That would depend on the meaning of 'undisturbed'.
Factors such as wind, ice, and warder contribute to sedimentary build up. As this occurs older layers of sedimentary rock are driven lower while newer layers replace them closer to the surface.
In an undisturbed strata, the oldest layers are at the bottom. It's called the law or principle of superposition.
When undisturbed sedimentary rock layers occur in horizontal layers, it is referred to as the principle of original horizontality. This geological principle states that sedimentary rocks are initially deposited in horizontal layers due to the influence of gravity. If the layers are found tilted or folded, it indicates that geological processes, such as tectonic activity, have occurred after their formation.
True. In an undisturbed sequence of sedimentary rocks, the bottom layer is the oldest and the top layer is the youngest due to the principle of superposition, which states that in any undisturbed sequence of rock layers, the youngest rocks are at the top and the oldest are at the bottom.
In an undisturbed rock sequence, the oldest rock layer is typically found at the bottom. This is due to the principle of superposition, which states that in sedimentary rock layers, younger layers are deposited on top of older ones. Thus, as you move upwards through the sequence, the age of the rock layers decreases.
The principle of superposition states that in undisturbed sedimentary rock layers, the youngest layers will be on top and the oldest layers will be at the bottom. This principle forms the basis of relative dating in geology.
The Law of Superposition is a geologic principle that states in a sequence of undisturbed sedimentary rock layers, the oldest layer is at the bottom and the youngest layer is at the top. It is not a type of rock; rather, it is a fundamental concept used in geology to determine the relative ages of rock layers.
Stratification
the principle of superposition, which states that in an undisturbed sequence of rock layers, the youngest layer is on top and the oldest is on the bottom. This principle helps geologists determine the relative ages of rock layers based on their position in a stratigraphic sequence.
The layer of rock at the bottom of a sedimentary rock is older. This is due to the principle of superposition, which states that in an undisturbed sequence of rock layers, the oldest rocks are at the bottom and the youngest are at the top.
Limestone is not an igneous rock, it is sedimentary.
Scientists can use sedimentary rock to determine a fossil's relative age by examining the layers in which the fossil is found. The principle of superposition states that in an undisturbed sequence of sedimentary rock layers, the oldest layer is at the bottom and the youngest layer is at the top. By identifying the layer in which the fossil is located, scientists can approximate its relative age compared to other fossils and rock layers.