progress")]
        [CloseAlertBox(TriggerEvents.AfterSet)]
        public SLCombobox<Progress, _> EnumBasedCombobox { get; private set; }

        protected override void OnInitCompleted() =>
            Find<Button<_>>(new FindByIdAttribute("onetrust-accept-btn-handler")).Click();
    }
}

redpajama_set_name: RedPajamaGithub


Merchandise will be shipped via U.S. Postal Service (USPS) 1st Class Mail (US only) 2-3 business days of completed purchase. You will receive a Shipment Confirmation email once your order has shipped containing your tracking number(s). The tracking number will be active within 24 hours. Please note that packages take an average of 2-5 days to arrive to destination in continental US. We are not responsible for postal service delays.
At the moment we ship in the USA and Canada ship only. All parcels are shipped via USPS and Canada Postal Service. Recycled Glass Jewelry is not responsible for any customs and taxes applied to your order. All fees imposed during or after shipping are the responsibility of the customer (tariffs, taxes, etc.).
Our priority when preparing items to be sent in the mail is the safety of the jewelry, but we also pay special attention to the aesthetics of the packaging so you can be sure you will receive a lovely package.
"return to sender" policies. If the package comes back to me due to an incorrect address that the customer wrote in, they will be responsible for reshipment.
These items are produced for adults and not designed to be worn or used by children. These items are not toys nor are they meant for children. They are made of glass and some of these items may have sharp points.
Due to the handcrafted nature of the items, dimensions in the product descriptions should be regarded as approximate.
All the pieces are handmade, There are never tow identical. That's what makes them unique! These are small batch productions of the items displayed in the photos. Please allow slight variations from the photographed item are inevitable due to the nature of this work each design is hand-painted in between the layers of glass.
Are these products for children?
NO. These items are produced for adults and not designed to be worn or used by children. These items are not toys nor are they meant for children. They are made of glass and some of these items may have sharp points.
In general, the glass is fairly sturdy due to the thickness and the heating processes done during beadmaking. For example, if you drop a small necklace or earrings on a rug, they usually will not break. However, if you drop them on concrete they may break or get chipped.
Fusing glass involves cutting glass and stacking it together and firing the glass in a kiln to about 1475 degrees until it fuses or joins together in one piece. This process takes about 12 to 14 hours, including heating and cool down. Additional aspects of fusing glass include grinding to smooth rough edges and polishing the glass.
Can I order another pendant exactly like the one I have?
We can use the same colors and make a similar shape, but the pieces will never come out exactly the same. Every piece is unique!
All of our fused glass items are individually handmade. While every effort is made to replicate the style and color of the piece you have chosen, slight variations may be present. These elements add to the unique beauty that makes each piece a one-of-a-kind treasure made just for you! This should be considered part of what makes your purchase special.
Are the dimensions listed in the product descriptions exact?
Please contact us regarding any wholesale inquiries.
What is the best way to contact Carolina?
We respond promptly to all inquiries via email. You can contact us at karopor@Yahoo.com.


text:
Mason is a town in Hillsborough County, New Hampshire, United States. The population was 1,448 at the 2020 census. Mason, together with Wilton, is home to Russell-Abbott State Forest.

History
Mason was first known as "Number One", the easternmost in a line of border towns including area allotted to the Province of New Hampshire after its border with neighboring Massachusetts was fixed in 1739. The town was granted its own charter in 1749 by colonial governor Benning Wentworth, and in 1768 his nephew, Governor John Wentworth, named it in honor of New Hampshire's founder, Captain John Mason, who along with Sir Ferdinando Gorges had been granted the territory in 1622 by the Council of New England. In 1629 the land grant was split between the two proprietors, with Gorges retaining the eastern portion of the territory (present-day Maine), and Mason holding the patent with title to the land that became New Hampshire.

Greenville was set off from Mason in 1872.

Near the center of Mason is the boyhood home of Samuel Wilson, the meat supplier who is believed to have inspired the Uncle Sam character. The private house is today identified by a state historical marker. Another prominent local figure was Elizabeth Orton Jones, an author, illustrator and teacher better known as "Twig". Jones is noted for her recording of town history and her dedication to Andy's Summer Playhouse, a renowned youth theater founded in Mason. Pickity Place, a local cottage built in 1759 by Ebenezer Blood, was the model for the grandmother's house in Jones' 1948 illustrated version of "Little Red Riding Hood". Pickity Place was created by David and Judith Walter.

Geography
According to the United States Census Bureau, the town has a total area of , of which  are water, comprising 0.23% of the town. Mason is drained to the east by Spaulding Brook, Gould Mill Brook, and Wallace Brook, tributaries of the Nissitissit River, and to the south by Walker Brook, a tributary of the Squannacook River in Massachusetts. The Nissitissit and Squannacook are both tributaries of the Nashua River, and the entire town is thereby part of the Merrimack River watershed. The town's highest point is  above sea level, on an unnamed summit near the border with Greenville.

Mason is bordered by New Ipswich and Greenville to the west, Wilton to the north, Milford to the northeast, Brookline to the east, and Ashby, Massachusetts, and Townsend, Massachusetts, to the south.

The town is served by state routes 31, 123 and 124.

Adjacent municipalities
 Wilton, New Hampshire (north)
 Milford, New Hampshire (northeast)
 Brookline, New Hampshire (east)
 Townsend, Massachusetts (southeast)
 Ashby, Massachusetts (southwest)
 New Ipswich, New Hampshire (west)
 Greenville, New Hampshire (west)

Demographics

As of the census of 2000, there were 1,147 people, 433 households, and 328 families residing in the town.  The population density was 48.0 people per square mile (18.5/km2).  There were 455 housing units at an average density of 19.0 per square mile (7.4/km2).  The racial makeup of the town was 98.08% White, 0.17% African American, 0.09% Native American, 0.44% Asian, 0.44% Pacific Islander, and 0.78% from two or more races. Hispanic or Latino of any race were 0.96% of the population.

There were 433 households, out of which 31.9% had children under the age of 18 living with them, 65.8% were married couples living together, 5.5% had a female householder with no husband present, and 24.2% were non-families. 18.0% of all households were made up of individuals, and 6.2% had someone living alone who was 65 years of age or older.  The average household size was 2.65 and the average family size was 3.02.

In the town, the population was spread out, with 24.3% under the age of 18, 5.5% from 18 to 24, 33.0% from 25 to 44, 28.8% from 45 to 64, and 8.5% who were 65 years of age or older.  The median age was 40 years. For every 100 females, there were 106.3 males.  For every 100 females age 18 and over, there were 106.7 males.

The median income for a household in the town was $60,433, and the median income for a family was $61,908. Males had a median income of $43,558 versus $26,042 for females. The per capita income for the town was $28,503.  About 3.6% of families and 3.4% of the population were below the poverty line, including 3.3% of those under age 18 and 4.9% of those age 65 or over.

Town facilities

Mason is immediately north of the Massachusetts border, with the center of town about  from the state line. At the center of town are five public buildings: the library, elementary school, meetinghouse, church, and police station, all situated where Darling Hill, Old Ashby, Merriam Hill, Meetinghouse Hill and Valley roads meet. The students at the public middle and high school are tuitioned to Milford, which is northeast of Mason. Tto the west is Greenville, location of the shared post office. On Depot Road, less than a mile down the hill from town center, is the Volunteer Fire and EMS Department and Town Highway Department.

Notable people

 C. W. Anderson (1891–1971), author, illustrator
 John Boynton (1791–1868), founder of Worcester Polytechnic Institute
 F. Ross Holland, Jr. (1927–2005), historian; best known for his books about American lighthouses
 Elizabeth Orton Jones (1910–2005), children's book author and illustrator
 Samuel Wilson (1766–1854), meat-packer, legendary potential origin of "Uncle Sam"
 Walter A. Wood (1815–1892), US congressman

References

External links

 New Hampshire Economic and Labor Market Information Bureau Profile

Towns in Hillsborough County, New Hampshire
Populated places established in 1768
1768 establishments in New Hampshire
Towns in New Hampshire

redpajama_set_name: RedPajamaWikipedia


text:
Q: Append search query (ng-model) to JSON http.get request
I am looking to append a search query to a JSON http.get request and then display the order below when the data is received (previously I have accessed all orders)
I am using and assuming ng-model is the solution here, but I struggling to get a successful JSON call with my current code.
Search Page (List)
  <ion-header-bar class="bar-dark">

Order List

  </ion-header-bar>

              <input type="search" ng-model="query" placeholder="Search">

        <ion-content class="has-subheader">
          <ion-list>
            <ion-item ng-show="query" ng-repeat="order in orders | filter:query" class="item-thumbnail-left item-text-wrap"
            href="#/tab/list/{{order.bkor_user}}">

Production Name: {{order.bkev_name}}

Seatcount: {{order.bkor_seatcount}}

Order Subtotal: £{{order.bkor_subtotal}}

            </ion-item>
          </ion-list>
        </ion-content>

Controller
    .controller('ListController', ['$scope', '$http', '$state','$cordovaBluetoothSerial', '$window', '$location', function($scope, $http, $state, $cordovaBluetoothSerial, $window, $location) {
              $http.get('http://example.co.uk/bookingref/get/host/{{ query }}').success(function(data) {
                $scope.orders = data;
                $scope.query = query;
                //console.log($scope.orders);
                //console.log(JSON.stringify(config));
                $scope.whichorder = $state.params.aId;
                //console.log($scope.whichorder);

              })

I think I will also have to edit my ng-repeat too now that it is one single order rather than an array of order

A: You should append your parameter to string by concatenate it to URL string.
$http.get('http://example.co.uk/bookingref/get/host/'+ $scope.query)


Comfort and relaxation await you in Villa #207. This beautifully-decorated three-bedroom offers an oceanfront covered porch complete with furniture for taking in a gentle ocean breeze while drinking your morning coffee.
The Oak Island Beach Villas is an oceanfront condominium complex located along historic Caswell Beach that offers eleven oceanfront buildings as well as five buildings with an ocean view. Two- and three-bedroom, individually decorated units are available to accommodate the size of your family. The community boasts many amenities such as a centrally located pool in front of the 600-building, walkways to the beach through the community, outside showers at each building, ample parking, a recreation area, and designated grilling areas. For the golf lovers in your family, the Villas are conveniently located just across the street from the Oak Island Golf Course and Country Club.
Book directly with us for the best rates on Oak Island vacation rental homes.


text:
Consuming Vitamins and Fortified Foods May Be Too Much of a Good Thing
Roshni L. RountreeHoward University News Service
The dietary supplements millions of women across the nation depend on to fight against illness have the potential to cause harm if they are consumed in combination with some foods common in everyday diets.
Katherine Tallmadge, a registered dietician in Washington, D.C., advises her clients to take a multivitamin but to avoid the combination of a supplement and fortified foods which have been enhanced with vitamins and minerals.
As an example, Tallmadge said, drinking vitamin water fortified with calcium and consuming foods naturally rich in calcium such as diary products can lead to interference with the body's absorption of other minerals.
When there is too much calcium, other minerals like zinc and iron found in multivitamin supplements compete against each other. In this case, the body will not make the best use of one of the minerals due to the excessive amount of its competitor.
Another combination to be wary of is consuming multivitamins rich in Vitamin A while consuming foods rich in beta carotene.
A report published in May 2006 by the National Institutes of Health found that beta-carotene increased the risk of illness in healthy women and in women with already elevated health threats.
The body breaks beta carotene, which gives foods such as carrots and sweet potatoes their orange coloring, into Vitamin A. According to the NIH report, beta carotene in supplements caused an increase risk of stroke in healthy women. It also increased the risk of cardiovascular disease in women who smoke.
Vitamin A only, according to the report, created no increased risk of illness. However, in combination with beta carotene, Vitamin A resulted in increased deaths caused by lung cancer and cardiovascular disease.
The report acknowledged the evidence that calcium and Vitamin D produce stronger bones in women. Yet, it found that the intake of these two, above their approved maximum levels, may increase the risk of kidney stones.
Five years ago, the Centers for Disease Control estimated that 25 to 41% of women in the US. take a multivitamin at least four times a week.
Women who take multivitamins have come to their own conclusions about the supplements. Gloria Outlaw, 71, of Maryland, said she has been using a multivitamin since her mid-40s.
Outlaw uses a daily multivitamin specially made for women. She began to include the supplement in her diet because she hoped it would provide the nutrients that she was not receiving from her food.
"I hope that taking this multivitamin will give me a longer lifespan and that my body will be strong enough to fight off disease that may be detrimental to my health," Outlaw said. She said she would switch to another supplement if she discovered that the one she takes poses a threat to her health.
Though Outlaw is not dependent on her multivitamin, some women rely on the supplements to do more than fill in the gaps from their diets. Some women take a the supplements to fight against an illness they currently have.
Donna Waters, 45, has an autoimmune disease known as lupus, an illness in which the immune system loses its ability to differentiate between foreign substances and its own cell tissue. Therefore, it tends to fight itself.
Because of her disease, she depends on a multivitamin in order to better the abilities of her immune system.
"I take Centrum – Advanced Formula because I have lupus and with my weak immune system, doctors recommended a multivitamin," said Waters.
Waters explained that she could not see or feel a physical change within herself but her regular check-ups with her physician reveal levels of normalcy with her immune system.
"I think it's essential to take a multivitamin, especially in my case, but also just to keep up good health," Waters said.
Contact the writer: R0813Qt@aol.com
http://consensus.nih.gov/2006/2006MultivitaminMineralSOS028html.htm
Osteoporosis, Cancer Meds Linked to Jawbone Decay
Residents Are Mixed on Fenty's School Takeover Plan
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Shenishe Kelly
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Southwest Residents Stuck Between a Rock and Steel Girders
Courtney Edwards
Longtime Homeowners Near Nationals Ballpark Fight to Keep Their Property Amid the loud cranes and construction worker bellows, a 30-year Southwest resident gazes…
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Kandace Brown Howard University News Service
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Alison Brock
The room is dark. Neon lights illuminate images of bodiesin motion. Girls and guys move to the music, laughing andjoking, even cheering when the DJ…
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Caryn Grant
Multiple NBA, NFL and NHL Coaches Get the Axe When the Sacramento Kings gave Reggie Theus the boot Monday, they became the sixth NBA team to fire a head coach…
Keith A. Laing, Political Update Writer
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Keith A. Laing is a senior print journalism major, business administration minor, from Stone Mountain, Georgia.As an aspiring journalist, Keith has already completed…
Wheels When You Want Them
Zipcar Targets College Students by Adding More Convenient Locations The days of being unable to rent a car unless you're 25- years-old and being restricted…
Nonprofits Pinched as Gov't Shutdown Continues
The government shutdown is well into its second week and nonprofit organizations around the United States have been feeling its effects. More programs like Meals…
Apple Releases Two New iPod Models; Now Stands at the Top of the Game
With the new release of Apple's new iPod player, music junkies will be scrambling to the nearest Best Buy to get their fix on the hottest gadget to hit stores…
Youth Activism: What Happened to Kings Dream?
"...We must make the pledge that we shall always march ahead. Wecannot turn back. There are those who are asking the devotees ofcivil rights, 'When will you be…
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St Mary's Church in Rotherhithe has been associated with the history of London and its connections with the river Thames and its cemetery. The Watch House coffee shop gets its name from its use as house to watch the graveyard to prevent grave robbing. The inside of the café is cosy and comfortable with a nice display of fresh bakery and a selection of cakes and sandwiches. The staff is pleasant and attentive. There is no need to stay indoors as the surrounding garden and front tables allow to enjoy the best of the area and the German influence of the menu adds that extra touch needed for something special.
After a busy day, most of the bread is sold out.


This patient is a 40 year old woman who desired a tummy tuck to improve the appearance of her abdomen. A tummy tuck with liposuction to the illiac rolls was performed by Jaime Perez, M.D., a board certified plastic surgeon serving the Tampa Bay, Florida area. The patient is very happy with her results.