The type of rock that forms where the remains of plants and animals are deposited in thick layers are called organic sedimentary rock.
Sedimentary rock, specifically organic sedimentary rock such as coal or limestone, forms where the remains of plants and animals are deposited in thick layers over time. These rocks are primarily made up of organic material and are created through the compression and cementation of these remains.
The process in which sediment is deposited in layers is called sedimentation. This occurs when particles settle out of a transporting medium, such as water or wind, and accumulate over time to form distinct layers of sediment.
It is called the 'Principle of Original Horizontality' and was proposed by the Danish geological pioneer Nicholas Steno (1638-1686). This principle states that layers of sediment are originally deposited horizontally. However, please note that it is now known that not all sedimentary layers are deposited purely horizontally and the principle is only an approximation of reality.
Any evidence of ancient life is called a fossil.
The wavy line between layers of rock is called a "cross bedding." Cross bedding forms when sediments are deposited at an angle due to currents, resulting in distinct layers that intersect at an angle to the horizontal bedding.
Fossils are remains of plants and animals that are deposited in thick layers of sediment over time. These remains can be bones, shells, footprints, or other traces that provide clues about past life on Earth. Fossils play a crucial role in helping scientists understand the history of life and evolution.
Sedimentary rock, specifically organic sedimentary rock such as coal or limestone, forms where the remains of plants and animals are deposited in thick layers over time. These rocks are primarily made up of organic material and are created through the compression and cementation of these remains.
Dead and decayed remains of plants and animals, called Humus.
The layers of soil that were naturally deposited are called, 'Horizons'.
The layers of soil that were naturally deposited are called, 'Horizons'.
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It is called sedimentation.
loess/dunes or aeolian deposits
The process in which sediment is deposited in layers is called sedimentation. This occurs when particles settle out of a transporting medium, such as water or wind, and accumulate over time to form distinct layers of sediment.
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Strata (singular: stratum)
The topmost rock layer is the one that was deposited last, as rock layers are typically deposited in a vertical sequence with the oldest layers at the bottom and the youngest layers at the top.