description Bradford Kames Overview
The Bradford Kames are a notable geological formation in Canada, distinguished by their steep-sided mounds of glaciofluvial sand and gravel.
help Bradford Kames FAQ
What are the Bradford Kames made of?
The Bradford Kames are steep-sided mounds formed from glaciofluvial sand and gravel. Those sediments were deposited by meltwater associated with retreating glacial ice.
What does the word kame mean in geology?
A kame is a mound or irregular hill of sand and gravel left by glacial meltwater. Kames often occur near former ice margins and can appear in groups or ridges.
How are the Bradford Kames different from drumlins?
Kames are mainly meltwater deposits of sand and gravel, while drumlins are streamlined hills shaped largely by moving glacial ice. Their steep, irregular form is therefore a useful clue that the Bradford Kames are kame landforms.
Why are the Bradford Kames important geologically?
They preserve evidence of glacial meltwater and the former position of ice during deglaciation. Their sediment and shape help explain how the local landscape developed after the last Ice Age.
explore Explore More
Reviews & Comments
Write a Review
Be the first to review
Share your thoughts with the community and help others make better decisions.
