why is found laterite soil in meghalaya plateau?
Answers
Explanation:
konsa class hein baur konsa ch hein
Answer:
Laterite soil is reddish to yellow in color with a lower content of nitrogen, phosphorus, potassium, lime, and magnesia with 90–100% of iron, aluminum, titanium, and manganese oxides. The word laterite has been derived from the Latin word that means brick. The laterite soil is formed under conditions of high temperature and heavy rainfall with alternate wet and dry periods, which leads to leaching of soil, leaving only oxides of iron and aluminum. It lacks fertility due to a lower base-exchanging capacity and a lower content of nitrogen, phosphorus, and potassium. However, proper irrigation and use of fertilizers make it suitable for growing crops, such as tea, coffee, rubber, cinchona, coconut, etc. It also supports growth of paddy (rice) in low-lying areas. Laterite soil is one of the valuable sources for building material, as it can be easily cut with a spade but hardens like iron when exposed to air. In India, laterite soil is widespread, covering over 10% of the total geographical area, namely on the summits of the Western Ghats, Eastern Ghats (Rajamahal Hills, Vindhyas, Satpuras, and Malwa Plateau), southern parts of Maharashtra, parts of Karnataka, Andhra Pradesh, West Bengal Orissa, Jharkhand, Kerala, Assam, and Meghalaya