To install click the Add extension button. That's it.

The source code for the WIKI 2 extension is being checked by specialists of the Mozilla Foundation, Google, and Apple. You could also do it yourself at any point in time.

Kelly Slayton
Congratulations on this excellent venture… what a great idea!
Alexander Grigorievskiy
I use WIKI 2 every day and almost forgot how the original Wikipedia looks like.
Live Statistics
English Articles
Improved in 24 Hours
Added in 24 Hours
Show all languages
What we do. Every page goes through several hundred of perfecting techniques; in live mode. Quite the same Wikipedia. Just better.

Lambert Graben

From Wikipedia, the free encyclopedia

Lambert Graben is a graben in Antarctica. It intersects the coast at Prydz Bay and contains the largest glacier in the world, Lambert Glacier. The graben is a Permian rift which contains coal beds. The graben has been correlated with the coal bearing Godavari Valley of the Indian Peninsula prior to the breakup of Gondwana.[1]

YouTube Encyclopedic

  • 1/1
  • ✪ Lambert Glacier is one of the world's largest and longest glaciers.



The graben is a Late Palaeozoic-Mesozoic triple junction failed rift. Precambrian metamorphic rocks, composed of granulite-facies sequences intruded by granites and pegmatites, are overlain by the Permian sedimentary Amery Group. These rocks outcrop on the Platforma Kamenistaja and Else Platform within the northern Jetty Peninsula (Jetty Oasis).[2]


  1. ^ Mat Harrowfield, et al., Tectonic significance of the Lambert graben, East Antarctica: Reconstructing the Gondwanan rift, Geology, March 2005, v. 33, no. 3, p. 197-200, doi:10.1130/G21081.1
  2. ^ Hofmann, J. (1991). Thomson, M.R.A.; Crame, J.A.; Thomson, J.W. (eds.). Fault tectonics and magmatic ages in the Jetty Oasis area, Mac.Robertson Land: a contribution to the Lambert rift development, in Geological Evolution of Antarctica. Cambridge: Cambridge University Press. pp. 107–112. ISBN 9780521372664.

This page was last edited on 15 January 2020, at 19:51
Basis of this page is in Wikipedia. Text is available under the CC BY-SA 3.0 Unported License. Non-text media are available under their specified licenses. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc. WIKI 2 is an independent company and has no affiliation with Wikimedia Foundation.