Rock evidence refers to the geological clues that help scientists understand Earth's history, such as how different rock layers were formed, what types of organisms lived in the past, and how the Earth's surface has changed over time. By studying rock evidence, scientists can reconstruct past environments and events that have shaped the planet.
A sill is a slab of volcanic rock formed when magma squeezes between layers of rock. It is typically horizontal and parallel to the surrounding rock layers. Sills are distinguishable from dikes, which cut across the rock layers.
Those rock layers are quite colorful.
The sandstone layer is older than the basalt. The older rock cannot be on top of the younger rock. The sandstone and the basalt (or basalt dike) are both deposited at the same depth.
A fault is considered the youngest feature in a rock body because it displaces the surrounding rock layers, indicating that it occurred after those layers were formed. Geologists use principles such as superposition and cross-cutting relationships to determine the relative ages of geological features. If a fault cuts through other rock layers, it must be younger than those layers. Additionally, any sediment or material that accumulates in the fault zone itself can provide further evidence of its relative youth.
You learn that expose rock layers are the evidence that there was erosion and disturbances going on in that area.
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Fossils are found most commonly in layers of sedimentary rock. This type of rock begins to form when water and wind form layers of sand and silt.
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It is determined because in layers of rocks the fossils are found so the layers of rocks give information to the scientist about the age of a fossil so like that the relative age of a fossil is determined.
sedimentary, igneous, metamrphic -con
geologic colums
Rock evidence refers to the geological clues that help scientists understand Earth's history, such as how different rock layers were formed, what types of organisms lived in the past, and how the Earth's surface has changed over time. By studying rock evidence, scientists can reconstruct past environments and events that have shaped the planet.
Aquifers are permeable layers of rock that have non permeable layers of rock under them so water remains in the permeable layers
Sedimentary rock provides evidence of the different changes in the earth's environments. Evidence is deposited in layers which have characteristics of wet, dry, hot or cold climates.
Rock layers that are forming are stratifying.