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
What we do. Every page goes through several hundred of perfecting techniques; in live mode. Quite the same Wikipedia. Just better.

From Wikipedia, the free encyclopedia

Hawkins Glacier Head (21426626109)
Hawkins Glacier Head (21426626109)

A glacier head is the top of a glacier. Although glaciers seem motionless to the observer they are in constant motion and the terminus is always either advancing or retreating. [1]

The accumulation zone is found at the highest altitude of the glacier, where accumulation of material is greater than ablation.
The accumulation zone is found at the highest altitude of the glacier, where accumulation of material is greater than ablation.

On a glacier, the accumulation zone is the area above the firn line, where snowfall accumulates and exceeds the losses from ablation, (melting, evaporation, and sublimation). The annual equilibrium line separates the accumulation and ablation zone annually. The accumulation zone is also defined as the part of a glacier's surface, usually at higher elevations, on which there is net accumulation of snow, which subsequently turns into firn and then glacier ice. Part of the glacier where snow builds up and turns to ice moves outward from there.

The glacier head is the highest upslope edge of an alpine glacier or the upslope end of the zone of accumulation. The head of the glacier comes up against a steep bedrock cliff called a cirque headwall[2]

Refer to caption
Cross section of a cirque glacier showing the bergschrund

Movement and ice loss

The head can come away from the cirque in a downslope movement which can create a large crevasse called a bergschrund. This crevasse can be a major obstacle for mountaineers. The existence of a bergschrund is evidence that ice mass has pulled away from the cirque. [2]

A shrinking glacier thins faster near the terminus than near the head, which explains why glaciers retreat up-valley and the glacier head stays in place[3]

The speed of erosion or accumulation is partly dependent on a shape factor which is the ratio of the change in thickness at the glacier head to the change in the thickness at the terminus.[4]


  1. ^ "Glacier Features: Glacier terminus | National Snow and Ice Data Center". Retrieved 27 October 2019.
  2. ^ a b Monroe, James S.; Wicander, Reed (January 2014). The Changing Earth: Exploring Geology and Evolution. p. 526–536. ISBN 9781285733418.
  3. ^ "USGS Fact Sheet 2009–3046: Fifty-Year Record of Glacier Change Reveals Shifting Climate in the Pacific Northwest and Alaska, USA". Retrieved 27 October 2019.
  4. ^ "Glacier response time". Retrieved 27 October 2019.

attribution:Contains text copied from Accumulation zone and Bergschrund and Terminus.

This page was last edited on 18 December 2020, at 13:39
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.