asial
sedimentary
igneous
metamorphic
An arch
We call them clastic rock also referred to us the sedimentary rock.
The threefold work of the agents of gradation includes erosion, transportation, and deposition. Erosion involves the wearing away of rocks and soil by natural forces such as water, wind, and ice. Transportation refers to the movement of these eroded materials from one location to another. Finally, deposition occurs when the transported materials settle and accumulate in new locations, forming various geological features.
Is called an unconformity.
What may happen to a rock/mineral is that the softer layers of a rock that are closest to the surface get weathered or eroded away while the harder center parts do not. This usually results in interesting and uneven rock shapes. Also, some weathering isn't exactly even in terms of the surface of a rock.
The depositing or placing of eroded material is called sedimentation. This process occurs when eroded particles settle and accumulate in a new location, often leading to the formation of sedimentary rocks over time.
Most eroded soil ends up in bodies of water like rivers, lakes, and oceans. It can also accumulate in areas like floodplains and deltas.
Eroded soil can be carried away by water, wind, or ice to various locations. It may be deposited in nearby bodies of water like rivers, lakes, or oceans, or settle on the land surface, altering the landscape. In some cases, eroded soil can also accumulate in valleys, forming sediment deposits.
Eroded soil can enter water bodies such as rivers, lakes, and streams, where they accumulate and cause sedimentation. This can lead to decreased water quality, habitat degradation, and reduced water flow capacity.
Approximately 15-20% of sediments eroded from the continents reach beyond coastal regions to the continental shelf and slope. The majority of eroded sediments tend to accumulate and deposit near the coast due to factors such as wave action and currents.
erosion results in a flattening of land form.
This process is called sedimentation. It occurs when eroded materials, such as sand, silt, and clay, are carried by water, wind, or ice, and then come to rest in a new location. Over time, these sediments can accumulate and form sedimentary rocks.
When a rock is weathered or eroded, it can become sedimentary rock. This process involves the breakdown and transportation of rock particles, which then accumulate and eventually form sedimentary rocks through processes like compaction and cementation.
Eroded sediment can end up in various places, such as rivers, lakes, oceans, or coastal areas. Sediment may accumulate at the bottom of these bodies of water, be transported downstream, or be deposited along the coastline. This process plays a crucial role in shaping landforms and ecosystems.
Detrital sediment consists primarily of mineral grains that were eroded from rocks on land. These mineral grains are transported by wind, water, or ice and eventually settle and accumulate to form detrital sedimentary rocks, such as sandstone or shale.
Materials eroded from the Abilene area would most likely be deposited downstream in rivers and streams as they flow towards larger bodies of water like lakes or the Gulf of Mexico. These sediments can accumulate in channels, riverbanks, delta regions, or in the floodplains of rivers and streams.
"Eroded" refers to the process of wearing away or deteriorating over time due to natural forces like water, wind, or ice. It often results in the gradual removal of material from a surface or landform.