Jump to content

Talk:Pine Island Glacier/GA1

Page contents not supported in other languages.
From Wikipedia, the free encyclopedia

GA Review

[edit]

Article (edit | visual edit | history) · Article talk (edit | history) · Watch
GA review – see WP:WIAGA for criteria

  1. Is it reasonably well written?
    A. Prose quality:
    B. MoS compliance:
  2. Is it factually accurate and verifiable?
    A. References to sources:
    B. Citation of reliable sources where necessary:
    C. No original research:
  3. Is it broad in its coverage?
    A. Major aspects:
    B. Focused:
  4. Is it neutral?
  1. Fair representation without bias:
  2. Is it stable?
    No edit wars, etc:
  3. Does it contain images to illustrate the topic?
    A. Images are copyright tagged, and non-free images have fair use rationales:
    None provided.
    B. Images are provided where possible and appropriate, with suitable captions:
    None Provided.
  4. Overall:
    Pass or Fail:

There were some formatting errors, but I think the article is overall a very good article. ceranthor 22:38, 9 June 2009 (UTC)[reply]

Your last sentence in the acceleration section. It would seem that this question can be explored more by describing the acceleration observed. Polargeo I encourage you to do so. That is where is acceleration greatest, is it propogating. This will help indicate whether it is a calving front-ice shelf or upstream induced phenomenon. I did the bathymetry for the Polar Freeze journey for T.Kellogg and T.Hughes.