This is apparent in the Lake District in Northwestern England where post-glacial sediments are normally between 4 and 6 metres deep.[2] These lakes are often surrounded by drumlins, along with other evidence of the glacier such as moraines, eskers and erosional features such as striations and chatter marks.
Hal ini ketara di Lake District di Barat Laut England kerana endapan pasca glasier adalah antara 4 dan 6 meter dalam.[2] Tasik ini sering dikelilingi drumlin, bersama bukti glasier yang lain seperti morain, esker dan ciri hakisan lain seperti penstriaan dan tanda gelatuk.
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