Erosion
When pressure is applied to pieces of sediment, compaction takes place. Compaction is the process in which pieces of sediment are under severe pressure and it becomes solid rock. Therefore, pressure turns pieces of sediment into sedimentary rock.
Erosion is important because without it material wouldn't be able to move from one location to another.
According to uniformitarians, sediments are laid down slowly over millions of years. Eventually, conditions change and the sediments harden to form rocks. The conditions during which the sediments were laid down determine the type of sediment, which in turn determines the kind of rock formed.
As water hits the coastline it slowly takes dirt and sediments back into the ocean with it causing the erosion process. Also if it rains and water runs off the coastline it is able to carry sediments that way.
Catastrophists believe that the majority of sedimentary rocks where formed quickly in a catastrophic global flood (Noah's flood). The dynamics associated with the movement of the water and location of sedimentary deposits dictated the types of sedimentary rock produced. Compare this with the uniformitarian view wherein sediments are laid down slowly over vast periods of time. Throughout this period, conditions evolved and the sediments hardened to become sedimentary rock.
Erosion.
Pressure of water and other sediments.
The process in which sediments move slowly downhill, is called creep. It is common where freezing and thawing occur. As ice expands in soil, it pushed sediments up. Then as soil thaws, the sediments move farther downslope. Over time, creep can move large amounts of sediment, possibly causing damage to some structures
Sedimentary rock is formed from sediments are piled on top of one another, then compacted and cemented into rocks. Sandstone and limestone are examples of sedimentary rocks.
Sedimentary rock is formed from sediments are piled on top of one another, then compacted and cemented into rocks. Sandstone and limestone are examples of sedimentary rocks.
Sedimentary rock is formed from sediments are piled on top of one another, then compacted and cemented into rocks. Sandstone and limestone are examples of sedimentary rocks.
Sedimentary rock is formed from sediments are piled on top of one another, then compacted and cemented into rocks. Sandstone and limestone are examples of sedimentary rocks.
Sedimentary rock is formed from sediments are piled on top of one another, then compacted and cemented into rocks. Sandstone and limestone are examples of sedimentary rocks.
erosion
condensation is the process of gas slowly turning to a liquid.
When pressure is applied to pieces of sediment, compaction takes place. Compaction is the process in which pieces of sediment are under severe pressure and it becomes solid rock. Therefore, pressure turns pieces of sediment into sedimentary rock.
sediments are transported by ocean rift, streams, river currents, wind (air). they are deposited according to size. The largest sediments are deposited first. The sediments settle into the sand and are carried by the stream. Near the mouth of the stream where the water moves slowly the small sediments settle out. The larger sediments get carried by the river into the sea then the samller sediments. The sea water dissolved minerals and soak the sediments and cement together. This eventually forms sediments.