Continent-continent convergence
The ice age and the subsequent sliding and melting of glaciers account for the mountain belt bounded on either side by craters
The sequences of sedimentary rocks in cratons are typically thin and are relatively undeformed or gently warped. The sequences in mountain belts, meanwhile, are thick and extensively folded and faulted.
The part of a continent that is stable and forms the central mass of the continent; typically Precambrian.
Areas of ancient continental interiors are called cratons.
According to Wikipedia, a craton is an "...old and stable part of the continental lithosphere" -- the earth's outermost rocky shell. Kimberlite pipes, where diamonds are commonly found, are sometimes rooted in cratons. You can read more by following the link, below.
Cratons, large geologically stable areas in continental interiors.
Continent-continent convergenceThe ice age and the subsequent sliding and melting of glaciers account for the mountain belt bounded on either side by craters
The sequences of sedimentary rocks in cratons are typically thin and are relatively undeformed or gently warped. The sequences in mountain belts, meanwhile, are thick and extensively folded and faulted.
The sequences of sedimentary rocks in cratons are typically thin and are relatively undeformed or gently warped. The sequences in mountain belts, meanwhile, are thick and extensively folded and faulted.
Cratons contain the ancient crust of igneous rocks.
cratons
The part of a continent that is stable and forms the central mass of the continent; typically Precambrian.
Old Continental cratons with diatremes or in sediments derived from such.
Areas of ancient continental interiors are called cratons.
According to Wikipedia, a craton is an "...old and stable part of the continental lithosphere" -- the earth's outermost rocky shell. Kimberlite pipes, where diamonds are commonly found, are sometimes rooted in cratons. You can read more by following the link, below.
Cratons, large geologically stable areas in continental interiors.
In old areas of continental crust called "cratons" in volcanic structures called "kimberlite pipes".
It was formed when cratons collided and welded together.I dont know if he is right but i think that he is really good I dont know what it means.