Tuesday 19 September 2017 photo 7/15
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A secondary school revision resource for GCSE Geography covering glacial landscapes and deposition landforms such as drumlins and erratics.
DRUMLIN An oval-shaped hill, largely composed of glacial drift, formed beneath a Variations in drumlin shape include spindle-like forms, two-tailed forms
The flow of ice over this deposited material then shapes it into the characteristic form of a drumlin. /**/ Erratics - These are large boulders that have been carried
Drumlin. Definition: An elongate hill, streamlined in the direction of ice flow and Whilst the classic drumlin is entirely a depositional form and the classic crag
Drumlins are commonly found in clusters numbering in the thousands. Often arranged in belts, they disrupt drainage so that small lakes and swamps may form
Drumlins. Drumlins are formed of till. They are elongated features that can reach a kilometer or more in length, 500m or so in width and over 50m in height.
22 Mar 2015 A better understanding of how drumlins form could lead to better reconstructions of the glaciological history of the region. If drumlin formation is
Drumlins are elongated, teardrop-shaped hills of rock, sand, and gravel that formed under moving glacier ice. They can be up to 2 kilometers (1.25 miles) long.
A drumlin, from the Irish word droimnin ("littlest ridge"), first recorded in 1833, and in the 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
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