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Probably because the subsurface ice in a glacier has recrystallized, much as the minerals in some sedimentary rock do when undergoing metamorphism.
By looking at the sedimentary and studying it
Geologists classify rocks by looking at their chemical and mineralogical composition then at the the size and shape of their component minerals then at any texture, pattern or grain that the rocks may display. They also classify them in relation to how they were formed.
Geologists based their findings because of fossils. Fossil distribution identifies the ancient areas of land & sea, & also determines the approximate shoreline.
Most rocks are subjected to weathering and erosion and it is difficult to see what a rock is made of if it is weathered. That is why geologists break rocks, to see a fresh example of the rock. It is also the best way of finding fossils in the field if you are working in an unfamiliar area.
Sedimentary, metamorphic and igneous.
Metamorphic rock is formed deep in the Earth's crust under tremendous heat and pressure. Fossiles are formed in sedimentary rock near the surface.
Geologists classify rocks into three groups. The first group are igneous rocks, the second are metamorphic rocks and the third are sedimentary rocks.
Probably because the subsurface ice in a glacier has recrystallized, much as the minerals in some sedimentary rock do when undergoing metamorphism.
Rocks are classified by mineral and chemical composition, by the texture of the constituent particles and by the processes that formed them. These indicators separate rocks into igneous, sedimentary, and metamorphic. They are further classified according to particle size. The transformation of one rock type to another is described by the geological model called the rock cycle.
Geologists classify metamorphic rocks by the arrangements of the grains that make up the rocks.
By looking at the sedimentary and studying it
A stratum.
Sedimentary
sedimentary,metormorphic , igneous .........
Yes.
Geologists classify rocks by looking at their chemical and mineralogical composition then at the the size and shape of their component minerals then at any texture, pattern or grain that the rocks may display. They also classify them in relation to how they were formed.