Soil texture is defined as the relative ratios of particle diameter that comprise the soil.
Texture refers to the particle size. The average size of a soil particle is determined by the relative proportions of sand, silt, and clay in the soil. The average size of soil particles geography increases as the quantity of sand in the soil increases, and the resulting soil gets coarser in texture. Conversely, increasing the quantity of clay in the soil reduces the average diameter of the soil particles, resulting in a finer-textured soil. Locate the percentages of clay and silt on the triangular textural diagram's silt and clay side lines, respectively. Then, in the first scenario, draw lines thru these points inwards, perpendicular to the clay side.
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<em>B. Area near a sea having flat land and low relief</em>
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<em>A coastal plain is flat, low-lying land adjacent to a sea coast.</em>
Troposphere is the layer where the air is thin as well as very warm
They occur along a fault line or where two tectonic plates meet
