Answer:
1. oceanic-oceanic boundaries
2. oceanic-continental boundaries
3. continental-continental boundaries
Explanation:
The three types of plate convergence are:
1. oceanic-oceanic boundaries: this occurs when two oceanic plates clash; thereby the heavier plate forms below the lighter plate resulting in dark, heavy, basaltic volcanic islands.
2. oceanic-continental boundaries: this occurs when there is a collision between oceanic and continental plates, resulting in the downward movement of oceanic plate, while the volcanic arc rises on land
3. continental-continental boundaries: this occurs due to the massive crust of slabs clashing against each other. Thereby leading to big mountains forming from folded, faulted, and thickened convergent boundaries
What role did Mohandas Gandhi play in Indian independence?
Answer:
Mahatma Gandhi was the leader of India's non-violent independence movement
Explanation:
Mahatma Gandhi was the leader of India's non-violent independence movement against British rule and in South Africa who advocated for the civil rights of Indians.
Rivers downcutting into a land surface, in the absence of other forces, usually tend to erode a ________-shaped form when viewed in cross-section across its valley. flat bottomed U delta V groove
Answer:
Rivers downcutting into a land surface, in the absence of other forces, usually tend to erode a V-shaped form when viewed in cross-section across its valley.
Explanation:
Rivers on steep surfaces tend to have a very high flow speed and the higher the slope of the terrain and the speed of the river, the greater the erosion power of these rivers. Under these conditions, a river can deepen its bed, creating a V-shaped valley, especially at the headwaters of the banks, where the erosion process is usually greater.
When seismographs are received at a station, the seismograph records the vibrations on paper in the form of lines. The height of the lines traced on paper is a measure of the energy released by the earthquake, also known as its
Answer:
Magnitude
Explanation:
The height of the lines traced on paper is a measure of the energy released by the earthquake, also known as its "Magnitude"
Usually, the Magnitude" of vibration can be calculated by multiplying the vibration value by itself (10 x 10) and then double it.
Hence, in this case, the correct answer to the question is "Magnitude"