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#1. The classic route begins with the weathering and erosion of sedimentary, igneous, or metamorphic rocks. Through these processes, larger rock is broken up into smaller particles which are transported by moving water, ice, gravity or wind, and deposited at the bottom of a lake, a river delta, an ocean, or similar location where further movement is restricted or slowed down. The rock particles can range in size from boulders to clay particles less than .002 mm in diameter. If these rock particles are covered by additional particles, eventually the weight from above will start the process of lithification. Lithification is the compaction and cementation of particles which form rock. Compaction squeezes out the fluids and space that exist between the particles, and cementation results when the fluids that are squeezed out are replaced with minerals that crystallized from the fluids. Once cementation occurs, the new sedimentary rock has been formed. Rocks formed in this manner include sandstone, shale, mudstone, breccia, and conglomerate and are called clastic sedimentary rocks. #2. Organic sedimentary rocks like some limestones and coal are formed largely from the remains of once living organisms. Chalk and fossiliferous limestones are formed from the skeletons of marine organisms. Coal is formed from vegetation that previously existed in swampy and marshy waterlogged soils which prevented their full decay after their death. As their remains piled up and were covered by more and more deposits, they gradually underwent compaction and cementation as described in #1. above. #3. Sedimentary rocks can also form when minerals in a body of water have so saturated the water that they precipitate out, like a cloud that is so full of moisture that it pours out rain. Some limestones are formed in this manner as the mineral calcite precipitates out of a saturated solution and undergoes the process of compaction and cementation. The supersaturated solutions can also be caused by evaporation of a body of water high in mineral content. As the water evaporates, the mineral percentage of the remaining solution becomes higher and higher, until the mineral crystallizes. Rocks such as rock salt and rock gypsum are formed in this manner. Sedimentation from precipitation and evaporation form rocks called chemical sedimentary rocks.


Sedimentary rocks are formed when sediments are tightly compacted together and compressed of a period of time. The longer they are left, the bigger the bonds (crystals) between the particles gets.

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Some sedimentary rocks form as a result of processes acting on the remains of once living organisms.

Others form from the deposit of loose sediments that acculate on Earth's surface.

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Q: How land derived sedimentary rocks formed?
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What is the texture of inorganic land derived sedimentary rocks?

what is the texture of all inorganic land derived sedimentary rocks


What is the texture of all inorganic land derived sedimentary rocks?

what is the texture of all inorganic land derived sedimentary rocks


Can sedimentary rocks form under the ocean or on land only?

Sedimentary rocks formed under oceans, but the ocean may no longer be there. The Great Lakes region was once all under water and has much sedimentary rock.


Rocks formed from sediments deposits?

Sedimentary rocks are formed from sediment deposits (gravel, sand, silt, clay) over long periods of time either on land or in water (lakes, oceans). As more and more sedimentary layers are deposited, the newer layers exert pressure on the older layers, which compacts the loose particles and cements them together - forming sedimentary rocks. Sedimentary rocks can also be formed through the precipitation of dissolved minerals to form limestone or dolomite.


What type of sedimentary rock is formed from weather land particles of rocks and minerals?

Sandstone is one possible form.


Crystalline sedimentary rocks?

All sedimentary rocks are made by of deposition of the products of erosion either on land or more usually in water. Crystalline sedimentary rocks can be produced by the evaporation of a brine.


Do you ever think we will run out of sedimentary rocks. Why or why not.?

We can only run out of them if we ship them off the planet. They are being formed as we speak, under the surface of the land and at the bottom of the ocean.


How much of the Earth's surface is covered by sedimentary rocks?

Although sedimentary rocks are estimated to comprise only 5% of crustal rock, 75-80% of the land surface is covered by them.


What rock type are most common at earths surface?

Sedimentary Rocks. 75% of rocks exposed to the surface are sedimentary. Basalt is the most common type of rock and it is igneous.


Is breccia foliated?

Breccia is an inorganic land-derived sedimentary rock. It is clastic (fragmental), but not foliated. Breccia is composed of mostly quartz, feldspar, and clay minerals; it may contain fragments of other rocks and minerals.


Why are sedimentary rocks found as a thin layer covering most of the the continental igneous rocks?

Sedimentary rocks are the result of broken down igneous rocks so they cover up most of igneous rocks.


How the earth form?

The Earth's surface has not always had the same form or with the same continents as it has now. A process of plate tectonics has the continents drifting (at an incredibly slow but measurable pace) across the surface. They split apart and ram back together to form new land masses. The Himalayan mountains were formed when the Indian land mass pushed into the southern boundary of the ancient Asian land mass, folding the crust and forming mountains. Other mountains were formed by similar processes.The Earth's crust was originally formed from igneous rocks, much like the rocks formed when lava cools. These rocks gradually weathered away into sand and silt, which were deposited in the valleys and on the ocean bed. Here, they were compressed into sedimentary rocks such as sandstone and shale. The earth's surface is constantly changing, and many sedimentary rocks were later uplifted to form new mountains.