Because of the way the waves in the water move to lift the sediment...
Sediment sorting-Range of particle sizes layering- stratification of sediments and rocks texture- grain size grain Roundness- loss of edges on sediment grains (just took the Quiz of apex!)
Till is unsorted and unstratified glacial sediment, consisting of a mix of different-sized particles. It can contain a wide range of rock types and sizes, from clay to boulders. It is often deposited directly by the moving glacier as it retreats.
Sediment sorting refers to the uniformity of grain sizes in a sediment deposit, with well-sorted sediments having similar-sized grains. Layering refers to the stratification of sediment deposits into distinct layers. Texture refers to the size, shape, and arrangement of grains within a sediment. Grain roundness indicates the degree of abrasion a sediment particle has undergone, with well-rounded grains being smoother and more spherical.
Deposition is a geological process where sediment is deposited by air, water, or ice. It contributes to the formation of sedimentary rocks over time. Deposition occurs when the energy transporting sediment decreases, causing sediment to settle out of the transport medium.
The sediments with a mixture of sizes are known as poorly sorted sediments. This means that the particles have not been sorted by size and can range from fine to coarse within the same sediment deposit.
Sediment of smaller mass is easier for the power of wind to overcome the power of gravity in moving it from one place to another. Most sediment moved by wind that is tiny as sand.
well there is differnt sizes of the hailstones
No, sediment particles can vary in size from fine clay and silt to coarser sand and gravel. Sediment can contain a mixture of different particle sizes depending on the source and transport processes.
it is round and different sizes and is found in the forest
Sweden are different in many shapes and sizes they can be as big as a ladies but
The four types of sediment sizes are gravel (larger than 2 mm), sand (0.0625–2 mm), silt (0.004–0.0625 mm), and clay (smaller than 0.004 mm). These sizes are used to classify sediment based on their particle diameter.
Rocks are broken down into different sizes of sediment through processes like weathering, erosion, and transportation. Weathering breaks down rocks into smaller pieces, which are then carried away by erosion. The sediment is transported by wind, water, or ice, and deposited in new locations where it can accumulate and form layers of varying size.
Sediment size is primarily controlled by the energy of the transporting medium, such as water or wind. Higher energy environments can transport larger sediment sizes, while lower energy environments are limited to smaller sizes. Other factors, such as the type of sediment-producing rock and distance of transport, also play a role in determining sediment size.
It is a small prickly object with all different shapes and sizes.
To answer this, think about the way water moves and how ice moves. Now think of steady fast-moving streams of water and massive hulking glaciers scraping across the land. Streams push sediments along and sort them into normalized groups. Sand is separated from stones of different sizes. Glacier pick up rocks in their slow progress and deposit them later as the ice melts. The streams' depositions are very regular; the glaciers' depositions are very irregular.
Weathering and erosion transform rock into sediments of certain sizes.
A jumble of many sizes of sediment is typically referred to as "conglomerate." This sedimentary rock is composed of various clastic particles, ranging from gravel to sand and silt, often cemented together by minerals. Conglomerates form in environments where water or ice can transport and deposit diverse sediments, creating a mixture of different grain sizes. This rock type provides valuable insights into past geological processes and environments.