there is little leaching:) novanet
The upper layer of desert soil is rich in minerals because the lack of rainfall prevents leaching of nutrients deeper into the soil. This accumulation of minerals over time leads to the development of nutrient-rich topsoil in desert regions.
the lack of rainfall in deserts prevents minerals from being leached out through water runoff, allowing them to accumulate in the soil over time. Additionally, the breakdown of rocks and minerals by wind and weathering contributes to the mineral content in desert soils. This combination of factors can result in the upper layer of desert soil being rich in minerals.
the lack of water in deserts prevents leaching, allowing minerals to accumulate near the surface. Additionally, minerals in the soil may come from the weathering of rocks and minerals in the surrounding area, contributing to its richness.
The desert receives little rainfall that would normally dissolve and wash away minerals.
The layer composed of peridotite is the mantle, which is located between the Earth's crust and core. Peridotite is the main rock type found in the upper mantle and is rich in minerals such as olivine and pyroxene.
The layer of Earth that contains iron-rich silicate rock is the mantle. The upper mantle is composed of silicate minerals rich in iron and magnesium, such as olivine and pyroxene. This layer lies beneath the Earth's crust and extends to a depth of about 2,900 kilometers.
The Earth layer that is made of peridotite is the mantle. Peridotite is a type of rock rich in olivine and pyroxene minerals that primarily makes up the upper mantle beneath the Earth's crust.
The layer classified based on chemical composition that is also found in the asthenosphere is the upper mantle. The upper mantle lies beneath the Earth's crust and is composed mainly of silicate minerals rich in magnesium and iron. This layer is partially molten, allowing for the plasticity that characterizes the asthenosphere, enabling the movement of tectonic plates.
The upper mantle is composed mainly of silicate minerals such as olivine, pyroxene, and garnet. These minerals are rich in magnesium and iron, which are the main elements found in the upper mantle.
The Atacama Desert in Chile is known for being rich in minerals, particularly copper and lithium. Its unique arid conditions and geological features contribute to the concentration of these valuable resources. The desert's mineral wealth has made it a significant area for mining activities, especially in the context of global demand for lithium in battery production.
The O horizon is the top layer made of organic material like plant litter. The A horizon is rich in organic matter and minerals, where most root activity occurs. The B horizon is known as the subsoil, containing minerals leached from the upper layers.
Topsoil consists primarily of the A horizon, which is the uppermost layer rich in organic matter and nutrients. Below the A horizon is the B horizon, which contains minerals leached from the upper layers.