agents of gradation are
-sea waves
-rivers
-winds
-glaciers
Weathering is the process by which rocks and minerals break down into smaller pieces, while gradation refers to the sorting and transportation of these weathered particles by natural agents like water, wind, or ice. Weathering contributes to gradation by producing smaller particles that can be easily transported and sorted by these agents, leading to the formation of sedimentary deposits.
Agents of gradation refer to the natural forces or processes that cause erosion and weathering of landforms, such as water, wind, and ice. These agents work to gradually reshape the Earth's surface by breaking down rock and carrying sediment from one place to another. Over time, they play a significant role in shaping the landscapes we see today.
The process involved in gradation is called "sorting," which refers to the separation and categorization of sediments based on their size, shape, and density. Sorting plays a key role in determining the texture and composition of sedimentary deposits.
Weathering and gradation are closely related processes in geology, particularly in the context of erosion and sedimentation. Weathering refers to the breakdown and alteration of rocks and minerals at or near the Earth's surface due to physical, chemical, and biological processes. These processes include mechanical weathering (such as frost action, abrasion, and root wedging) and chemical weathering (such as dissolution, oxidation, and hydrolysis). Weathering breaks down rocks into smaller fragments and alters their mineral composition, preparing them for transportation and deposition. Gradation refers to the process by which weathered rock and mineral particles are transported and deposited by natural agents such as water, wind, ice, or gravity. This transportation and deposition of sediment result in the formation of sedimentary deposits and landforms. Gradation involves three main stages: erosion (removal of sediment), transportation (movement of sediment), and deposition (settling of sediment). The relationship between weathering and gradation is that weathering processes break down rocks into smaller particles and alter their composition, making them more susceptible to erosion and transportation by natural agents. As weathering continues, it produces sediment that is transported and deposited through gradation processes, leading to the formation of sedimentary rocks and various landforms such as valleys, river deltas, and beaches. In summary, weathering prepares rocks and minerals for erosion and transportation, while gradation involves the movement and deposition of weathered material to form sedimentary deposits and shape the Earth's surface.
The exception is glaciers. Glaciers are not sediment transporting agents; they are instead agents of erosion that can carry sediment as they move across the landscape. Rivers, wind, and waves are all examples of sediment transporting agents.
Gradation has a few different agents. The agents of gradation are as follows: the sea's waves, rivers, winds, and glaciers.
Weathering is the process by which rocks and minerals break down into smaller pieces, while gradation refers to the sorting and transportation of these weathered particles by natural agents like water, wind, or ice. Weathering contributes to gradation by producing smaller particles that can be easily transported and sorted by these agents, leading to the formation of sedimentary deposits.
Agents of gradation refer to the natural forces or processes that cause erosion and weathering of landforms, such as water, wind, and ice. These agents work to gradually reshape the Earth's surface by breaking down rock and carrying sediment from one place to another. Over time, they play a significant role in shaping the landscapes we see today.
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.
repetition, alteration, and gradation? contrast, alteration, and placement? repetition, placement, and gradation? gradation, alteration, and isolation?
i like the word gradation < it is not hard dumbrain
Exogenetic forces are constantly working to bring about levelling or the gradation of land. They attempt to achieve a condition of balance between erosion and deposition which mean a graded position. The above forces operate through the process called 'Gradation'. Agents of gradation like rivers, glaciers winds, sea, waves and underground water perform their task with the help of the triple action of weathering, erosion and deposition. The filling up of elevated portions of the earth's surfaces is done by erosion. The filling up of depressions is done by deposition of the eroded material transported by the external agents of gradation as spoken earlier. A surface can be said to be a featureless plain if it is neither being filled nor levelled by exogenetic forces. However, such areas are never permanent as both endogenetic and exogenetic forces continue undoing the work of each other.
Since gradation means a series of successive changes, a sentence could be: "Within each family, there is a gradation of sports abilities." If you mean the definition of a minute change from one shade, tone, or color to another, then: "This picture has a gradation of green and blue."
The image below should show a smooth gradation of colors from white to gray.
Weathering is going to degrade or otherwise alter the nature, structure or composition of the actual insult or contaminant. Transportation mechanisms merely move the contaminant, unaltered, to other locations.
gradation
The driving force behind the movement of material from high to low areas if the force of gravity. But before that occurs, he rock material has to be broken (eroded), transported and deposited. This dynamic process is known as gradation and it is responsible for sculpting a variety of landforms.