The buildup of sediment where a river empties into a slow-moving or nonmoving body of water is known as a/an a type of soil made almost entirely of windblown sediment is called the in soil comes from decaying plants and animals and their waste products. which is made up of tiny particles and drains water very poorly, is one of the main components of soil. a type of soil called peat is most likely to form in a/an water in the development of soil by carrying and nutrients from upper layers to lower layers. the of nutrients from soil is common in wet environments, like rain forests. quartz-rich parent material leads to the development of soils. the layers of soil composed mainly of organic matter are known as the and horizon. a layer of soil in which clay, iron, and other elements from the overlying soil accumulates is known as the horizon, or subsoil.

The buildup of sediment where a river empties into a slow-moving or non moving body of water is known as a/an  Delta. A type of soil made almost entirely of windblown sediment is called Loess. The organic matter in soil comes from decaying plants and animals and their waste products. Clay, which is made up of tiny particles and drains water very poorly, is one of the main components of soil. A type of soil called peat is most likely to form in a/an Coastal environment in Tropical setting. Water helps in the development of soil by carrying Mineral and nutrients from upper layers to lower layers. The Richness of nutrients from soil is common in wet environments, like rain forests. Quartz-rich parent material leads to the development of Sandy soils. The layers of soil composed mainly of organic matter are known as the O and A horizon. A layer of soil in which clay, iron, and other elements from the overlying soil accumulates is known as the B horizon, or subsoil.

Explanation:

Delta is said to be a body of sediments deposited when a river flows into a standing water, such as the sea or a lake.

Loess are wind blown deposits of silts and clay composed of quartz, feldspar and other minerals . Loess dominantly have high porosity.

Organic matters compose mainly of remains of animal and plants . After this plants and animals dies they form organic matter that adds to soil nutrients.

Clayey soil constitute very tiny particles that have a poor draining ability due to it tiny poor spaces .

Tropical setting in a coastal environment provides the necessary environments for soils like peat to form . It has abundant of plant remains . Moreover peat is the first stage of coal formation, containing moist and unconsolidated plant materials.

Minerals a part of what assist in the development of the soil .And it is usually carried down to the earth by water through a process called Leaching.

Richness of nutrient are common in tropical environment that are wet and support abundant life.

Sandy soil are formed from parents materials containing minerals such as feldspar and quartz.

Horizon O and A are known as topsoil and are mainly compose of animal and plants remains and large amount of minerals.

The subsoil or B Horizons contains mineral such as irons , clay minerals due to percolation from the top soils and it tends to accumulate here(subsoil).

most historians agree that gabriel mouton, the vicar of st. paul’s church in lyons, france, is the “founding father” of the metric system. he proposed a decimal system of measurement in 1670. mouton based it on the length of one minute of arc of a great circle of the earth (now called a nautical mile, 1852 meters). he also proposed the swing-length of a pendulum with a frequency of one beat per second as the unit of length (about 25 cm). a pendulum beating with this length would have been fairly easy to produce, thus facilitating the widespread distribution of uniform standards. over the years, his work was revised, improved, and extended by a number of french scientists.

the political sponsor of weights and measures reform in the french revolutionary national assembly was the bishop of autun, better known as talleyrand. under his auspices, the french academy appointed several committees to carry out the work of developing a usable system of weights and measures for france. one of the committees recommended a decimalized measurement system based upon a length equal to one ten-millionth of the length of a quadrant of the earth’s meridian (i.e., one ten-millionth of the distance between the equator and the north pole).