Gypsum is formed underwater, usually between layers of shale and limestone. When the water evaporates and the area dries, the gypsum becomes solid "rock" gypsum.
Location. Different layers of rock/soil tell a roughly chronological tale of the past, barring cataclysm. There are enough undisturbed sites worldwide that a mosaic can be discerned. Good question.
every thing
it forms a sedimentary rock
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The shale layer is the youngest in the series. In undisturbed rock layers, the Law of Superposition states that the youngest layer is on top and the oldest is at the bottom. So, in this case, the limestone would be the oldest layer, followed by sandstone, and then shale.
Probably Kaibab limestone, Coconino sandstone, Hermit shale, Redwall limestone, Muav limestone, Vishnu Schist, and other layers.
Sedimentary rock, such as limestone, chalk, slate and sandstone.
Limestone is a sedimentary rock formed from the accumulation of calcium carbonate, while sandstone is made up of sand-sized grains of minerals like quartz and feldspar. Limestone is typically softer and more porous than sandstone, which is harder and more resistant to weathering. Sandstone often has visible layers or bedding, while limestone can contain fossils and may exhibit a more uniform appearance.
Geologists know that rock layers are undisturbed by examining the relationships between the different layers. If the layers are parallel and show no signs of folding, tilting, or faulting, they are likely undisturbed. Additionally, the presence of index fossils can help date the layers and determine if they have been disturbed.
They are sedimentary rock. Four examples being chalk, sandstone, limestone and slate.
Probably Kaibab limestone, Coconino sandstone, Hermit shale, Redwall limestone, Muav limestone, Vishnu Schist, and other layers.
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.
Gneiss is neither limestone nor sandstone. Gneiss is a metamorphic rock that forms from the transformation of pre-existing rocks such as granite or sedimentary rocks under high heat and pressure. The resulting gneiss typically exhibits banded layers of minerals.
The rock layers will be easily visible.
The undisturbed rock layers are horizontal and in order of age from youngest nearest the surface to oldest at the bottom of the rock unit.
The most common type of rock on a cliff face is sedimentary rock, such as sandstone or limestone. These rocks are often found in layers, which can erode at different rates, leading to the formation of cliffs.