Weathering, Erosion, and Masswasting.
Actually, the larger the load a river has, the more sediment it can carry. A river's capacity to transport sediment is often determined by factors like its velocity and volume of water flow. When a river has a larger load, it can transport more sediment downstream.
Fine sediment would be easier to compact compared to coarse sediment. Fine sediment particles are smaller and have more surface area contact, allowing them to interlock and compress more tightly when pressure is applied. Coarse sediment particles are larger and have more space between them, making it harder to compact.
The igneous rock that, when weathered, could produce sediment composed of potassium feldspar, quartz, and amphibole is granite. Granite is a coarse-grained rock primarily composed of these minerals, and upon weathering, it breaks down into smaller particles, contributing to sediment in the environment. This sediment can then be transported and deposited, forming sedimentary rock or contributing to soil formation.
A tall building on a mountain of granite is less likely to be damaged by an earthquake compared to a valley of sediment. Granite is a more stable and solid foundation that can help dissipate the seismic waves, whereas sediment in the valley is more prone to liquefaction and amplification of seismic waves, making it more vulnerable to damage.
The ease with which water flows through the open spaces in a rock or sediment indicates the permeability of the rock or sediment. Permeability refers to the ability of fluids to flow through the rock or sediment. A more permeable rock or sediment will have higher porosity and allow for better fluid flow.
an older river deposits more sediment.
Actually, the larger the load a river has, the more sediment it can carry. A river's capacity to transport sediment is often determined by factors like its velocity and volume of water flow. When a river has a larger load, it can transport more sediment downstream.
The smaller the load a river has the more sediment it can carry is false. When the river has more energy, it is able to carry a larger load, therefore more sediment.
The greater the time that stream sediment is transported, the greater the probability that the sediment will become more rounded and well-rounded due to abrasion and attrition processes.
Fine sediment would be easier to compact compared to coarse sediment. Fine sediment particles are smaller and have more surface area contact, allowing them to interlock and compress more tightly when pressure is applied. Coarse sediment particles are larger and have more space between them, making it harder to compact.
The steeper the slope, the faster the water will run, and the more sediment it can carry.The larger the volume of water that is moving, the more sediment it can carry with it.
The steeper the slope, the faster the water will run, and the more sediment it can carry.The larger the volume of water that is moving, the more sediment it can carry with it.
The steeper the slope, the faster the water will run, and the more sediment it can carry.The larger the volume of water that is moving, the more sediment it can carry with it.
The steeper the slope, the faster the water will run, and the more sediment it can carry.The larger the volume of water that is moving, the more sediment it can carry with it.
The steeper the slope, the faster the water will run, and the more sediment it can carry.The larger the volume of water that is moving, the more sediment it can carry with it.
The steeper the slope, the faster the water will run, and the more sediment it can carry.The larger the volume of water that is moving, the more sediment it can carry with it.
The igneous rock that, when weathered, could produce sediment composed of potassium feldspar, quartz, and amphibole is granite. Granite is a coarse-grained rock primarily composed of these minerals, and upon weathering, it breaks down into smaller particles, contributing to sediment in the environment. This sediment can then be transported and deposited, forming sedimentary rock or contributing to soil formation.