A rock column is made of many rock layers.
a break in a sedimentary sequence that does not involves a difference of inclination between the strata on each side of the break
The distance between Earth's topsoil layer and the solid rock layer beneath it can vary, but on average it is around 10-20 feet (3-6 meters). This layer of soil is called the regolith and sits above the bedrock, which is the solid rock layer.
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To determine whether the fault is older or younger than rock layer A, we can use the principle of cross-cutting relationships. If the fault cuts through rock layer A, it is younger than that layer, as it must have formed after the rock was deposited. Conversely, if rock layer A is found to be disrupted by the fault, then the fault is older. Therefore, examining the relationship between the fault and rock layer A is key to establishing their relative ages.
The asthenosphere is a layer of Earth's mantle upper consisting of hot rock with a plastic texture. It is beneath the rigid lithosphere. The magnetosphere is Earth's magnetic field.
Impermiable rock means nothing can go through it
a break in a sedimentary sequence that does not involves a difference of inclination between the strata on each side of the break
The distance between Earth's topsoil layer and the solid rock layer beneath it can vary, but on average it is around 10-20 feet (3-6 meters). This layer of soil is called the regolith and sits above the bedrock, which is the solid rock layer.
The layer that is partly weathered rock is called the saprolite layer. This layer is between the unaltered rock below and the soil layer above. Through weathering processes, the saprolite becomes broken down and forms the basis for soil formation.
mantle
Mesophere
Disconformity
Density would be the most noticeable difference between the rock and the model.
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its called the mantle
"mantel"