e/Trafalgar Moraine

Information
has gloss	eng: The Trafalgar Moraine is a geological landform in northern Oakville, Ontario, Canada. It is a subtler topological feature than the better-known Oak Ridges Moraine, primarily because it was formed as an end moraine at the terminus of a glacial ice sheet, instead of between two retreating ice lobes (known as interlobate). The ice sheet pushed material to form the ridge, which is composed of Halton Till sediment, rich in silt and clay. By contrast, the Oak Ridges Moraine is primarily sand and gravel. The ridge was probably formed during a pause in the retreat of the ice sheet.
lexicalization	eng: Trafalgar Moraine
instance of	c/Moraines of Canada