Tag: climate and season cycle

Aeolian soil is the wind deposited materials that consist primarily of sand or silt-sized particles. These materials tend to be extremely well sorted and free of coarse fragments. CaO content in such soils varies from 1.0-1.5 per cent.

Formation of soil is called pedogenesis. Soil formation is nothing but the process of soil formation from its parental material. In most of the cases colouration, mineral composition and texture of the soil is determined by its parental material. In addition to the soil parent material, soil formation is also dependent upon other prevailing processes like Climate, Relief etc.

Desertification is a type of land degradation in which a relatively dry area of land becomes a desert, typically losing its bodies of water as well as vegetation and wildlife.

Cyclonic rainfall Mediterranean sea,

Summer Season, Winter Season, Rainy Season all are the seasons of Rajasthan.

A famine is a widespread scarcity of food, caused by several factors including war, inflation, crop failure, population imbalance, or government policies. 

Churu Coldest Place In Rajasthan At 1.7 Degrees Celsius. Jaipur: Cold wave conditions prevailed in parts of Rajasthan where Churu remained the coldest place with a minimum temperature of 1.7 degrees Celsius followed by Mount Abu.

The hottest of all seasons, summer extends in Rajasthan from April to June. During summers, the temperature in Rajasthan is very high and it ranges somewhere between 32 degree Celsius and 46 degree Celsius. The place has an average temperature of 38 degree Celsius. The only place in the state which has a lower temperature during this season is Mt Abu. At day, hot winds blow from the west and these winds are called ‘Loo’.

Kaveri , is an Indian river flowing through the states of Karnataka and Tamilnadu. It is the fourth largest after Godavari and Mahanadi River in south India and the largest in Tamil Nadu which on its course, bisects the state into North and South. Originating in the foothills of Western Ghats at Talakaveri, Kodagu in Karnataka it flows generally south and east through Karnataka and Tamil Nadu and across the southern Deccan plateau through the southeastern lowlands, emptying into the Bay of Bengal through two principal mouths in Poompuhar, Tamil Nadu. Amongst the river valleys, the Kaveri delta forms one of the most fertile regions in the country.