Rock glacier

Formation

The two known factors that must be present in order to create rock glaciers are low ice velocity and permafrost. Most glacial rock glaciers are created by the recession of debris covered glaciers. Glacial rock glaciers are often found in cirque basins where rocky debris falls off the steep sides and accumulates on ice glaciers.{{Cite book

With the exception of ice-cored rock glaciers, rock glaciers are a periglacial/permafrost process. This means that they are a nonglacial landform associated with cold climates, particularly with various aspects of frozen ground. Permafrost rock glaciers require permafrost-derived ice instead of glacial ice in order to form. Instead, they are caused by continuous freezing occurring within a talus lobe.{{Cite book

Nearby cliffs are in many cases a requirement for the formation of rock glaciers, and as such many rock glaciers form in valleys steepened by glacier erosion. Rock masses of rock glaciers have been found to make up different rock types depending on the local geology. These rock types include andesite, basalt, granite, porphyry, quartzite, and sandstone.

Ordinary glaciers can override rock glaciers, acquiring some of its material and properties. More usually, rock glaciers originate from weathered rock debris progressively covering an existing glacier. Typically in the European Alps, this is post Little Ice Age

Movement

Rock glaciers move downslope by deformation of the ice contained within them, causing their surface to resemble those of glaciers. Rock glaciers may flow or creep at a very slow rate, in part dependent on the thickness of ice present. Surface velocities are generally less than 2m/a, although this depends where measurements have been taken on the length of the rock glacier.

Some rock glaciers can reach lengths of 3 km and can have terminal embankments 60 m high. Blocks on the surface can be up to 8 m in diameter. Flow features on the surface of rock glaciers may develop from:

• Deformation of a glacier ice core.

• Movement of the debris cover along the debris-ice interface.

• Deformation from a period of glacial advance.

• Changes in the hydrologic balance. Their growth and formation is subject to some debate, with three main theories:

• A glacier origin, where a small glacier has been buried by weathered debris that has largely prevented melting.

• A permafrost origin, which implies that the features are related to the presence of permafrost ice rather than a glacier core;

• A mass wasting or landslide origin, which does not require the presence of ice and suggests a sudden catastrophic origin with little subsequent movement.

According to recent studies, rock glaciers positively influence the streams around them.

Subject to climate variation, rock glaciers in proximity tend to have a highly synchronous movement pattern over a short time scale; over long term, however, the relationship between rock glacier velocity and climate difference may not be as pronounced, due to the influences of topographic factors and lack of ice or debris budget within the glacier body.

Human use

Rock glaciers in the Chilean Andes help supply the water for much of Chile, including the capital of Santiago. Mining operations in the high mountains have led to the degradation and destruction of more than two rock glaciers. Several copper mines dump their waste rock onto rock glaciers, which results in faster melting and higher velocity movement of these rock glaciers. The dumping of waste rock on the rock glaciers may lead to their destabilization. In 2004, protesting irrigation farmers and environmentalists changed rules so new mining projects can no longer damage or alter rock glaciers in Chile.{{Cite book

Parts of the only road into Denali National Park and Preserve in Alaska are built on a rock glacier known as "Pretty Rocks". In late summer 2021 the road had to be closed due to accelerating rockslides in that area, sometimes sliding up to 10 in in a single day, apparently due to climate change. In Colorado, the large landslide, Slumgullion Earthflow has a plan-form more typical of a rock glacier but it does not flow from a glacial cirque.{{cite journal|last1 = Hu | first1=Xie |last2 = Bürgmann| first2 = Roland | last3 = Schulz| first3 = William H.| last4 = Fielding| first4 = Eric J.

References

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• {{Cite journal

References

1. (1906). "Glacial phenomena of the San Juan mountains, Colorado". Bulletin of the Geological Society of America.
2. Capps, Stephen R. jr.. (1910). "Rock glaciers in Alaska". Journal of Geology.
3. JGabrielli, S, Spagnolo, M., De Sienna, L. (2020):Journal of Maps 16, 585-594.
4. Whalley, W. Brian. (2003). "Rock glaciers and protalus landforms: Analogous forms and ice sources on Earth and Mars". Journal of Geophysical Research.
5. Jarman D, Wilson P, Harrison, S. (2013): Are there any relict rock glaciers in Britain? Journal of Quaternary Science 28, 131-143.
6. Whalley, W.Brian. (2024). "Glacier–rock glacier interactions in the eastern Hindu Kush, Nuristan, Afghanistan [35.92,71.13] in the period 1976-2019". [[Geografiska Annaler A]].
7. Potter, Noel. (1972). "Ice-cored rock glacier, Galena Creek, northern Absaroka Mountains, Wyoming". [[Geological Society of America Bulletin]].
8. Corte, Arturo E.. (1976). "Rock glaciers". [[Biuletyn Peryglacjalny]].
9. Whalley, W.Brian. (2020). "Gruben glacier and rock glacier, Wallis, Switzerland: glacier ice exposures and their interpretation". [[Geografiska Annaler A]].
10. (1992). "Rock glaciers: II models and mechanisms". Progress in Physical Geography.
11. (1987). "A glacier icecored rock glacier, Tröllaskagi, Iceland". Jökull.
12. (1996). "Rockglaciers. Indicators for the present and former geoecology in high mountain environment". Springer.
13. (1984). "Rock glacier formation by high-magnitude low-frequency slope processes in the southwest Yukon". Annals of the Association of American Geographers.
14. (1 August 2014). "Influence of Rock Glaciers on Stream Hydrology in the La Sal Mountains, Utah". Arctic, Antarctic, and Alpine Research.
15. (2015-02-06). "Contrasting responses of Central Asian rock glaciers to global warming". Scientific Reports.
16. Brenning, Alexander. (2010). "Minería y glaciares rocosos: impactos ambientales, antecedentes políticos y legales, y perspectivas futuras". [[Revista de Geografía Norte Grande]].
17. [https://www.nps.gov/dena/learn/nature/pretty-rocks.htm Pretty Rocks Landslide], National Park Service. Retrieved 2025-10-06.