The slope of any flowing surface like lava, ash, pebbles is called the "angle of repose."
the philosophy of the lava supposodely forms from the specific material of the slope
A shield volcano has very broad, gentle slopes.
huge gently slopes
The slope of any flowing surface like lava, ash, pebbles is called the "angle of repose."
The parasitic cone is the name of the smaller vent-structure on the side of some volcanoes. This structure is not part of the central vent of a volcano.
the philosophy of the lava supposodely forms from the specific material of the slope
A shield volcano has very broad, gentle slopes.
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huge gently slopes
The slope of any flowing surface like lava, ash, pebbles is called the "angle of repose."
The slope of any flowing surface like lava, ash, pebbles is called the "angle of repose."
The slope of any flowing surface like lava, ash, pebbles is called the "angle of repose."
A cinder cone or cinder volcano is a steep hill of volcanic debris that gradually builds up from a volcanic vent. It can be on the slope of a larger stratavolcano or shield volcano.
very or highly viscous magmas formed it
the magma growing in size and large cracks forming
An island slope is analogous to a continental slope, but it is attached to an oceanic island (volcano) rather than attached to a continent. In simple terms, it is that portion of the sea floor that slopes from an island's shallows down to the deep ocean floor.