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They indicate a depositional event.
a rock specimen of a particular depositional enviroment
Conglomerate rocks can sometimes have spaces between the rocks and other times be filled in with a matrix cement, like concrete. A common place to find conglomerate is near a river. Rivers, because they move at different velocities, are able to transport and deposit rocks of all different sizes.
Cross-bedding refers to inclined layers in sedimentary rock that were formed as a result of wind or water driven ripples or dunes in the original depositional environment.
Yes, sedimentary rocks can contain bands or layers of minerals. These bands are often formed through various processes such as sediment deposition, compaction, and cementation. The minerals within these bands can vary in composition and can provide valuable information about the depositional environment and the history of the rock.
a high energy depositional environment is one in which enough energy was present to transport large materials such as rocks and boulders. a low energy depositional environment like a stream is only able to transport materials such as fine sands.
A Sliding Rocks of Racet
They indicate a depositional event.
the reason is because rocks can have different depositional environments and diagenesis history.
An sedimentary enviorment is when all the rain rains in a puddle and all the rocks settle and a sedimentary enviorment develops/forms. This is my thinking/opinion.
a rock specimen of a particular depositional enviroment
shallow sea
Conglomerate rocks can sometimes have spaces between the rocks and other times be filled in with a matrix cement, like concrete. A common place to find conglomerate is near a river. Rivers, because they move at different velocities, are able to transport and deposit rocks of all different sizes.
Cross-bedding refers to inclined layers in sedimentary rock that were formed as a result of wind or water driven ripples or dunes in the original depositional environment.
They can be found in Death Valley National Park.
depositional contacts occur between rocks that formed when sediments were deposited on other sediments.fault contacts are usually shown as thick black lines on geologic maps
rocks big and small glide across a mirror flat landscape.