Permafrost and Other Periglacial Landforms

Yukon Landform Atlas

C.A.Huscroft and P.S. Lipovsky

Periglacial landforms are landforms that are characteristic of cold environments that are not glacial.  They include environments that are dominated by permafrost processes.

Below are a variety of interactive maps of examples of various periglacial landforms found in the Yukon Territory. The list is by no means exhaustive, but you will also find links to further reading.

Please scroll over the icons and click "View Features" to explore each interactive story map.

 

Active Layer Detachment Failures

These landslides involve the detachment of the thawed or thawing portion of the active layer from the underlying frozen material.

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Pingos

These mounds consist of a core of permafrost composed mostly of massive ice produced  by injection of water, covered with soil and vegetation

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Cryoplanation Terraces

These step-like benches are cut in bedrock in cold climate regions.

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Rock Glaciers

These masses of rock fragments and finer material contain either interstitial ice or an ice core and they show evidence of past or present movement on slopes.

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Patterned Ground

This group of features exhibit a discernibly ordered, more or less symmetrical, pattern of sediment and, where present, vegetation.

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Solifluction Features

These landform features are produced by slow downslope flow of saturated unfrozen earth materials and are common in permafrost areas.

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Palsas and Palsa-like mounds

A permafrost mound possessing a core of alternating layers of ice and peat or mineral soil material

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Retrogressive Thaw Slumps

These landslides are produced by thawing of slopes that contain ice-rich permafrost on a slope.

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Tors

These tower-shaped outcrops of rock are common in landscapes that have experienced long periods of cold climate without glaciation.

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Ice Wedge Polygons

This type of patterned ground is identified by its distinctive pattern of angular and multi-sided closed shapes which are bounded by underlying wedge-shaped bodies of ice.

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Other Periglacial Landslides

These types of landslides are influenced by the presence of permafrost and are less common in the Yukon.

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Thermokarst lakes

This type of lake fills a depression formed by settlement of the ground following thawing of ice-rich permafrost or the melting of buried massive ice.

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http://ygsftp.gov.yk.ca/LandformAtlas_Draft2/Img/Fig_G16_1.jpg

Sheetwash

 

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