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If rock layers are not horizontal, then some force must have diturbed them after they were fomed.
Meteorite. An asteroid is probably a better description of the thing that hit Earth.
Garnet schist-- as well as mica schist--can be found anywhere where clay rock with some calcite content-- such as siltstone or a mudstone, for example-- can be compressed (via metamorphism) and consequently sqeezed into rock-like layers.
some of the ways geologists study rocks in the field are they look for ''outcrop areas'', or ''outcrops'', which are outside places where much rock, mineral, crystal or gem is exposed.
Those are deposition layers influenced by wind or moving water.
Rivers,rock outcrops,and slate.
Firstly, it is hard for animals to have access to sufficient food sources on rock platforms. Also, being in an exposed position makes them more vulnerable to predators such as eagles and hawks. there is no shelter on rock platforms. Some animals do prefer rocky outcrops (such as the rock wallabies of Australia), but these are outcrops and hillsides, not single platforms.
Usually along a fault the rock layers are broken and displaced in some manner so that the rock layers are not continuous across the fault.
Not exactly. Some metamorphic rocks have foliation, which can appear similar to the layers of sedimentary rock. Foliation develops from mineral grains being oriented by pressure, rather than the deposition of layers.
The wavy features found on some sandstones are the build up of the different layers of rock the rock has produced over the decades.
When magma flows between rock layers and spreads upward, it sometimes pushes the overlying rock layers into a dome. The base of the intrusion is parallel to the rock layer beneath it.
If rock layers are not horizontal, then some force must have diturbed them after they were fomed.
Meteorite. An asteroid is probably a better description of the thing that hit Earth.
Garnet schist-- as well as mica schist--can be found anywhere where clay rock with some calcite content-- such as siltstone or a mudstone, for example-- can be compressed (via metamorphism) and consequently sqeezed into rock-like layers.
The crust alone contains millions of different layers of sedimentary rock. For the layers of the Earth, some of which are rock and some of which are not, see the related link below.
some of the ways geologists study rocks in the field are they look for ''outcrop areas'', or ''outcrops'', which are outside places where much rock, mineral, crystal or gem is exposed.
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.