Yes, massive areas of Earth are covered by sedimentary rocks. A good geology map will tell you what rocks are in your area.
Reverse Grading.
Sedimentary rocks are commonly found near bodies of water such as rivers, lakes, and oceans where deposition and accumulation of sediment occur. They can also form in areas where wind-blown sediment accumulates, such as deserts and coastal dunes. Additionally, sedimentary rocks can form from the consolidation of organic materials in environments like swamps and marshes.
Stratus Clouds are clouds that cover large areas and form in layers.
Sedimentary rock in Michigan is primarily the result of the very large shallow sea that covered the state in the distant past.
Almost the entire continent of Antarctica is desert. Africa and Australia also have large areas covered by deserts.
The principle that indicates rock layers separated by a valley were once continuous is called the Principle of Original Continuity. This principle suggests that sedimentary layers are deposited in continuous sheets over large areas. When a valley forms, it can erode through these layers, but the original continuity of the layers prior to erosion implies they were once part of a larger, uninterrupted sequence.
Large areas of sea floor are covered with thick layers of sediment containing calcium due to the accumulation of calcium carbonate shells and skeletons from marine organisms over time. This process, known as biomineralization, contributes to the formation of limestone and other calcium-rich sediments.
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A plutonic dome is found in areas of flat-lying sedimentary rocks that sloped up to create a roughly circular shape. Its core is made up of plutonic or igneous rocks that arched up the overlying sedimentary layers.
Large flat areas of the ocean floor are called abyssal plains. These regions are typically covered in thick layers of fine sediment and are among the flattest, most featureless parts of the ocean floor. Abyssal plains are found at depths between 3,000 and 6,000 meters.
It most likely means that each layer of the stratificaton represents a time of flood, when a large layer of fresh silt was washed into the body of water, settling to the bottom over pre-existing layers.
Index fossils are used to correlate rock layers over large geographic areas. These fossils are commonly found in distinct layers and can be used to determine the relative ages of rocks in different locations. By identifying the same index fossil in different rock layers, geologists can establish correlations between widely separated areas.