In the lowest layers
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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.
strata
If the strata layers are folded or tilted then the older rocks can be found on top of the younger rocks in a cross-section.
The densest form of interplanetary debris are asteroids. Asteroids are basically thick rocks that come together from the interplanetary dust and debris that sometimes fall to Earth.
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uplifted mountains
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.
when rocks are thrown in it
older than the one above it
sideways
The layers in sedimentary rocks are called strata.
Strata (singular: stratum)
strata
They're called strata. Strata less than 1cm thick are Laminae.
Strata refers to distinct layers or divisions within a rock formation or other material. Stratification refers to the process of arranging or forming these layers. In essence, strata are the actual layers, while stratification is the process of layering.