Cosmogenic nuclide romance may be used to establish prices of ice-sheet thinning and economic downturn, history of moraines, and also the chronilogical age of glacially eroded bedrock floors

How do we time rocks?

Cosmogenic nuclide romance enables you to set rates of ice-sheet thinning and economic slump, the years of moraines, and also the period of glacially eroded bedrock materials.

For glaciation, essentially the most mon implementing cosmogenic nuclide dating is date the coverage age of glacially shipped rocks.

Cosmogenic nuclide relationship employs the communications between cosmic radiation and nuclides in glacially moved boulders or glacially eroded bedrock to give you era offers for stone publicity at the Earth’s exterior. It confides in us how long the rocks have-been found at the area, like, on a moraine.

Its a very good way of immediately matchmaking glaciated countries. Truly particularly useful in Antarctica[1], considering various factors[2]: