Drumlin



A drumlin, from the Irish word droimnín ("little ridge"), first recorded in 1833, in the classical sense is an elongated hill in the shape of an inverted spoon or half-buried egg formed by glacial ice acting on underlying unconsolidated till or ground moraine. Assemblages of drumlins are referred to as fields or swarms; they can create a landscape which is often described as having a 'basket of eggs topography'.

Morphology
Drumlins occur in various shapes and sizes, including symmetrical (about the long axis), spindle, parabolic forms, and transverse asymmetrical forms. Generally, they are elongated, oval-shaped hills, with a long axis parallel to the orientation of ice flow and with an up-ice (stoss) face that is generally steeper than the down-ice (lee) face.

Drumlins are typically between 250 and 1,000 m long and between 120 and 300 m wide. Drumlins generally have a length to width ratio of between 1.7 and 4.1 and it has been suggested that this ratio can indicate the velocity of the glacier. That is, since ice flows in laminar flow, the resistance to flow is frictional and depends on area of contact; thus, a more elongated drumlin would indicate a lower velocity and a shorter one would indicate a higher velocity.

Occurrence
Drumlins and drumlin swarms are glacial landforms composed primarily of glacial till. They form near the margin of glacial systems, and within zones of fast flow deep within ice sheets, and are commonly found with other major glacially-formed features (including tunnel valleys, eskers, scours, and exposed bedrock erosion).

Drumlins are often encountered in drumlin fields of similarly shaped, sized and oriented hills. Many Pleistocene drumlin fields are observed to occur in a fan-like distribution. The long axis of each drumlin is parallel to the direction of movement of the glacier at the time of formation. Inspection of aerial photos of these fields reveals glacier's progress through the landscape. The Múlajökull drumlins of Hofsjökull are also arrayed in a splayed fan distribution around an arc of 180°. This field surrounds the current lobe of the glacier and provide a view into the past, showing the previous extent and motion of the ice.

Composition
Drumlins may comprise layers of clay, silt, sand, gravel and boulders in various proportions; perhaps indicating that material was repeatedly added to a core, which may be of rock or glacial till. Alternatively, drumlins may be residual, with the landforms resulting from erosion of material between the landforms. The dilatancy of glacial till was invoked as a major factor in drumlin formation. In other cases, drumlin fields include drumlins made up entirely of hard bedrock (e.g. granite or well-lithified limestone). These drumlins cannot be explained by the addition of soft sediment to a core. Thus, accretion and erosion of soft sediment by processes of subglacial deformation do not present unifying theories for all drumlins—some are composed of residual bedrock.

Formation
There are two main theories of drumlin formation. The first, constructional, suggests that they form as sediment is deposited from subglacial waterways laden with till including gravel, clay, silt, and sand. As the drumlin forms, the scrape and flow of the glacier continues around it and the material deposited accumulates, the clasts align themselves with direction of flow. It is because of this process that geologists are able to determine how the drumlin formed using till fabric analysis, the study of the orientation and dip of particles within a till matrix. By examining the till particles and plotting their orientation and dip on a stereonet, scientists are able to see if there is a correlation between each clast and the overall orientation of the drumlin: the more similar in orientation and dip of the clasts throughout the drumlin, the more likely it is that they had been deposited during the formation process. If the opposite is true, and there doesn't seem to be a link between the drumlin and the till, it suggests that the other main theory of formation could be true.

The second theory proposes that drumlins form by erosion of material from an unconsolidated bed. Erosion under a glacier in the immediate vicinity of a drumlin can be on the order of a meter's depth of sediment per year, depending heavily on the shear stress acting on the ground below the glacier from the weight of the glacier itself, with the eroded sediment forming a drumlin as it is repositioned and deposited.

A hypothesis that catastrophic sub-glacial floods form drumlins by deposition or erosion challenges conventional explanations for drumlins. It includes deposition of glaciofluvial sediment in cavities scoured into a glacier bed by subglacial meltwater, and remnant ridges left behind by erosion of soft sediment or hard rock by turbulent meltwater. This hypothesis requires huge, subglacial meltwater floods, each of which would raise sea level by tens of centimeters in a few weeks. Studies of erosional forms in bedrock at French River, Ontario, Canada, provide evidence for such floods. The recent retreat of a marginal outlet glacier of Hofsjökull in Iceland exposed a drumlin field with more than 50 drumlins ranging from 90 to(-) in length, 30 to(-) in width, and 5 to(-) in height. These formed through a progression of subglacial depositional and erosional processes, with each horizontal till bed within the drumlin created by an individual surge of the glacier. The above theory for the formation of these Icelandic drumlins best explains one type of drumlin. However, it does not provide a unifying explanation of all drumlins. For example, drumlin fields including drumlins composed entirely of hard bedrock cannot be explained by deposition and erosion of unconsolidated beds. Furthermore, hairpin scours around many drumlins are best explained by the erosive action of horseshoe vortices around obstacles in a turbulent boundary layer.

Semi-submerged or drowned drumlins can be observed where rising sea-levels flooded the low-lying areas in between drumlin ridges. The most notable example of this is Clew Bay in the west of Ireland, which contains hundreds of drumlin islands and islets. It was once a field of drumlins that was "drowned" following the Last Glacial Period.

Soil development on drumlins
Recently formed drumlins often incorporate a thin "A" soil horizon (often referred to as "topsoil" which accumulated after formation) and a thin "Bw" horizon (commonly referred to as "subsoil"). The "C" horizon, which shows little evidence of being affected by soil forming processes (weathering), is close to the surface, and may be at the surface on an eroded drumlin. Below the C horizon the drumlin consists of multiple beds of till deposited by lodgment and bed deformation. On drumlins with longer exposure (e.g. in the Lake Ontario drumlin field in New York State) soil development is more advanced, for example with the formation of clay-enriched "Bt" horizons.

Europe
Besides the Icelandic drumlins mentioned above, the literature also documents extensive drumlin fields in England, Scotland and Wales, Switzerland, Poland, Estonia (Vooremaa), Latvia, Sweden, around Lake Constance north of the Alps, in the Republic of Ireland (County Leitrim, County Monaghan, County Mayo and County Cavan), in Northern Ireland (County Fermanagh, County Armagh, and in particular County Down), Germany, Hindsholm in Denmark, Finland and Greenland.

North America
The majority of drumlins observed in North America were formed during the Wisconsin glaciation.

The largest drumlin fields in the world formed beneath the Laurentide Ice Sheet and are found in Canada — Nunavut, the Northwest Territories, northern Saskatchewan, northern Manitoba, northern Ontario and northern Quebec. Drumlins occur in every Canadian province and territory. Clusters of thousands of drumlins are found in:
 * Southern Ontario (along eastern end of Oak Ridges Moraine near Peterborough, as well as areas to the west near Dundas and Guelph )
 * Central-Eastern Ontario (Douro-Dummer)
 * Ontario – most of Northumberland County (between Rice Lake and Trenton, including Trent Hills)
 * The Thelon Plan of the Northwest Territories
 * Alberta – drumlins are located on the Morley Flats in the Stony Indian Reserve west of Calgary, as well as south of the Ghost Reservoir.
 * Saskatchewan – 80 km south of the east end of Lake Athabasca
 * Southwest of Amundsen Gulf in Nunavut
 * West Lawrencetown, Nova Scotia.

In the United States, drumlins are common in:
 * Central New York (between the south shore of Lake Ontario and Cayuga Lake)
 * The lower Connecticut River valley
 * Long Island
 * Manhattan
 * Eastern Massachusetts
 * Eastern Connecticut in Windham and New London Counties
 * The Monadnock Region of New Hampshire
 * Michigan (central and southern Lower Peninsula)
 * Minnesota
 * The Puget Sound region of Washington state
 * Wisconsin.

Asia
Drumlins are found at Tiksi, Sakha Republic, Russia.

South America
Extensive drumlin fields are found in Patagonia. A major drumlin field extends on both sides of the Strait of Magellan covering the surroundings of Punta Arenas' Carlos Ibáñez del Campo Airport, Isabel Island and an area south of Gente Grande Bay in Tierra del Fuego Island.

Land areas around Beagle Channel host also drumlin fields; for example Gable Island and northern Navarino Island.

Antarctica
In 2007, drumlins were observed to be forming beneath the ice of a West Antarctic ice stream.