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by Rabeea Tahir & Shahan Zafar December 12,2017
By Rabeea Tahir & Shahan Zafar
Microsoft Stream Classic is a video content management system that is probably included in your Office 365 subscription, or should I say - was included. Microsoft Stream recently announced a new vision for Microsft Stream where the new version will make video a part of SharePoint. The idea is to have a system to centrally access all types of files - as opposed to having a separate video portal as in the case of the classic stream.
The change in vision for Microsoft Stream may be ideal for many - those that prefer all documents in one place as it makes it easy to share data and also ensure privacy and governance. However, certain features of the Classic Stream will be lost, for instance:
There's no option to manually upload a transcript or closed caption file.
There's no pre-encoding to enable ready playback for large video files.
The new Stream doesn't allow you to add quizzes or forms to videos.
There's more - Read in our blog on the New Microsoft Stream.
Nevertheless, for those that are looking for a video portal approach to managing and streaming their content, there are other options.
VIDIZMO, is one such platform that offers a YouTube-like portal to stream live and on-demand videos to internal or external audiences. It's packed with features that the new Stream doesn't offer such as AI-generated transcripts, transcoding, video embedding and more. it integrates with MS Teams and SharePoint, giving your users a choice - access video files separately through the VIDIZMO platform or along with other files through SharePoint.
Through VIDIZMO, you get access to added features on top of what the New Microsoft Stream offers in SharePoint. Click here to learn about additional features you get for video in SharePoint.
What is Microsoft Stream Classic?
What is the New Microsoft Stream?
What Microsoft Stream Does Not Offer?
Our Analysis: Where Microsoft Stream Stands
Microsoft Stream Classic is a corporate YouTube-like video platform that allows people in organizations to upload, share, manage, and view videos from a centralized video platform.
Microsoft first entered the enterprise video market in 2015 with the launch of Office 365 video, which has now converged into Stream. Despite its promise, the Classic Stream currently only offers an intelligent and password-protected enterprise YouTube, without several basic functionalities provided by most industry-recognized enterprise video platforms.
Microsoft Stream (Classic) provides the following product capabilities as part of Microsoft Office 365 enterprise subscription:
Video upload and (limited) metadata editing: Users can upload video files individually or in bulk. Once uploaded, the file owner can make changes to file name/ title, add a description, choose a thumbnail, assign hashtags or upload caption files.
Video Transcoding: All videos are optimized for playback on varying devices and bandwidth conditions through the video transcoding process.
Video playback on internal sites: Once the videos are automatically transcoded, users can watch the videos within the Stream portal. However, it must be noted that the classic Stream does not support external stakeholder access and only allows authorized active directory users to access the videos, whether they are embedded on other organizational sites or played within Microsoft Stream.
Video sharing within the organization: The Classic Stream allows video owners to share and assign videos to one or multiple channels, a custom group of viewers, or make the videos private. The video files can only be shared within the company via a link, email or an embed code, which displays the content on other organizational platforms.
Organizing videos: The Classic Stream enables users to create channels to organize videos by topics or other categories. Channel creation and content contribution can be restricted to an authorized list of users. Videos can also be organized in mini-group portals, only available to authorized group members. Groups also contain channels for further categorization of content. However, you can't create folders for simplification or add custom metadata (such as author name, shoot location etc.) to enable better filtering of videos.
Intelligent video search: As part of an upgraded premium plan, Microsoft Stream features a range of intelligent features that improve content searchability within the portal. All videos are supported with speech to text transcription, which becomes searchable text that helps users jump to any spoken word in the video. However, Stream doesn't offer face detection in a clickable timeline that shows every person who appears in the video.
Microsoft Stream Classic is an enterprise YouTube that only fulfills a few business video use cases in a password-protected cloud video storage solution with limited streaming capabilities.
Microsoft Stream Classic, however, has had a new vision and will be known as the New Microsoft Stream. Some of the features that were included in the new Microsoft Stream
The New Microsoft Stream will integrate video into OneDrive and SharePoint - essentially creating a centralized place to manage both documents and videos. The idea is to merge the strengths of the Classic Stream (video playback) with SharePoint (document management). For instance, in the classic Stream you couldn't share video files externally but now you can through SharePoint. It works the other way round as well. For instance, in SharePoint, Microsoft Teams' recordings weren't ingested into your folders, making it difficult to share and collaborate on. Now they are!
You can benefit from the following in the New Microsoft Stream:
Better organization of video as now you can categorize them neatly in folders.
Recorded MS Teams meetings will be automatically ingested into the Team SharePoint (or OneDrive folders for private meetings).
Share videos outside your organization through links.
Benefit from APIs to integrate your SharePoint videos with other applications.
Set custom retention policies for deleted video files.
However, you'll lose on the following Microsoft Stream Classic features:
Playback speed options will no longer be available.
Editable video transcripts in multiple languages won't be available.
Video files won't be pre-encoded so your users might struggle to watch them in low bandwidths or certain devices.
Can't add quizzes or forms to videos.
No options for easily embedding video files.
Organizations now have the option to use both the New Microsoft Stream or the Classic Stream. However, at some point (not clarified by Microsoft yet) organizations will have to migrate from the Classic Stream and it will be discontinued.
Microsoft Stream (Classic and New) lack a range of fundamental platform capabilities that are integral for most medium to large organizations employing video for critical business functions.
Over the years, many of Stream's lacking capabilities have become a standard requirement for most enterprise video platforms in the market. In fact, the capabilities mentioned in the Gartner Market Guide for Enterprise Video Content Management, are missing from Microsoft Stream.
VIDIZMO, recognized as a Challenger in Gartner Magic Quadrant for EVCM, contains all capabilities offered by Microsoft Stream and much more.
Following are 18 main video platform functionalities that are not available in Microsoft Stream:
No External Sharing or Viewing (Classic Stream)
Microsoft Stream does not offer external sharing or public viewing. Video use is no longer limited to a company's internal workforce, and this is where Microsoft Stream falls short. Organizations now increasingly need to give external access to partners, investors, third-party contributors and even customers, an option that is not available in Microsoft Stream since it only allows internal content viewing and sharing. This problem, however, is addressed in the New Stream.
However, video platforms like VIDIZMO can provide secure external stakeholder access to specific videos or dedicated portals for public access or viewing by specific third parties. For instance, VIDIZMO can share marketing videos on a company's website and social media channels for viewing by customers, prospects, etc. by making them available for public viewing. Similarly, any CEO broadcasts could also be sent to investors, partners or other stakeholders by giving them external viewing access.
Within external access too, VIDIZMO provides several options, ranging from YouTube-like public access, password-protected videos in end-to-end encrypted formats, or a dedicated external YouTube-like portal with third-party username and password credentials.
Learn more about Video Sharing in VIDIZMO.
Content Organization and Searchability (Classic Stream)
It's difficult to organize large amounts of videos in Microsoft Stream, with options to create channels but no folders. Moreover, Microsoft Stream offers very basic search features. You can only search by title and description. No filters, No tags!
This problem is addressed in the New Stream. However, a new problem has risen where the new Stream doesn't provide a portal or video gallery approach in SharePoint.
VIDIZMO, on the other hand, allows you to categorize your video files into playlists, collections or categories. You can also add tags to videos using AI, add any custom attributes of choice (Location, author name, instructor name etc.), search using transcripts, faces objects and much more. All of this helps you in better organizing video content as use increases.
Learn More About Search in VIDIZMO.
Platform branding, UI and feature customization
Most organizations today already use a large number of business and IT applications. The last thing employees want is yet another application with a new or non-familiar user interface. To resolve this, companies opt for white-labeled enterprise platforms like VIDIZMO that not only have the company's branding, but are also come with the company's domain name and other configurable platform settings. Not only does this prevent the platform from appearing as a separate disintegrated entity from the rest of the business applications, but it also improves and simplifies platform adoption across the company.
Here is what the VIDIZMO interface looks like as opposed to MS Stream:
While most enterprise video platforms come with customized branding and configuration options, Microsoft Stream only offers a standard, non-configurable interface without any corporate branding options. Additionally, Stream does not allow any types of configurations to platform features and functionalities, flexibility most enterprise video platforms like VIDIZMO offers to facilitate custom organizational requirements.
Learn More About VIDIZMO White-label VOD Platform.
Encoding profiles control and file format support
With encoding profiles, video and media producers can exercise a significant degree of control over encoding quality and other settings such as choice of software or hardware encoders, which may be pertinent for different types of video use. In both the Classic and New Microsoft Stream, admins can't configure encoding profiles to be created.
VIDIZMO gives users complete and granular control over their encoding video output quality, support formats, codecs, etc.
Additionally, since Stream exclusively uses Azure Media Services for encoding, it only supports a limited number and types of file formats to convert from as compared to the vast range of file formats supported by VIDIZMO. Due to its support for Azure Media Services and encoding.com as well as flexibility of integration with any encoding software, VIDIZMO provides the widest range of support for video file formats and encoding flexibility.
Support for CDN or third-party eCDN/ SDN
Typically, videos are streamed across content delivery networks (CDNs) such as Akamai, Azure, and Amazon Web Services or third-party eCDNs/ SDNs such as Hive or Kollective that enable video delivery to a geographically dispersed user base or to external users such as partners, customers or the to the public outside the corporate firewall. Currently, Microsoft Stream offers no support for Azure CDN or third party eCDNs, though it is on Stream's roadmap. In addition, videos hosted in Stream can only be shared with internal co-workers, not external stakeholders.
VIDIZMO, on the other hand, provides supports for all CDNs and third-party SDNs, while also provisioning VIDIZMO enterprise CDN (eCDN) for optimizing bandwidth and video delivery over enterprise networks. Because of this, VIDIZMO can be set up on a wide area network (WAN) with CDN and edge caching servers in the cloud, or a local area network with VIDIZMO eCDN and edge caching support on-premises for live an on-demand video streaming delivered to users in varying bandwidth conditions or in geographically dispersed locations.
Storage limitations
Microsoft Stream has certain quotas and limitations associated with some of its key features like video storage and video file size outlined here. Moreover, there are limits to the number of AD users that can be assigned to a video along with caps on group, channel and tenant size – all of which can be extremely limiting for medium to large organizations producing large volumes of video for distribution to a large user base. Moreover, firms in more regulated industries have data retention policies that require long-term content storage, which would become extremely problematic with Stream's storage constraints.
VIDIZMO imposes no such limits or quotas on its users as we provide an unlimited storage capacity for an infinitely scalable user base.
Flexibility and choice of deployment models
Microsoft Stream, a cloud-based platform, does not offer deployment options on-premises, or in private or hybrid cloud. This is an issue if you need to choose your cloud provider and datacenter location, due to compliance and security requirements. Moreover, you can't choose to store and stream videos on your on-premise datacenter.
VIDIZMO, on the other hand, provides the flexibility to choose where your data is stored and processed. You can choose your cloud provider (Azure, AWS and more) in commercial or government cloud, your data center location, and even choose to deploy on-premises or in a hybrid infrastructure. You can also get on VIDIZMO cloud as SaaS.
Video is boring when it just involves one-way communication. Videos require interactive content to engage audiences and enable collaboration. This involves adding surveys, handouts, comments, timed annotations to on-demand videos. In the case of live videos, you'd need live chat or QnA functionality as well to gather feedback from viewers.
Microsoft Stream (the new one) doesn't offer this functionality. VIDIZMO, on the other hand allows you to add quizzes to videos, forms and surveys, handouts and related files, annotations and much more.
Learn more about VIDIZMO interactive video.
Video analytics are vital to determine the ROI of video communication, analyze viewing behavior, and generate detailed reports of who watched what videos, when and how much. For trainers, video analytics are fundamental to gauge how trainees are engaging with the video content, when viewers typically stopped watching the videos, as well as user-specific data like which employees watched the videos, for how long, etc.
For corporate communication, business leaders need to assess how many people across the company attended the webcast, drop-off rates, etc. Additionally, the lack of analytics could also be an issue for networking teams who need analytics to monitor and resolve any quality of service (QoS) issues with the streamed video. While such insights are provisioned by most video platforms like VIDIZMO, Microsoft Stream currently only provides a simple count of how many times a video was watched and liked by viewers.
Integration with existing line of business applications
Microsoft Stream currently provides integration with Microsoft Office 365 tools such as SharePoint, Yammer, Teams, etc. (O365 integrations are also available in VIDIZMO) but it still lacks interoperability with other third-party software such as CMS like Jive, Drupal, etc., LMS such as Moodle and Blackboard, CRM solutions like Salesforce, or online meeting services such as WebEx, Go-To-Meeting, etc. The New Stream, however, will offer an API to integrate with other business applications.
VIDIZMO, on the other hand, provides integration with all line of business applications and IT systems, whose details can be found here.
Rich Video Player
The Classic Stream offered a rich video player with transcripts, people's timeline, playback speed controls, quality controls and captions. These features are to be replaced with the OneDrive player. On top of it, the OneDrive player has progressive playback.
VIDIZMO EnterpriseTube offers a rich HTML5 video player that you can embed on any site, and has annotations, editable transcripts, quality controls, playback speed options and more. You can even brand the player to include your colors and fonts. You can even choose what buttons to show on the player to restrict the actions audiences can perform (e.g., don't allow them to seek forward in your training videos)
Learn more VIDIZMO online video player.
Video editing and auto-generated transcript editing
Every video platform needs to have basic video editing functions to make recorded videos suitable for sharing or presentation to a wide set of audience. VIDIZMO, for instance, has in-built video editing features that allow users to trim videos, split them into clips, incorporate a title screen, or add a custom thumbnail, among other things. Microsoft Stream does not offer any of these essential video editing features except for the addition of a thumbnail. Additionally, VIDIZMO allows users with authorized access to edit automatically generated machine transcripts to attain greater accuracy of all video transcripts and closed captioning. Users can conveniently add or remove content from the transcripts directly from the transcription pane that runs alongside the video playback screen.
Support for non-video media assets
Video is a tremendously powerful media asset, but it is not the only one used by organizations today. Contemporary organizations use a wide range of rich media assets such as audios, images, PDFs, slides, infographics, SCORM content, etc. in combination with video for training, documentation-supported communication, marketing, and collaboration. Despite its name, video platforms like VIDIZMO support all types of video and non-video media so all of a company's digital media could be collectively stored, managed, shared, and viewed through one consolidated platform. Without this provision, organizations will have to invest in a separate tool for managing their long and growing list of non-video assets – which would be the case with Microsoft Stream as it does not provide support for non-video digital assets.
Video Embedding
Videos are not only meant to be shared internally, as these may need to be shared for marketing or public relations purposes. Hence, it's important to be able to embed videos on your website. The Classic and New Microsoft Stream, both don't offer easy options for embedding your videos
VIDIZMO, on the other hand, offers rich video embedding options to add videos to any internal or external site. You can enable authenticated embedding as well.
Learn more about video embedding in SharePoint.
Bulk editing of video settings
Video creators and editors typically make use of bulk editing of video settings to minimize time and efforts required to assign video settings, permissions, meta details, etc. For instance, in Stream, you'll need to delete every video individually as there is no option to select multiple videos and bulk delete them.
VIDIZMO, on the other hand, allows bulk editing of all videos being added to the platform where a range of settings or changes are applied to all video with a single click, instead of doing it manually for individual videos, which is especially impractical in case of bulk media upload. Microsoft Stream, however, does not support bulk editing and, therefore, requires the users to go through each video's settings individually.
Content ingestion tool & broad integrations support
Currently, Microsoft Stream does not have any content ingestion tool that allows for bulk upload or automatic upload of video files from watch folders, the way VIDIZMO does using its Publisher Tool. Stream only provides limited or partial support for integration with Skype for Business (on the roadmap) but still does not offer broader integrations with other live video sources such as WebEx or Go-To-Meeting or video conferencing tools like Cisco TelePresence or Polycom RealPresence. Video platforms like VIDIZMO, on the other hand, seamlessly integrates with such all such services and automatically captures live or on-demand videos and delivers them to any number of audience, and on any device, through the VIDIZMO portal.
Content moderation, time-based archival, & data retention policies.
Even though Microsoft Stream now employs some restrictions over who can create channels and upload content, it still lacks content moderation workflows for videos to go through a structured approval process before they're made available for viewing, which prevents unfiltered videos from hitting the portal. Similarly, most enterprise platforms also come equipped with basic governance features such automatic video archival after a given date or data retention of video files over an extended time period – all of which Stream lacks.
One of the hot suggestions for Microsoft Stream on Stream UserVoice, has been the ability to blur faces and other PII, for compliance purposes. Microsoft Stream lacks a tool that can automatically redact PII from videos, without needing to use separate software. VIDIZMO, on the other hand, provides such a tool that uses AI to make it convenient and speed up the process for you.
Learn More About Video Redaction
Microsoft Stream Pricing
MS Stream is included in Office 365 Enterprise subscriptions and these start at $8 per user and go over $20 per use user.
For Office 365 business users, Microsoft Stream is not included in the Business Premium or Business Essentials plans, and for others, it only offers varying levels of platform capabilities depending on plan subscriptions.
Microsoft Stream, on the surface, appears to be less costly than an enterprise video content management system. This brings down to one question that IT administrators would have; "Why pay for an additional enterprise video content management system when we already have Microsoft Stream bundled with our Office 365 subscription?". The answer is simple; Microsoft Stream will cost your in lost productivity, and also make it difficult for your large enterprise to meet compliance needs. Think about it, it's definitely an issue if you need to download a video and upload it on another platform, every time you need to redact PII within the video. The same goes for other limitations within Microsoft Stream.
With its current capabilities, Microsoft Stream offers a foundational enterprise YouTube product that can be useful for smaller organizations with fewer video use cases and limited video storage and distribution needs. However, with its existing capabilities, it is highly unlikely that Stream will be able to handle even slightly more advanced, not to mention the continuously evolving sophisticated video use cases now being demanded by organizations across all industries. Additionally, Stream video is only available to an organization's employees so it doesn't serve other key business stakeholders such as partners, customers, investors, etc., thereby only serving partial video communication and collaboration needs.
Enterprise video platforms like VIDIZMO, on the other hand, are capable of handling large-scale video needs for all video use cases, including customized industry-specific video uses. Additionally, VIDIZMO's video streaming platform is capable of managing any volume and all types of video and digital media content in a comprehensive platform that is accessible to internal employees and external users such as partners and customers, with varying levels of access rights and permissions. VIDIZMO is available in all deployment models in the cloud and on-premises and offers high interoperability with all different line of business applications and IT systems and well as high customizability to suit specific customer needs.
Even with some basic features on its roadmap, Microsoft Stream is far behind its competitors in a rapidly evolving enterprise video platform market with players like VIDIZMO that will always have a competitive advantage in terms of platform features and functionality, its breadth of use, and the number of customers and enterprise needs it can serve. Over time, even as Stream plays catch up in a fast-growing market, a video-focused vendor such as VIDIZMO that solely specializes in video streaming solutions will always have superior product features and functionalities coupled with continuous innovation and platform enhancements adapted and customized for changing customer needs.
To learn more about VIDIZMO video streaming capabilities or for inquiries regarding our pricing plans, contact us today or visit our website for details regarding our solutions and offerings.
Posted by Rabeea Tahir & Shahan Zafar
This article is written jointly by Shahan Zafar (Product Marketing Manager) and Rabeea Tahir (An Expert in Video Streaming Technologies).
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Lieutenant-Colonel Scott MacGregor, Commandant Infantry School; Sergeant Quincy Smith (3rd Battalion, Princess Patricia's Canadian Light Infantry), Top Candidate of the Basic Assault Pioneer course given in June 2018; Chief Warrant Officer Sylvain Isabelle, Regimental Sergeant Major, Infantry School. The Axe symbolizes a tradition for the Pioneers and is awarded to the Top Candidate. Photo: Corporal Roger Simard, Canadian Army Combat Training Centre. ©2018 DND/MDN Canada.
The Canadian Army has decided to reactivate the Assault Pioneers in an attempt to increase the lethality of its infantry units.
Known for their specialized training, different grooming standards (they are allowed to wear well-groomed beards), and their axes, Assault Pioneers are a mix of an infantryman and a combat engineer. Aside from the normal infantry tasks, they are trained in explosive breaching and other combat engineer skill sets.
Don't get me wrong; we'd plow through thousands of russians with our axes if the call came. Might even drop a few Hind's with them too.
This is just our way of saying we are way too ill equipped to have guns, so here is our 'Lumberjack Commando's'. We just package it up with a cute title. In reality, those guys want better coms, 300wm rifles, and better helo's.
Beards are not something special in the CAF. Once we complete training to deployable status, most can grow them. They do have regulations though about length, style, etc. Depending on what branch you serve in, you may not be allowed. Sailors at sea need to be clean shaven, and a beard is not ideal for when we use our gas masks, so infantry must shave before CBRN training and the gas hut.


Colleen Bauer, owner of Bakersfield-based Fairy Godmother Events, dresses as a 1920s flapper for the Padre Halloween Murder Mystery Party her company planned. Bauer is seeing more companies book murder mysteries for team building.
When Colleen Bauer started her Bakersfield event and wedding planning business, she had no idea that her fairy godmother would make her dreams come true.
A regional bank officer who was climbing the corporate ladder, Bauer had been organizing her company's events for years. It was a natural extension of growing up in a family of four girls and having a mother constantly planning parties.
But it was in 2009, when Bauer served as the chairwoman of the Bakersfield Women's Business Conference, that she was inspired by fellow board members and event partners to start her own event planning company. She chose Fairy Godmother as the company's name because it was what her niece, Elise, called her.
When a co-worker announced she was getting married in 2010, Bauer offered to plan the event as a wedding gift. Weddings were the start of Fairy Godmother's list of services that included such things as holiday and birthday parties.
As Bauer continued to work at the bank, rising to the level of senior vice president, her business grew.
Bauer has assembled a team that includes event producers, designers, marketing specialists, office assistants and even officiants, when needed. Although she continues to plan and execute some events, Bauer focuses on staffing and operating the business.
Her years of experience in the corporate world also has allowed her to expand services to helping businesses with grand openings, employee events, holiday parties, business dinners, client or employee appreciation events, incentive/award trips, company picnics, trade shows, sales training and annual meetings.
Bauer said she is seeing an increasing number of company officials opting to bring in an expert to take care of details.
She also is seeing planned themed events, such as "murder mysteries," used as elements of company team-building strategies.
"The first murder mystery we did was for a fundraiser, but since then, we have had several businesses book us for team building using these parties," she said, adding that solving a murder mystery is not only fun, it encourages employees who may not regularly interact to work together.
But as Bauer's Fairy Godmother grew, so did the need to improve the company's business operations. And for that, Bauer turned to the Small Business Development Center at California State University, Bakersfield.
Bauer encourages local entrepreneurs to seek the help of SBDC consultants.
"It's like having a mentor and business coach — someone pushing you and looking out for you; someone challenging you to be the very best you can be," she said.
The center at CSUB assists entrepreneurs and small-business owners in Kern, Inyo and Mono counties by providing free consulting, small business training and research. For more information, go to www.csub.edu/sbdc.


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Quantitative fluorescence in situ hybridization and its ability to predict bladder cancer recurrence and progression to muscle-invasive bladder cancer
Benjamin R. Kipp, Mihaela Tanasescu, Terry A. Else, Sandra C. Bryant, R. Jeffrey Karnes, Thomas J. Sebo, Kevin C. Halling
Fluorescence in situ hybridization (FISH) testing is used to detect bladder cancer in urine specimens. The purpose of this study was to determine whether there are associations between the percentage of chromosomally abnormal cells by FISH and time to bladder cancer recurrence and progression to metastasis. Clinical records were searched to identify patients with urine FISH results, history of non-invasive bladder cancer, and at least one follow-up pathological diagnosis. Covariates analyzed included age, gender, smoking status, treatment after FISH, cystoscopy result, and prior stage of bladder cancer. The percentage of abnormal cells (hazard ratio [HR] 1.03, 95% CI 1.02-1.03; P < 0.001), age (HR 1.02, 95% CI 1.00-1.03; P = 0.033), male gender (HR 0.60, 95% CI 0.41-0.87; P < 0.001), treatment (HR 0.37, 95% CI 0.25-0.55; P < 0.001), and history of TIS/T1-stage tumors (HR 1.66, 95% CI 1.23-2.24; P = 0.001) were significantly associated with time to cancer recurrence. Time to invasive cancer was significantly associated with the percentage of abnormal cells (HR 1.02, 95% CI 1.01, 1.03; P < 0.001), history of TIS/T1 tumor (HR 3.73, 95% CI 1.88, 7.38; P = 0.001), and treatment (HR 0.33, 95% CI 0.13, 0.83; P = 0.019), suggesting that the percentage of abnormal cells independently predicts cancer recurrence and progression to invasive disease in patients with a history of non-invasive bladder cancer.
Journal of Molecular Diagnostics
https://doi.org/10.2353/jmoldx.2009.080096
10.2353/jmoldx.2009.080096
Dive into the research topics of 'Quantitative fluorescence in situ hybridization and its ability to predict bladder cancer recurrence and progression to muscle-invasive bladder cancer'. Together they form a unique fingerprint.
Fluorescence In Situ Hybridization Medicine & Life Sciences 100%
Urinary Bladder Neoplasms Medicine & Life Sciences 94%
Aptitude Medicine & Life Sciences 67%
Muscles Medicine & Life Sciences 59%
Urine Medicine & Life Sciences 28%
Cystoscopy Medicine & Life Sciences 23%
Kipp, B. R., Tanasescu, M., Else, T. A., Bryant, S. C., Jeffrey Karnes, R., Sebo, T. J., & Halling, K. C. (2009). Quantitative fluorescence in situ hybridization and its ability to predict bladder cancer recurrence and progression to muscle-invasive bladder cancer. Journal of Molecular Diagnostics, 11(2), 148-154. https://doi.org/10.2353/jmoldx.2009.080096
Quantitative fluorescence in situ hybridization and its ability to predict bladder cancer recurrence and progression to muscle-invasive bladder cancer. / Kipp, Benjamin R.; Tanasescu, Mihaela; Else, Terry A. et al.
In: Journal of Molecular Diagnostics, Vol. 11, No. 2, 03.2009, p. 148-154.
Kipp, BR, Tanasescu, M, Else, TA, Bryant, SC, Jeffrey Karnes, R, Sebo, TJ & Halling, KC 2009, 'Quantitative fluorescence in situ hybridization and its ability to predict bladder cancer recurrence and progression to muscle-invasive bladder cancer', Journal of Molecular Diagnostics, vol. 11, no. 2, pp. 148-154. https://doi.org/10.2353/jmoldx.2009.080096
Kipp BR, Tanasescu M, Else TA, Bryant SC, Jeffrey Karnes R, Sebo TJ et al. Quantitative fluorescence in situ hybridization and its ability to predict bladder cancer recurrence and progression to muscle-invasive bladder cancer. Journal of Molecular Diagnostics. 2009 Mar;11(2):148-154. doi: 10.2353/jmoldx.2009.080096
Kipp, Benjamin R. ; Tanasescu, Mihaela ; Else, Terry A. et al. / Quantitative fluorescence in situ hybridization and its ability to predict bladder cancer recurrence and progression to muscle-invasive bladder cancer. In: Journal of Molecular Diagnostics. 2009 ; Vol. 11, No. 2. pp. 148-154.
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title = "Quantitative fluorescence in situ hybridization and its ability to predict bladder cancer recurrence and progression to muscle-invasive bladder cancer",
abstract = "Fluorescence in situ hybridization (FISH) testing is used to detect bladder cancer in urine specimens. The purpose of this study was to determine whether there are associations between the percentage of chromosomally abnormal cells by FISH and time to bladder cancer recurrence and progression to metastasis. Clinical records were searched to identify patients with urine FISH results, history of non-invasive bladder cancer, and at least one follow-up pathological diagnosis. Covariates analyzed included age, gender, smoking status, treatment after FISH, cystoscopy result, and prior stage of bladder cancer. The percentage of abnormal cells (hazard ratio [HR] 1.03, 95% CI 1.02-1.03; P < 0.001), age (HR 1.02, 95% CI 1.00-1.03; P = 0.033), male gender (HR 0.60, 95% CI 0.41-0.87; P < 0.001), treatment (HR 0.37, 95% CI 0.25-0.55; P < 0.001), and history of TIS/T1-stage tumors (HR 1.66, 95% CI 1.23-2.24; P = 0.001) were significantly associated with time to cancer recurrence. Time to invasive cancer was significantly associated with the percentage of abnormal cells (HR 1.02, 95% CI 1.01, 1.03; P < 0.001), history of TIS/T1 tumor (HR 3.73, 95% CI 1.88, 7.38; P = 0.001), and treatment (HR 0.33, 95% CI 0.13, 0.83; P = 0.019), suggesting that the percentage of abnormal cells independently predicts cancer recurrence and progression to invasive disease in patients with a history of non-invasive bladder cancer.",
author = "Kipp, {Benjamin R.} and Mihaela Tanasescu and Else, {Terry A.} and Bryant, {Sandra C.} and {Jeffrey Karnes}, R. and Sebo, {Thomas J.} and Halling, {Kevin C.}",
doi = "10.2353/jmoldx.2009.080096",
journal = "Journal of Molecular Diagnostics",
publisher = "Association of Molecular Pathology",
T1 - Quantitative fluorescence in situ hybridization and its ability to predict bladder cancer recurrence and progression to muscle-invasive bladder cancer
AU - Kipp, Benjamin R.
AU - Tanasescu, Mihaela
AU - Else, Terry A.
AU - Bryant, Sandra C.
AU - Jeffrey Karnes, R.
AU - Sebo, Thomas J.
AU - Halling, Kevin C.
N2 - Fluorescence in situ hybridization (FISH) testing is used to detect bladder cancer in urine specimens. The purpose of this study was to determine whether there are associations between the percentage of chromosomally abnormal cells by FISH and time to bladder cancer recurrence and progression to metastasis. Clinical records were searched to identify patients with urine FISH results, history of non-invasive bladder cancer, and at least one follow-up pathological diagnosis. Covariates analyzed included age, gender, smoking status, treatment after FISH, cystoscopy result, and prior stage of bladder cancer. The percentage of abnormal cells (hazard ratio [HR] 1.03, 95% CI 1.02-1.03; P < 0.001), age (HR 1.02, 95% CI 1.00-1.03; P = 0.033), male gender (HR 0.60, 95% CI 0.41-0.87; P < 0.001), treatment (HR 0.37, 95% CI 0.25-0.55; P < 0.001), and history of TIS/T1-stage tumors (HR 1.66, 95% CI 1.23-2.24; P = 0.001) were significantly associated with time to cancer recurrence. Time to invasive cancer was significantly associated with the percentage of abnormal cells (HR 1.02, 95% CI 1.01, 1.03; P < 0.001), history of TIS/T1 tumor (HR 3.73, 95% CI 1.88, 7.38; P = 0.001), and treatment (HR 0.33, 95% CI 0.13, 0.83; P = 0.019), suggesting that the percentage of abnormal cells independently predicts cancer recurrence and progression to invasive disease in patients with a history of non-invasive bladder cancer.
AB - Fluorescence in situ hybridization (FISH) testing is used to detect bladder cancer in urine specimens. The purpose of this study was to determine whether there are associations between the percentage of chromosomally abnormal cells by FISH and time to bladder cancer recurrence and progression to metastasis. Clinical records were searched to identify patients with urine FISH results, history of non-invasive bladder cancer, and at least one follow-up pathological diagnosis. Covariates analyzed included age, gender, smoking status, treatment after FISH, cystoscopy result, and prior stage of bladder cancer. The percentage of abnormal cells (hazard ratio [HR] 1.03, 95% CI 1.02-1.03; P < 0.001), age (HR 1.02, 95% CI 1.00-1.03; P = 0.033), male gender (HR 0.60, 95% CI 0.41-0.87; P < 0.001), treatment (HR 0.37, 95% CI 0.25-0.55; P < 0.001), and history of TIS/T1-stage tumors (HR 1.66, 95% CI 1.23-2.24; P = 0.001) were significantly associated with time to cancer recurrence. Time to invasive cancer was significantly associated with the percentage of abnormal cells (HR 1.02, 95% CI 1.01, 1.03; P < 0.001), history of TIS/T1 tumor (HR 3.73, 95% CI 1.88, 7.38; P = 0.001), and treatment (HR 0.33, 95% CI 0.13, 0.83; P = 0.019), suggesting that the percentage of abnormal cells independently predicts cancer recurrence and progression to invasive disease in patients with a history of non-invasive bladder cancer.
U2 - 10.2353/jmoldx.2009.080096
DO - 10.2353/jmoldx.2009.080096
JO - Journal of Molecular Diagnostics
JF - Journal of Molecular Diagnostics

redpajama_set_name: RedPajamaCommonCrawl


text:
The Rest of Spain
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is mount wrangell active
Wrangell has more snow and ice in its caldera than any other active volcano in the world. 1984 would be expected to have a longer recovery. Mount Wrangell, in Ahtna K'ełt'aeni or K'ełedi when erupting, is a massive shield volcano located in Wrangell-St. Elias National Park and Preserve in southeastern Alaska, United States. His ridiculous religious freedom legislation would be repealed and any religion denying science and thus endangering life and property would be banned. Like the "recursive volcano of Taal" in the Philippines: the island has a volcano: its caldera has a lake; on the lake there is a volcano, etc. If you study paleoclimatology then you realise cold is the enemy. Add your article. Jarvis was active at the same time but grew larger. During the winter and on cool summer mornings, it is not unusual to see a steam plume rising out of the vents situated in craters along the margin of the summit caldera. That is exactly what happened. It's even got a name. View is to the southeast. If our Aboriginal population were stupid enough to burn twice this area every year, they would have never have lasted 60,000 years on the land. The eastern lobe covering a part of Canada came later, in an eruption several times larger than the first one. The Wrangell mountains are further from the coast and one may expect a shallower angle of subduction. For shallow subduction the volcanoes will be at considerable distance, whilst for steeper subduction they are closer. This is the first part of the Wrangell post. It is still over 4 km tall but is now deeply eroded. This is a much older mountain chain, extending to the coast. Wrangell was founded by Russians as one of the oldest non-Native settlements in Alaska. By eye, and from what's shown, I would be tempted to suggest a quadratic would be a marginally better fit. After this quake, there are some reports of increasing smoke coming from the summit. It was built by a series of large lava flows from 600,000 to 200,000 years ago. The Pacific plate subducts along the entire Aleutian arc, but volcanic activity is not the same everywhere. Webcams. But people who deny the data will not be convinced until their own lives become badly affected, by which time it may be too late. The information in this post comes to a large extent from that highly recommended source. The Wrangell Mountains are build on an ancient volcanic history, which played an important part not only in the building of America, but in the evolution of the Earth. There are some similarities here with the formation of volcanic mares on the Moon. The most recent results I have seen have pushed the median up from 3.0C to 3.3C based on data that shows that low clouds contribute to warming. Most of Mauna Loa is covered by pahoehoe in Google Earth suggest slower decades / centruies / millenia long tube – lake feed eruptions is the norm for Mauna Loa. However, Grewink himself assigns it to the Andreanof Islands, and it is now usually assumed to refer to Great Sitkin. Experience has shown that any PM challenging the mines is out within months. The naming was a bit of a long-service award for his public career. The last of the gang of three is Mount Wrangell itself, which is the only currently active volcano in the Wrangell Volcanic Zone. (It's only weird because we haven't seen a lot of the stuff that it does before and the guys who study it have to jump through hoops to figure out what it's up to. Among these are the Wrangell mountains. Source: https://home.nps.gov/wrst/planyourvisit/upload/Mud%20volcanoes%20Updated%2012-3.pdf. Locally, however, strata of the same age have been affected by a late pulse of tectonism, during which they were faulted, contorted into tight symmetrical folds, or overridden by pre-Cenozoic baserocks along southwesterly dipping thrust faults. There is a river of about this name near Wrangell, and therefore this eruption was subsequently identified as Mount Wrangell. That is the current level of discussion: it is about model differences at the 10% level. Other people only reported the smoke. This consisted of … Both Jarvis and Tanada became inactive 1 million years ago. Obviously, these volcanoes are not near the subduction trench, but some distance down stream – how far depends on the angle of subduction. Higher elevations of the field above 5,000 ft (1,500 m) are almost entirely covered in glaciers and icefields, especially on the windward southern side of the ranges. At the point where the melt initiates, the newly formed magma begins to percolate upwards. But underneath runs a deeper history, and lies an older volcanic field. Anywhere else, mountains such as these would dominate the region. CO2 is a non issue if you understand chemistry. https://www.volcanocafe.org/building-the-wrangell-mountains/. Mount Wrangell [rang-guhl] was named after Russian Admiral Ferdinand von Wrangel (or Wrangell), governor of Russian America from 1830 to 1836. 2014, Geosphere, 10, 1020-1042. Mount St. Elias, the second highest point in both the United States and Canada. New post is up! Mount Drum, with Snider Peak on the right. Best! On a side note, I've got an idea for an article. Its height is impressive too. Or in other words Mauna Loa will not have accumulated an extraordinary amount of pressure. These are the main volcanoes of the Wrangell Volcanics. Chitina residents report that the eruption is spectacular, not to mention huge columns of black smoke." Photograph by D. Richter, U.S. Geological Survey, 1989. 14,006 ft. (4269 m) From formal English to slang. I see the battle not between science and religion but between science and industry. Wrangell Volcanic Field lies within the Wrangell Mountains of Alaska, but the field also extends eastwards into the neighboring Saint Elias Mountains Mount Wran. The stratovolcanoof Mount Churchillhas had the largest recent eruptions, with two large-magnitude explosive eruptions in the last 2,000 years that blanketed most of the Yukon with volcanic ash(the White River Ash). The precise depth depends on the temperature and how wet the subducted rock is. Wrangell. The eruption is mentioned in a book on the geology of Alaska by the Estonian mineralogist Constantin Grewink, and is a second-hand mention of an eruption from 'Chetchina'. Mount Wrangell's broad, gentle form is an excellent example of a shield volcano, in fact, it is the largest andesite shield volcano in North America. This is clearly a volcano with a serious temper. Tephra found in Greenland's ice has given us a precise date: this eruption happened in the winter of AD 853 (a date 50 years earlier is also in the literature but is now out of date). Downgraded to 5.9 after review. Wrangell . Received a strange email allegedly from Albert entitled "the last post" when you click on the link to get to the posting the link doesn't work. Very rough on the edges, but fun. Other countries have ripped out their Eucalyptus plantations because of the extraordinary fire risk they pose due to flammable oils in the leaves. Very interesting if you can get your hands on it. https://www.theguardian.com/australia-news/datablog/ng-interactive/2019/dec/07/how-big-are-the-fires-burning-on-the-east-coast-of-australia-interactive-map. They have the appearance of small shields. Alaska is a wonderland. Very interesting, https://www.livescience.com/hidden-impact-crater-laos.html. There was a wobble after August but it has gone back to the previous trend. The calderas collapse to over a kilometer in depth, but much of this is filed in with basaltic flows which probably come from the ring fault. (Obvious AvE reference). The mountain started to build up by 600,000 years ago. With a diameter of 30 km at 2000 m elevation, 900 cu km Mount Wrangell is one of the world's largest continental-margin volcanoes. Mount, an active volcano in SE Alaska, in the Wrangell Mountains. Mount Wrangell is the only volcano in the Wrangell Mountains that is currently active. No one can do science and at the same time have an agenda, pick one or do neither. Although no centers younger than late Miocene are known in Canada, the eruption of rhyolite pumice, White River Ash, from Mount Churchill near the head of Klutlan Glacier blanketed large areas of northwestern Canada with tephra some 2,000 years ago. I oppose all science deniers equally. Another explosion at Shishaldin is reported by AVO. So the good news is we are unlikely to enter the next glacial cycle for a couple thousand years unless a big volcano gives us a push. The bulk of the mountain was destroyed in an explosion that happened between 200,000 and 100,000 years ago. This was followed in a minute or so by another, which was recognized then as a tongue of flame issuing from the crater of the mountain. It turns out that they came not from the Wrangell Mountains but from the other half of the park, the St Elias Mountains. A bit in the Hell's canyon area too..-H/T Nick Zentner Central Washington University.. i don't have time to look it up on You Tube.. Couldn't that be shortsighted in some form or another from the climate extremists? The volcanoes grew on top of an already highly elevated range. Religion might be closed to hypothesis but science never should be, even if someone argues AGW is false, just review the claims without bias, and offer an official explanation, that's science. Description Images Maps Bibliography Reported Activity. The Wrangell mountains are a volcanic region, build up relatively recently by eruptions. Mud pit and a mildly interested tourist. In the alkali vs silica diagram basalt is at the bottom, so there is no classification for something with lower alkalis, even if it had no at all it would still be called tholeeitic basalt…. Source: USGS. WASW. The Australian fires are an absolute disaster for the locals and they need support, not denial. Does not serve us as a species. All the mountains here are volcanic, and almost all are impressively high. Looking forward to next part. I am quite surprised by the absence of volcanic eruptions in Iceland. These were two serious eruptions; the second eruption was large enough to cause the local population to migrate south and temporarily vacate the region. https://phys.org/news/2020-01-formation-huge-underwater-volcano-offshore.html, Formation of a huge underwater volcano offshore the Comoros. It is the park's only active volcano and occasionally steam plumes can be seen rising from its summit. https://res.mdpi.com/d_attachment/climate/climate-06-00062/article_deploy/climate-06-00062.pdf, https://www.researchgate.net/publication/276497853_Late_Twentieth-Century_Warming_and_Variations_in_Cloud_Cover. I saw that this morning. Home Landforms by first-level administrative country subdivision Landforms of the United States by state Mountain ranges of the United States by state Mountain ranges of Alaska Wrangell Mountains. If you center the interactive map on the following website on a city like Birmingham (UK), or Oxford, or Dusseldorf, or Kansas City; you can get an idea of the scale of the current Australian bush fires. The Wrangell-St. Elias National Park is the largest protected wilderness in the United States. All of the higher peaks are less than 5 million years old, since the rate of glacial erosion is very high in this region of extreme snowfall and cold temperatures. 14,006 feet (4,269 meters). There is more here than meets the eye. We had to divert around the north side of the Wrangells. Source: Preece et al. Impressive indeed The field includes the four highest volcanoes in the United States, Mount Bona, Mount Blackburn, Mount Sanford, and Mount Churchill, all of which exceed 15,000 ft (4,600 m) in elevation. A back channel item was mistakenly put on the site. Deserts have also decreased in area and forest are expanding despite our worst efforts in the tropics. The magma is basaltic although there are differences from normal subduction zones. The Canadian portion of the field is dominated by scattered remnants of upper Cenozoic subaerial lavas and pyroclastic rocks. It lost almost 90% of its ice between 1965 and 1984, at a time when the other craters showed no change in ice cover. Looking forward to the follow-up. The eruptions seem to come in bursts, voluminous when they happen, quiet at other times. Mount Wrangell has an impressive summit caldera which measures 4 by 6 km, filled with 1-km thick ice. Quiet as the grave since you wrote that.. Likely will be an eruption soon I have decided to convert to "scientific evangelism" and preach Hell and Damnation to the lot of them with the same monotonous and tortured frequency that I am forced to tolerate their incessant, logiphobic drivel. The volcanoes all grow as a shield, and develop a caldera at the end of their evolution. However, things are a bit more complex. Let's GO! SAMPLES. The discussion is now on climate sensitivity. 4,317 m) is the youngest and only active volcano in the Oligocene to Holocene-aged Wrangell volcanic field that extends from beyond the Alaska-Yukon border northwest through the Wrangell Mountains to the Copper River Basin. From the article: "Mount Blackburn is erupting again. He does videos. It was named after the US senator Joseph Blackburn, well-known in his time but now remembered only because of the mountain. https://pubs.geoscienceworld.org/ssa/bssa/article-abstract/doi/10.1785/0120190198/579967/A-Reassessment-of-the-Magnitude-of-the-1755-Lisbon?redirectedFrom=fulltext, This one was a surprise to me. I think about all one can say with confidence is that activity is increasing. Fascinating geology. The Positive feedback just isn't there, Here are peer review articles on the observed cloud forcing seen the the earth radiation budget experiment. Wrangell reported activity. Mount Wrangell: Type: Shield volcano with summit caldera: Most Recent Activity: March 26, 1930: Seismically Monitored: Yes: Color Code: GREEN: Alert Level: NORMAL: Elevation: 14163 ft (4317 m) Latitude: 62.00572° N: Longitude: 144.01935° W: Quadrangle: Gulkana Valdez McCarthy Nabesna : CAVW Number: 315020: Pronunciation: Sound file The Wrangell and adjacent Elias Mountains. We are currently facing a hard time as a civilization…. Der 4317 m hohe Berg liegt in den Wrangell Mountains. yeah, well ok, its not at all simple, as would be expected. I don't single out Christian fundamentalists. WTF! The 1 meter deep pits at their peaks produce warm muddy water and methane gas. Yet despite this additional forcing not accounted for by climate models, the observed warming is only half that predicted from CO2 alone. Or is Thoelitic Basalt result of very most partial melting possible in something thats classifyed as a basalt? I see them as victims, who were hijacked. When will Mauna Loa start go go alkaline? This time in the southern part. They are among the tallest volcanoes in the world not by their own effort, but because they grew on the shoulders of giants. DustDevil More than almost any other volcano on Earth. Over a more long term it is very complex though, caldera lenght over the last decades: And also the last 5 years which overlapps in 2015-2016 with the previous graph to show the full picture. "The Wrangellia Terrane". Yesterday's radar image of Anak Krakatau. Wrangel; Wrangell … This was a double one-off event. Two of the rim craters show a vapour column. After the caldera collapsed, the volcanic activity ceased. Betelgeuse has some really strange convection going on. It began with a granite intrusion 5 million years ago, which developed into volcanic eruptions a million years later. Thanks to the rotation of the West Coast- the Seven Davils of Idaho have a goodly chunk of Wrangellia Terraine in them. It is only just underneath the surface and clearly represents a recent event. There may have been a phreatomagmatic explosion but the doubt comes from the fact that he was 30 miles away. The volcanic activity in the Wrangell Volcanic Zone has over time also moved northwest, although at a rather slower rate of 10 km per million years or 1 cm per year. LOCALS and natives often think climbing is pointless and perverse. Situation has reversed and I think that throughout our lifetimes it is going to remain like that, it might still erupt a few times this century though. Wran•gell [[t]ˈræŋ gəl[/t]] n. geg Mount, an active volcano in SE Alaska, in the Wrangell Mountains. Mount Drum is 3,661 m (12,010 ft) high and was active between approximately 700,000 and 240,000 years ago. Here is a link to the official Australian Bureau of Meteorology/CSIRO 2018 State of the Climate Report. Ash at 9 km. The location of Wrangell–St. The end of the video footage shows two distinct dark areas on the rim that is normally snow-covered. Some smaller peaks are not included, and it is conceivable that some further, minor eruption centres were buried under the developing shields. Interesting. The current long dormancy has some obvious reasons, first that the 1984 eruption reduced pressure significantly visible as a decrease in caldera distance, while the 1975 eruption had a comparatively small effect. Around 3.4 million years ago the 5-km wide caldera collapsed. Can anyone tell me how many words that should be? I did not pick this video for any specific reason. As it was covered with snow when the mountain was next seen, about the last of September, it seems probable that the bare area was due to material thrown out by the volcano." Another report from 1899 mentions an eruptive plume and a lava stream, although there is no confirmation of any lava. But there is no indication for this. n Mount Wrangell a mountain in S Alaska, in the W Wrangell Mountains. The next eruption coud be rather large in lava volume as it have sleept for a while… I remember my last trip to Fairbanks (Fire season 1992) in a DC7-due to weather. The shield rises over 12,000 feet (3,700 m) above the Copper River to its southwest. A 50-cm thick layer of white ash can be found in areas surrounding the Wrangell Mountains. Is there any basalt type that is result of larger partial melting than Thoelitic Basalt? The shield rises over 12,000 feet (3,700 m) above the Copper River to its southwest. The Alaska Volcano Observatory (AVO) receives several reports per year from pilots and local residents who observe larger than normal steam clouds over the summit. Along the caldera rim are three further smaller craters, imaginatively called: Mount Wrangell Crater, North Crater, and East Crater. Hey, its Alaska. In spite of frequent puffs of steam, geologists tell us that Wrangell is showing no signs of erupting any time soon. See more ideas about wrangell, alaska, national parks. Mount Wrangell, in Ahtna K'ełt'aeni or K'ełedi when erupting, is a massive shield volcano located in Wrangell-St. Elias National Park and Preserve in southeastern Alaska, United States. just saying there are a lot of excellent scientists in my religion….. they don't have to be exclusive of each other. This crater has significant ground heat. Since that time, the activity has moved around, building one mountain after another but rarely more than one at a time. The two pyroclastic flows together amounted to a 50km3 eruption. A doubling of CO2 cause 3.7W/m2 of warming. Summit caldera of Mount Wrangell, with the rim craters. Apart from the human costs to life and property, over half a billion animals are believed to have been killed already and several species are likely to become extinct. The caldera length increase fits a straight line for most of the past year. Its volume is over 220 cubic Map Display List Display. Of course Pleistocene rocks are buried under miles of lava flow rock now .. Mauna Loa and Kilauea are alternating dominance over the hotspot, for example Mauna Loa was dominant from 1840 to 1950 when it remained frequently active and very productive. In Australia, the exceptional influence of the coal mines decides on the government. They have said that for years it has been impossible to do this because it was too hot and dry to do this safely at any time. However, apart from this one angry spray, I shall refrain from further flaming on this location. The longest Mauna Loa slow tube eruptions lasted 1100 years in holocene I think. Mount Wrangell is the only active volcano in the park, as all the other volcanoes have officially been declared dormant. Mount Wrangell is an ice-covered volcano, having last erupted in 1907. He likes to take things apart and explain them.. https://www.youtube.com/watch?v=ZZjnbl1apeY. The field is named for Mount Wrangell, a massive shield volcano which has been active historically. You will find papers from this time about, for instance, the date in the year that a certain bird would lay eggs, and whether this was getting earlier in the year: if so, this would indicate a significant environmental change. The last and presumably final eruption was between 125,000 and 150,000 years ago. Wrangell — /rang geuhl/, n. Mount, an active volcano in SE Alaska, in the Wrangell Mountains. With their specially developed seismological methods, the researchers are reconstructing the partial emptying of one of the deepest and largest active magma reservoirs ever discovered in the upper mantle. I cannot get enough of these kinds of posts; never heard of before yet such interesting, much wow. The youngest lava flows are about 50,000 years old. It have erupted "large eruptions" 33 times since 1840. Webicorders. The volcanoes of the western Wrangell Mountains are less than 5 million years old with the youngest lava flows are probably as young as 50,000 years ago. Mount Hickman. Thanks, Albert, for another great post. This has nothing to do with falling caldera roof though, its the opposite way round! The current Mount Drum is only one side of the original mountain; the other side is Snider Peak. Fortunately we have a couple hundred years hopefully till the next 1ky bond solar cooling and the catastrophic cooling of the little ice age we are recovering from seems to have been due to the conjunction of the 2.4k bray solar cycle and a 1.5k oceanic cycle. Very extreme weather patterns unfolding. The Wrangell Mountains take up about a fifth of the park. Of course we are still testing predictions: that never stops. * * * … Universalium. High on the snow-covered flank, a gray-colored swath extends from a high point that we identify as the west caldera rim near Mount Wrangell Crater. Very productive volcano. Maybe Betelgeuse, one of the sky brightest stars (but now strangely dimming) will explode as a supernova before any Icelandic eruption happens. Mauna Loa is one of the most active volcanoes on the planet. Here, they live in the shadow of other, better known mountains. East of its current summit is a caldera 4 by 3 km across: this is likely the source of the ash, and probably the location of its summit before these events. So far an area of 32,400 square miles, or 83,915.60 square km, or 25.5 million acres, or 10,319,484 hectares has burned this year and summer has only just begun. No need for rewilding here – it is wild enough to begin with! Mauna Loa either does spectacular Icelandic style rift eruptions. but nothing prepared me for looking UP a these massive giants… that same trip I fortunate to get Denali in a good photo-cloud free.. Fred Beckey. The following headline account of an eruption from Mount Wrangell appeared in the April 15, 1911, edition of the Chitina Leader: 'Last night about 9:20 p.m. a flash which was at first mistaken for lightning, was observed at the summit of Mount Wrangell. Anyone who argues for AGW should be open to facts that prove otherwise and anyone who argues against AGW should be open to facts that prove it is so. every little twig is covered in frost and i'm hibernating till it warms a little. However, the one in 1784 is highly dubious, in part because the mountain wasn't discovered until 1819. Currently Kilauea is dominant over the hotspot with a supply many times higher, while the summit of Mauna Loa totals about 45 cm of extension since end of the 1984 eruption the summit of Kilauea has since the stop of the 2018 eruption inflated even more, about 50 cm of caldera lenght increase while at the same time inflating its east rift zone. The benefits of CO2 fertilisation and warmth. It is significantly lower than the other peaks, at a measly 3,661 meters, but this is not for want of trying. http://www.bom.gov.au/state-of-the-climate/State-of-the-Climate-2018.pdf. Mount Wrangell itself, over 4317 meters tall, remains an active volcano. HISTORIC EVENT DATES (22 events) Key: Eruption Questionable eruption Non-eruptive activity. See more ideas about Wrangell, National parks, Alaska. Its current volume is about 900 km3. At that time, indeed, there were scientists arguing on both sides. A lake on an island in a lake on an island? This was shown by an oceanographic campaign in May 2019. The dark ages correspond to cold periods, the golden years are warm periods. But there is no evidence of older eruptions similar to the 853 event. Ref the Andesite… the whole area is accretionary. I have yet to see any science program that includes Betelgeuse that does not also mention it's utter weirdness. Over large areas extrusive rocks lie in flat undisturbed piles on a Cenozoic surface of moderate relief. The observations show negative feedback with water vapour decreasing, consistent with Le Chatelier's principle, (the thermodynamic equilibrium law), The actual driver of climate is changes to cloud cover which is an order of magnitude larger than CO2 forcing. As much as 100 km3 may have been removed in the explosion. What is occurring? Rather than erupting explosive lavas forming stratovolcanoes, they have been built by the buildup of hundreds of comparatively fluid lava flows to form shield volcanoes. And one Wrangell volcano has produced this ultimate rarity, a rhyolitic voluminous lava flow. Science has a procedure for this: if you pose a model based on the currently available data, this model should make predictions which can be tested in the future. It is interesting that these shield volcanoes are also mostly andesite. I knew volcanos is skookum as frig, but now I've got a picture to go with it! The physics of global warming is most definite on the science side! It too is volcanic, and probably formed between 600,000 and 200,000 years ago. 3.0 shake in Katla. Considerable recent uplift, accompanied by rapid erosion, has reduced once vast areas of upper Cenozoic volcanic rocks to small isolated remnants. He reports seeing smoke from the mountain in December 1884 and on February 3 a very large column of smoke and 'hurling imense stones hundreds of feet high in the air' as well as a rumbling noise. A cone next to Wrangell, called Mount Zanetti, may be only 25,000 years old. The Wrangell Mountains are immediately east of this gap, and are a bit in-land, as a clearly separate mountain range. In 1834, Baron Ferdinand Petrovich Wrangel, then head of Russian government interests in Russian America, ordered a stockade built near the Naanyaa.aayí clan house of Chief Shakes, called Shéiksh Hídi. Page 8 talks about the drastic increasing chance of 'compound events'. The Mauna Loa deformation is remarkably uniform. Gone again. Mount Bona, in the adjacent St Elias mountain, is the tallest US volcano, beating such giants as Mauna Loa. I hope you, your house and your town are ok! It rises due south of another famous Wrangell volcano, Mount Sanford. Also concerned with the positive feedback loops currently happening in the Middle East. And bye bye pancake lava dome blasted away. This mountain complex is around 130 kilometers long The mounts are surrounded by dead trees, killed by the salty mud after activity here increased following the 1964 quake. Part 2 of the Wrangell saga. This area has mud volcanoes, where mounts of soil a kilometer wide and 100 meters high have been created by warm springs. Immediately west of the Wrangell Mountains is the Copper River valley, known for its large copper deposits. It was like we were driving on a huge belt of moving road travelling in the opposite direction at the same speed, cancelling all our progress. WRANGELL LINKS. Interestingly, the 1900 eruption was shortly after the September 3, 1899 Yakutat earthquake (M8). No matter how long we drove we seemed to be standing still and as the hours went by it was rather disconcerting. 3. Try living with the deadly consequences of intransigent science denial and the imposition of religious freedom legislation to discriminate where they like when it comes to supplying goods and services like medical attention; then tell me I'm being a tad too authoritarian. The volcano is a very large (900 km3) broad shield containing an ice-filled, nonexplosive, collapse caldera measuring 3.2 by 5.6 kilometers. Alert raised to Red now, first time for Shishaldin since 1999. It is that hot and dry in Australia this season that the bush fires started in August – late Winter; and have burned through areas that have only recently been burned to reduce fuel. There has been no large eruption for the past 200,000 years, and only a small region remains active. Capital Mountain became briefly active 1 million years ago but activity here ceased within 100,000 years. The Ahtna people call it K'elt'aeni, "the one who controls the weather," with the alternate name Uk'eledi, "the one with smoke on it" when it is active. The source of the Wrangell volcanics is clearly the subduction of the Pacific plate underneath Alaska. The individual Wrangell volcanoes are described very well in the Guide to the Volcanoes of the Western Wrangell Mountains, Alaska-Wrangell-St. Elias National Park and Preserve, by Donald Richter and collaborators, published by that most open-access publisher of all, the USGS. 1995, USGS Bulletin 2072 https://pubs.usgs.gov/bul/2072/report.pdf. When the eruption comes if it is at the summit it will be small (like 1975), if at the rifts probably similar to 1984. The volcanic zone may be in the process of dying. That leaves us with the 1900 eruption. It looks like the cone in the lake has itself developed a crater lake. Now, an international team led by the scientist Simone Cesca from the German GeoForschungsZentrum GFZ is illuminating the processes deep inside the Earth before and during the formation of the new volcano. Nice to know that other folks appreciate AvE! Tanada is around 1.5 million years old, and like the other volcanoes here it experienced caldera collapse and died. Source: https://endlessloopphotography.com/2016/08/09/the-alaska-highway-and-wrangell-st-elias-national-park-canada-and-alaska/. To give it a European scale, this park is larger than Switzerland. The one you just read is about 2500 words. To be "weathered-in" at the South eastern Alaska coastal town of Wrangell is an experience with frontier mentality, for fishing and drinking are the principal pursuits of the pop ulace. The 1900 event has stronger credentials than the others, being reported by three different people, but is not confirmed. Where all is not revealed. After Skookum became extinct, activity shifted southwest, to Tanada and Jarvis. I think 2019 saw an unusual area of fires across the world, considering also the fires in the Brazil, Bolivia, Siberia, Indonesia… That puts extra CO2 into the atmosphere, a classical positive feedback loop. The Wrangell Volcanic Zone is not overly active. Come back next week to read about reluctant subduction, building America, and the flood that brought the rain. Wrangell — Original name in latin Wrangell Name in other language WRG State code US Continent/City America/Sitka longitude 56.47083 latitude 132.37667 altitude 26 Population 2369 Date 2011 05 14 … Further east, there is a length of 400 kilometer without volcanoes, so unexpected that it has a name: it is called the Denali volcanic gap. As offtopic, and also on the "fires" topic, sad to see the massive fires in Australia. That is bigger than several European countries, or US states. It was deleted when the mistake was spotted, but the email didn't know that. But underneath runs a deeper history, and lies an older volcanic field. They just got the power back on and boom. Where the magma goes is less clear! This 14,163 ft volcano last erupted March, 1930. The last major eruption of the volcano occurred in 1900, although steam is a common sight above the massive peak. It too is a large shield volcano, build up by andesitic eruptions. These fumaroles frequently produce steam plumes that are mistaken for eruptive activity. REPORTED ACTIVITY. 2. It is sometimes suggested that this may have been smoke from the fumarole patch on the southwestern flank of Mount Wrangell. As a group they proved vulnerable to deception by people they thought were on their side. The 1884/5 eruption is also considered unconfirmed. Very interessting! The Wrangells are some of the most visually striking of the Alaskan mountains because of their rugged topography and perennial snow cover. It's predictions made over a year ago have come to pass. No worries. 2014. I take it you don't live in Australia Rob; and if you do you are nowhere near a fire? The Wrangell Mountains are build on an ancient volcanic history, which played an important part not only in the building of America, but in the evolution of the Earth. Description: Activity at Mount Blackburn was reported in an Associated Press article published March 26, 1930, but this activity is probably attributable to Mount Wrangell rather than Mount Blackburn. Andesite lava was ejected from the circular caldera fault at this time. Most of volcanoes of the Western Wrangell Mountains are not like the other volcanoes located around the Pacific Rim. If you need imaginary cycles to deny the blindingly obvious, you have a problem. True. As for the current Australian fires, the indigenous owners used to burn twice this area every year, thats the only way that you can prevent fire here, reduce the fuel load. Have the holocene magmas been "less" Thoelitic than the main building phase during Late Pleistocene? Probaly will be the same fast short lived voluminous style as 1984 and 1950 s with large fountains and fast moving open channels. The massive andesitic shield volcano has produced fluid lava flows as long as 58 km and contains an ice-filled 4-6 km diameter caldera located within a 15-km-wide ancestral caldera.
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LEADERSHIP JUDGMENT
By The John Maxwell Company | June 6, 2012 | 0
The outcome of a sporting event sometimes is heavily influenced by the judgment of an official or umpire. For instance, with game two of the playoff series between the Boston Celtics and Miami Heat tied 103-103, Celtics guard Rajon Rondo drove toward the hoop for a layup. Dwyane Wade of the Heat appeared to whack Rondo on the head, causing his shot to miss its mark. However, the referee decided not to whistle a foul, and the Heat took advantage of the no-call, quickly scoring a basket at the other end of the court. They would go on to defeat the Celtics 115-111.
We often think of judgment as taking place at a single moment in time, much like the pivotal decision made by the referee in the Heat-Celtics game. In actuality, judgment occurs as a dynamic, ongoing process in which we constantly receive new information and have the opportunity to make adjustments. As leaders, before we make the right call, we must first identify which decisions are the most critical. Then, after making a decision, we must be able to follow through on it in order to see results. Altogether, judgment takes place over the course of three stages: identification, decision-making, and execution.
To grow more productive, a person must be able to separate the trivial from the important and to focus on the latter. In leadership, however, setting priorities isn't enough. Priorities must also be shared, or held in common, by those in the organization. Furthermore, in order to bring about alignment, a leader has to sell key influencers within the organization on the importance of particular priorities.
The first step in identification is to revisit the big-picture vision. Where are you headed as an organization? What do you hope to accomplish? Only decisions with direct bearing on your vision deserve your attention.
Identification then proceeds by listening. Ask your teammates the biggest problems they encounter on the job from day to day. Also, solicit input on the opportunities they see to improve the way you do business. Asking for ideas and feedback from team members has two benefits. First, it allows you to overcome your personal blind spots as a leader. Second, it empowers others by giving them a voice.
Finally, identification involves focusing your team's attention on the major decision at hand. As a leader, this means taking the time to sit down with your most influential teammates to make sure they understand why the decision is important and how it may affect them. At this point, a leader asks for assistance in gathering the information needed to make an educated decision. Additionally, the leader secures a commitment from others to support whatever final decision is made.
After determining which decisions deserve precedence and evaluating information pertaining to the decision, a leader then makes the call. At this stage, courage counts just as much as intelligence. Oftentimes the difficulty in decision-making has nothing to do with uncertain knowledge about the best course of action but rather lies in overcoming the negative emotion associated with making a tough call.
What good is making a decision without taking steps to implement it? In the words of A.G. Lafley, former President and CEO of Procter & Gamble:
Execution is the only strategy that anybody on the outside ever sees. They [consumers, retailers, and competitors] don't see the strategy we wrote down. They don't see the choice set.
Your customers and clients know nothing of the decisions you reach except what you communicate to them through action.
Every time you make a decision as a team, assign someone to take ownership of its execution. Also, create milestones that will allow you to measure progress on decision's implementation. Finally, collect feedback on the impact of the decision once it has been executed and make adjustments as needed.
This article was inspired by Warren Bennis and Noel Tichy's excellent book: Judgment: How Winning Leaders Make Great Calls.
Posted in Downloads and tagged Decision Making, execution, Growth, identification, Influence, judgment, Leadership


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Two of the scene's most seminal dj's representing two of the longest-standing and respected labels in drum and bass joined us on the first night of Outlook 2018 at the Garden stage for a massive two hour b2b set that would set the bar for the rest of the festival.
Exit Record's bossman dBridge joined Metalheadz head honcho Goldie for what has to be one of the most powerful sets we've experienced at the fort (so powerful the speakers blew their drivers). Featuring the vocal expertise of one of scene's finest emcees SP:MC – there's nothing more to be said – only experienced.
Jumpin Jack Frost & Sofi Mari bring us the first instalment of Liquid Lounge.
Our 2019 promo mix in support of our new release – BMT046 – Dominion VIP / Stay, featuring loads of dubs, brand new music and tunes that we are really feeling at the moment.


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Das Mémorial des Martyrs de la Déportation (deutsch: Denkmal für die Märtyrer der Deportation) ist ein Denkmal auf der Île de la Cité in Paris zur Erinnerung an die zwischen 1941 und 1944 aus Frankreich Deportierten. Seine Architektur soll dazu beitragen, das Leid der Deportierten in Erinnerung zu rufen und den Besucher zum Nachdenken und zur Andacht zu bewegen.
Dieses Monument ist seit dem 23. November 2007 klassifiziert als Monument historique (historisches Monument).

Entstehung und Lage
Erbaut wurde es im Auftrag der Réseau du Souvenir, dem Netz der Erinnerung, das dem Staat am 29. Februar 1964 eine Spende zukommen ließ.
Gelegen ist es im 4. Arrondissement von Paris am östlichen Punkt der Île de la Cité.

Das Projekt wurde vom Architekten Georges-Henri Pingusson realisiert und am 12. April 1962 vom Präsidenten Charles de Gaulle freigegeben.

Beschreibung
Auf den ersten Blick wirkt das Monument wie ein weißer Steinbunker und wird über relativ schmale, unebene und steile Stufen betreten. Die Betonkonstruktion ist mit einer mit dem Hammer bearbeiteten Fassade bedeckt und mit Kies aus den verschiedenen Regionen Frankreichs bedeckt, was die Oberfläche eines rauen Natursteins nachahmt.
Von einem dreieckigen Innenhof entfaltet sich die Krypta, der Kern des Denkmals, mit engen und schlecht beleuchteten Passagen. Der lange, durch Gitter geschützte, Flur zeigt an seinen Wänden 200000 Glasstäbe als Symbol für die unzähligen Opfer der Deportation in NS-Lager. Am Eingang dieses Flurs befindet sich ein Grab mit den sterblichen Überresten eines unbekannten Opfers, das im Konzentrationslager Natzweiler-Struthof gestorben ist und am 10. April 1962 hierher überführt worden ist.

Der dreieckige Hof öffnet sich dem Fluss mit einer horizontalen Öffnung, die durch eckige Stangen verdeckt wird. Der Besucher befindet sich fast auf dem Niveau der Seine und durch die Fensteröffnung kann man das fließende Wasser sehen bzw. senkrecht den Blick gegen den Himmel richten. Nach dem Abstieg der Treppe beschreiben Besucher ein Gefühl der Fremdartigkeit, bei dem sie sich als außerhalb der Welt wie wir sie kennen wahrnehmen.
Links und Rechts befinden sich in runden Ausstülpungen Urnen, die Erde aus verschiedenen NS-Lagern oder Asche aus den Krematorien enthalten. An den Wänden sind Auszüge aus den Gedichten oder Zitaten von Robert Desnos, Paul Éluard, Louis Aragon, Vercors, Antoine de Saint-Exupéry, Jean-Augustin Maydieu und Jean-Paul Sartre geschrieben.

Oberhalb befinden sich mehrere Ausstellungsräume, die nur auf Anfrage betreten werden können.

Öffnungszeiten und Veranstaltungen
Das Denkmal ist frei zu betreten, für Kinder nur unter Begleitung eines Erwachsenen; täglich außer Montag vormittags und nachmittags. Jeden letzten Sonntag im April gibt es eine Gedenkveranstaltung anlässlich des Journée nationale du souvenir de la déportation, dem französischen Tag der Erinnerung an die Opfer der NS-Deportationen, der am 28. April stattfindet.

Weblinks

Gedenkstätte für NS-Opfer
Denkmal der politischen Geschichte
Erbaut in den 1960er Jahren
Monument historique im 4. Arrondissement (Paris)
Bauwerk in Paris
Monument historique (Bauwerk)
Monument historique seit 2007
Bauwerk aus Beton
Monument historique (Denkmal)

redpajama_set_name: RedPajamaWikipedia


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text:
with anatomy
Art Illustration
Dramatic Anatomical Drawings Comprised of Complex Hatched Colors by WanJin Gim
Laura Staugaitis
Seoul-based artist WanJin Gim illustrates the form and gesture of the human body using complex hatched layers of color and dramatic lighting. He adds intrigue to poses that could be considered traditional figure drawing studies by adding abstracted lines and watercolor washes that integrate the fragmented body parts into a larger visual field. In an interview with Trending All Day, the artist describes his inspiration and process:
I'm interested in expressing body temperature and skin smell and am studying the relationship between color and energy (Qi) for my work… Currently I usually use oil pastel and colored pencils. They both have limited colors, so I need to overlap them to produce a color that I like. Even if I can't express the color that I intend to make, I am satisfied with the exceptional effect coming from the imperfectness.
Gim studied animation in university, but began creating in his current style in earnest after coming across the work of painter and draftsman Lucian Freud. He shares his work on Instagram, as well as on his website.
Textile Bodies Reveal Branched Systems of Veins, Flowers and Roots by Raija Jokinen
Kate Sierzputowski
Finnish artist Raija Jokinen creates sculptural bodies out of flax which attempt to reveal the complicated relationship between the mind and body. Webs of flowers, veins, and roots cover her textile torsos, shape-shifting between plant and human forms. Jokinen invites the audience to get lost in these visual similarities, as she makes no distinction between whether the pieces are actually nerves or sprouting tree branches.
"It is fascinating how body-related details, such as skin, blood vessels, and nerve tracks resemble the forms of roots or branches, as well as many other organic things," Jokinen told Colossal. "I am excited in their apparent similarity, infinite variation, and how these visual allegories can be found almost everywhere. These forms are optimal for the life-support functions, and maybe also for our mind."
Jokinen compares her sculptural practice to painting, using handmade flax rather than paint. An upcoming solo exhibition of her fibrous sculptures opens March 14 at Galleria Uusi Kipinä and runs through April 8. You can see more of her body-based works on her website.
100 Fiberglass and Resin Skulls Fill a Room at the National Gallery of Victoria in Melbourne
Ron Mueck, an Australian artist known for his hyperrealistic figural sculptures, has created his largest work to date. His installation Mass contains 100 human skulls which are scattered and stacked throughout a gallery at the National Gallery of Victoria in Melbourne, Australia.
The individual forms are created from fiberglass and resin, and when stood upright, rise to approximately three feet tall. In some areas of the installation piles reach five skulls in height, while in others visitors can approach individual works resting on the gallery's floor. Placed amongst gilded paintings the works offer a somber reality, a morose peek into what physically relates each of us.
Mass opens December 15, 2017 as a part of the inaugural National Gallery of Victoria Triennial. Mueck is one of 100 international creatives that has contributed work to the exhibition which will run through April 18, 2018. (via Designboom)
Brittle Skeletons Crocheted from Discarded Textiles by Caitlin McCormack
Philadelphia-based artist Caitlin McCormack (previously) continues to explore the decay and remains of once-living things in her intricate crochet work. McCormick constructs her pieces using a labor intensive process that involves stiffening discarded textile materials with enamel paint to create brittle bone-like material. She then crochets fantastical intertwined skeletons of humans, birds, snakes, devils, and two-headed bats, which are displayed with stark black backdrops, glass cases, and lathed bases that reference old-fashioned displays for scientific specimens.
Her new show, Lazarus Taxa, refers to the paleontological concept of species that disappear and reappear in the fossil record. Lazarus Taxa is currently on display at Paradigm Gallery + Studio. You can also follow her on Instagram.
Artist Ronit Baranga's Disturbing Anatomical Dishware Creeps Across Tabletops
Artist Ronit Baranga (previously) creates ceramic sculptural works she describes as existing on the "border between living and still life"—objects guaranteed to either tickle your funny bone or haunt your worst nightmares, depending on your perspective. Baranga depicts dishware as sprouting human fingers and gaping mouths as the objects traipse across tabletops or physically cling to one another in a permanent embrace. The pieces are both silly and sinister as they come to life as if from a cartoon. A quick scroll through her Instagram reveals even darker works that give us the bonafide heebie-jeebies.
Ronit most recently had work on view at the Gross Anatomies show at the Akron Art Museum, and is also a contruting artist to the Small Works 2017 with beinArt Gallery through August. (via My Amp Goes to 11)
A post shared by Ronit Baranga (@ronitbaranga) on Jan 23, 2017 at 12:27pm PST
Anatomical Cross-Sections of Human Heads Reveal a Menagerie of Found Objects
Chicago-based artist duo Edwige Massart and Xavier Wynn (previously) sculpt cross-sections of human heads that are organized into compartments of tiny objects. The series began several years ago as an intersection of sorts involving Massart's personal collection of found objects that she began at the age of four, and Wynn's childhood discovery of "split body" models at Chicago's Field Museum that inspired a lingering fascination with human anatomy. Each sculpture is given only a number (ie. Head 14) leaving the viewer to examine the compartments of objects and draw their own parallels and conclusions. You can see more recent work from the Heads series on their website. (via Colossal Submissions)
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