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Moraine

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(Redirected from Glacial Drift)
This article is about geological phenomena. For other uses, see Moraine (disambiguation).
Not to be confused with Murrain, an antiquated term for various infectious diseases affecting cattle and sheep.
The snow-free debris hills around the lagoon are lateral and terminal moraines of a valley glacier in Manang, Nepal.

A moraine is any accumulation of unconsolidated debris (regolith and rock), sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice sheet. It may consist of partly rounded particles ranging in size from boulders (in which case it is often referred to as boulder clay) down to gravel and sand, in a groundmass of finely-divided clayey material sometimes called glacial flour. Lateral moraines are those formed at the side of the ice flow, and terminal moraines are those formed at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines (till-covered areas forming sheets on flat or irregular topography) and medial moraines (moraines formed where two glaciers meet).

Etymology

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The word moraine is borrowed from French moraine [mɔ.ʁɛn], which in turn is derived from the Savoyard Italian morena ('mound of earth'). Morena in this case was derived from Provençal morre ('snout'), itself from Vulgar Latin *murrum ('rounded object').[1] The term was introduced into geology by Horace Bénédict de Saussure in 1779.[2]

Characteristics

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Moraines are landforms composed of glacial till deposited primarily by glacial ice.[2] Glacial till, in turn, is unstratified and unsorted debris ranging in size from silt-sized glacial flour to large boulders.[3] The individual rock fragments are typically sub-angular to rounded in shape.[4] Moraines may be found on the glacier's surface or deposited as piles or sheets of debris where the glacier has melted.[5]

Formation

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Moraines may form through a number of processes, depending on the characteristics of sediment, the dynamics on the ice, and the location on the glacier in which the moraine is formed.[6] Moraine forming processes may be loosely divided into passive and active.[7]

Passive processes involve the placing of chaotic supraglacial sediments onto the landscape with limited reworking, typically forming hummocky moraines.[8][9] These moraines are composed of supraglacial sediments from the ice surface.[7]

Active processes form or rework moraine sediment directly by the movement of ice, known as glaciotectonism. These form push moraines and thrust-block moraines, which are often composed of till and reworked proglacial sediment.[10]

Moraine may also form by the accumulation of sand and gravel deposits from glacial streams emanating from the ice margin. These fan deposits may coalesce to form a long moraine bank marking the ice margin.[11] Several processes may combine to form and rework a single moraine, and most moraines record a continuum of processes. Reworking of moraines may lead to the formation of placer deposits of gold as is the case of southernmost Chile.[12]

Types of moraines

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See also: List of glacial moraines

Moraines can be classified either by origin, location with respect to a glacier or former glacier, or by shape.[13] The first approach is suitable for moraines associated with contemporary glaciers—but more difficult to apply to old moraines, which are defined by their particular morphology, since their origin is debated. Some moraine types are known only from ancient glaciers, while medial moraines of valley glaciers are poorly preserved and difficult to distinguish after the retreat or melting of the glacier.[citation needed]

Lateral moraines

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Lateral moraines above Lake Louise, Alberta, Canada.

Lateral moraines are parallel ridges of debris deposited along the sides of a glacier. The unconsolidated debris can be deposited on top of the glacier by frost shattering of the valley walls or from tributary streams flowing into the valley,[14] or may be subglacial debris carried to the surface of the glacier, melted out, and transported to the glacier margin.[15]

Moraines clearly seen on a side glacier of the Gorner Glacier, Zermatt, Switzerland. The lateral moraine is the high snow-free bank of debris in the top left hand quarter of the picture. The medial moraine is the double line of debris running down the centre-line of the glacier.

Lateral moraines can rise up to 140 meters (460 ft) over the valley floor, can be up to 3 kilometers (1.9 mi) long, and are steeper close to the glacier margin (up to 80 degrees) than further away (where slopes are typically 29 to 36 degrees.[15]

Ground moraines

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Ground moraines create irregular, rolling topography near Gainesville, New York.

Ground moraines are till-covered areas with irregular topography and no ridges, often forming gently rolling hills or plains,[16] with relief of less than 10 meters (33 ft). Ground moraine is accumulated at the base of the ice as lodgment till with a thin and discontinuous upper layer of supraglacial till deposited as the glacier retreats. It typically is found in the areas between end moraines.[17]

Rogen moraines

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Main article: Rogen moraine

Rogen moraines or ribbed moraines are a type of basal moraines that form a series of ribs perpendicular to the ice flow in an ice sheet. The depressions between the ribs are sometimes filled with water, making the Rogen moraines look like tigerstripes on aerial photographs. Rogen moraines are named after Lake Rogen[18] in Härjedalen, Sweden, the landform's type locality.

de Geer moraines

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Closely related to Rogen moraines, de Geer moraines are till ridges up to 5m high and 10–50m wide running perpendicular to the ice flow. They occur in large groups in low-lying areas.[19] Named for Gerard De Geer, who first described them in 1889, these moraines may have developed from crevasses underneath the ice sheet.[19] The Kvarken has a very high density of de Geer moraines.[20]

End or terminal moraines

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Main article: Terminal moraine
Multiple erratics on the Withrow terminal moraine of the Okanogan Lobe. Cascade mountains in the background.

End moraines, or terminal moraines, are ridges of unconsolidated debris deposited at the snout or end of the glacier. They usually reflect the shape of the glacier's terminus. Glaciers act much like a conveyor belt, carrying debris from the top of the glacier to the bottom where it deposits it in end moraines. End moraine size and shape are determined by whether the glacier is advancing, receding or at equilibrium. The longer the terminus of the glacier stays in one place, the more debris accumulate in the moraine. There are two types of end moraines: terminal and recessional. Terminal moraines mark the maximum advance of the glacier. Recessional moraines are small ridges left as a glacier pauses during its retreat. After a glacier retreats, the end moraine may be destroyed by postglacial erosion.[21]

Recessional moraine

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Recessional moraines are often observed as a series of transverse ridges running across a valley behind a terminal moraine. They form perpendicular to the lateral moraines that they reside between and are composed of unconsolidated debris deposited by the glacier. They are created during temporary halts in a glacier's retreat.[6][22]

Arctic push moraines

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Arctic push moraine in northern Ellesmere Island, Grant Land

In permafrost areas an advancing glacier may push up thick layers of frozen sediments at its front. An arctic push moraine will then be formed.

Medial moraine

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Medial moraines, Nuussuaq Peninsula, Greenland.

A medial moraine is a ridge of moraine that runs down the center of a valley floor. It forms when two glaciers meet and the debris on the edges of the adjacent valley sides join and are carried on top of the enlarged glacier. As the glacier melts or retreats, the debris is deposited and a ridge down the middle of the valley floor is created. The Kaskawulsh Glacier in the Kluane National Park, Yukon, has a ridge of medial moraine 1 km wide.[23]

The prominent dark streak at the left quarter is forming a medial moraine.
This is seen as a mudflat at the water's surface. (Brüggen Glacier, Patagonia).

Supraglacial moraines

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Supraglacial moraines are created by debris accumulated on top of glacial ice. This debris can accumulate due to ice flow toward the surface in the ablation zone,[24] melting of surface ice[25] or from debris that falls onto the glacier from valley sidewalls.[26]

Washboard moraines

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Washboard moraines, also known as minor or corrugated moraines, are low-amplitude geomorphic features caused by glaciers. They consist of low-relief ridges, 1 to 2 meters (3 ft 3 in to 6 ft 7 in) in height and around 100 meters (330 ft) apart, accumulated at the base of the ice as lodgment till.[27] The name "washboard moraine" refers to the fact that, from the air, it resembles a washboard.

Veiki moraine

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Main article: Veiki moraine

A Veiki moraine is a kind of hummocky moraine that forms irregular landscapes of ponds and plateaus surrounded by banks. It forms from the irregular melting of ice covered with a thick layer of debris. Veiki moraine is common in northern Sweden and parts of Canada.

See also

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See also: List of glacial moraines
Geologic features related to moraines
  • Glacial landform – Landform created by the action of glaciers
  • Drumlin – Elongated hill formed by glacial action
  • Esker – Long, winding ridge of stratified sand and gravel associated with former glaciers
  • Moraine-dammed lake – Type of lake formed by glaciation
  • Terminal moraine – Type of moraine that forms at the terminal of a glacier
  • Rogen moraine – Landform of ridges deposited by a glacier or ice sheet transverse to ice flow
  • Kame
Moraine examples

References

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  1. ^ "moraine". Oxford English Dictionary (Online ed.). Oxford University Press. (Subscription or participating institution membership required.)
  2. ^ a b Jackson, Julia A., ed. (1997). "moraine [glac geol]". Glossary of geology (Fourth ed.). Alexandria, Virginia: American Geological Institute. ISBN 0922152349.
  3. ^ Jackson 1997, "till".
  4. ^ Boggs, Sam (2006). Principles of sedimentology and stratigraphy (4th ed.). Upper Saddle River, N.J.: Pearson Prentice Hall. p. 281. ISBN 0131547283.
  5. ^ Boggs 2006, pp. 278–279.
  6. ^ a b Benn, Douglas I.; Evans, David J.A. (2010). Glaciers & glaciation (Second ed.). London: Routledge. ISBN 978-0340905791.
  7. ^ a b Möller, Per (December 2010). "Melt-out till and ribbed moraine formation, a case study from south Sweden". Sedimentary Geology. 232 (3–4): 161–180. Bibcode:2010SedG..232..161M. doi:10.1016/j.sedgeo.2009.11.003.
  8. ^ Kjær, Kurt H.; Krüger, Johannes (2001-10-21). "The final phase of dead-ice moraine development: processes and sediment architecture, Kötlujökull, Iceland". Sedimentology. 48 (5): 935–952. Bibcode:2001Sedim..48..935K. doi:10.1046/j.1365-3091.2001.00402.x. ISSN 1365-3091. S2CID 129374153.
  9. ^ Janowski, Lukasz; Tylmann, Karol; Trzcinska, Karolina; Rudowski, Stanislaw; Tegowski, Jaroslaw (2021). "Exploration of Glacial Landforms by Object-Based Image Analysis and Spectral Parameters of Digital Elevation Model". IEEE Transactions on Geoscience and Remote Sensing. 60: 1–17. doi:10.1109/TGRS.2021.3091771. ISSN 0196-2892.
  10. ^ Bennett, Matthew R. (2001-04-01). "The morphology, structural evolution and significance of push moraines". Earth-Science Reviews. 53 (3–4): 197–236. Bibcode:2001ESRv...53..197B. doi:10.1016/S0012-8252(00)00039-8.
  11. ^ Boulton, G. S. (1986-10-01). "Push-moraines and glacier-contact fans in marine and terrestrial environments". Sedimentology. 33 (5): 677–698. Bibcode:1986Sedim..33..677B. doi:10.1111/j.1365-3091.1986.tb01969.x. ISSN 1365-3091.
  12. ^ García, Marcelo; Correa, Jorge; Maksaev, Víctor; Townley, Brian (2020). "Potential mineral resources of the Chilean offshore: an overview". Andean Geology. 47 (1): 1–13. doi:10.5027/andgeoV47n1-3260.
  13. ^ Dreimanis, Aleksis (1989). "Tills: Their genetic terminology and classification". In Goldthwait; Matsch (eds.). Genetic classification of glacigenic deposits : final report of the Commission on Genesis and Lithology of Glacial Quaternary Deposits of the International Union for Quaternary Research (INQUA). Rotterdam: Balkema. pp. 17–83. ISBN 9061916941.
  14. ^ "Lateral Moraine". National Geographic Encyclopedia. May 5, 2011. Retrieved June 18, 2020.
  15. ^ a b Lukas, Sven; Graf, Andreas; Coray, Sandro; Schlüchter, Christian (March 2012). "Genesis, stability and preservation potential of large lateral moraines of Alpine valley glaciers – towards a unifying theory based on Findelengletscher, Switzerland". Quaternary Science Reviews. 38: 27–48. Bibcode:2012QSRv...38...27L. doi:10.1016/j.quascirev.2012.01.022.
  16. ^ Jackson 1997, "ground moraine".
  17. ^ Hilt Johnson, W.; Menzies, John (2002). "Supraglacial and ice-marginal deposits and landforms". Modern and Past Glacial Environments: 317–333. doi:10.1016/B978-075064226-2/50013-1. ISBN 9780750642262.
  18. ^ Möller, P., 2006. Rogen moraine: an example of glacial reshaping of preexisting landforms. Quaternary Science Reviews, 25:362–389
  19. ^ a b Metsähallitus (Forest and Park Services) (16 July 2006). The Kvarken Archipelago (PDF) (Report). Retrieved 3 October 2021.
  20. ^ Kotilainen, Aarno T.; Kaskela, Anu M.; Bäck, Saara; Leinikki, Jouni (2012). "Submarine De Geer Moraines in the Kvarken Archipelago, the Baltic Sea". Seafloor Geomorphology as Benthic Habitat: 289–298. doi:10.1016/B978-0-12-385140-6.00017-7. ISBN 9780123851406.
  21. ^ H.-E. Reineck; I. B. Singh (6 December 2012). Depositional Sedimentary Environments: With Reference to Terrigenous Clastics. Springer Science & Business Media. pp. 170–. ISBN 978-3-642-96291-2.
  22. ^ "Moraine". Columbia Electronic Encyclopedia, 6th Edition (2009): 1. Academic Search Complete. EBSCO. Web. 6 Oct. 2010.
  23. ^ Loomis, S.R. (1970). "Morphology and structure of an ice-cored medial moraine, Kaskawulsh Glacier, Yukon". Arctic Institute of North America Research Paper. 57: 1–65.
  24. ^ Boulton, G. S. (1967). "The Development of a Complex Supraglacial Moraine at the Margin of Sørbreen, Ny Friesland, Vestspitsbergen". Journal of Glaciology. 6 (47): 717–735. doi:10.3189/S0022143000019961. S2CID 127729549.
  25. ^ Fyffe, Catriona L.; Woodget, Amy S.; Kirkbride, Martin P.; Deline, Philip; Westoby, Matthew J.; Brock, Ben W. (August 2020). "Processes at the margins of supraglacial debris cover: Quantifying dirty ice ablation and debris redistribution". Earth Surface Processes and Landforms. 45 (10): 2272–2290. Bibcode:2020ESPL...45.2272F. doi:10.1002/esp.4879. S2CID 218998898.
  26. ^ Nakawo, M.; Iwata, S.; Watanabe, O.; Yoshida, M. (1986). "Processes which Distribute Supraglacial Debris on the Khumbu Glacier, Nepal Himalaya". Annals of Glaciology. 8: 129–131. Bibcode:1986AnGla...8..129N. doi:10.3189/S0260305500001294. S2CID 246062157.
  27. ^ Stewart, Robert A.; Bryant, Deborah; Sweat, Michael J. (March 1988). "Nature and origin of corrugated ground moraine of the Des Moines lobe, Story County, Iowa". Geomorphology. 1 (2): 111–130. Bibcode:1988Geomo...1..111S. doi:10.1016/0169-555X(88)90010-4.

Further reading

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  • Easterbrook, D. J. (1999), Surface processes and landforms (Second ed.), Upper Saddle River, N.J.: Prentice Hall, ISBN 9780138609580
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