Idk but you can research I hope it help
B. Accidental spills at extraction sites and during transport.
Answer:
Its given as below.
Explanation:
Mantle convection is a type of current that raises from the mantle plumes with lava or magma and its rising lava reaches the earth through volcanic eruption and further through the burning of plates inside the mantel, it is directly connected with at of the plates on earth as its due to this effect that the ring of fire is dotted by earthquakes of all types. The Hawaiian volcanoes are on this line also thus are highly explosive and viscous lava flowing from vents, the zone of most active volcanoes.
Answer:
Upon contact with the continental plate, the oceanic plate, being denser, begins to sink into the asthenosphere. This sinking of the plate is called subduction. Once in the asthenosphere, the oceanic plate melts due to high temperatures. The melts thus formed come to the surface in the form of volcanic eruptions, forming a volcanic chain of subduction.
When two plates come in contact, a collision is created, which leads to earthquakes or sediment wrinkles, followed by their elevation and mountain formation.
<em>Thus, the mountain ranges were formed: the American Cordillera and the Himalayan mountains.</em>
Answer:
The Deccan plateau is a topographically variegated region located south of the Gangetic plains -the portion lying between the Arabian Sea and the Bay of Bengal- and includes a substantial area to the north of the Satpura Range, which has popularly been regarded as the divide between northern India and the Deccan. The plateau is bounded on the east and west by the Ghats, while its northern extremity is the Vindhya Range. The Deccan's average elevation is about 2,000 feet (600 m), sloping generally eastward; its principal rivers, the Godavari, Krishna, and Kaveri, flow from the Western Ghats eastward to the Bay of Bengal. Tiruvannamalai in Tamil Nadu is often regarded as the Southern gateway of Deccan plateau.
Explanation:
