00:01
Hello there students today we're going to describe magma formation in a spreading center, a hot spot, and a subduction zone.
00:18
So let's begin with the spreading center.
00:29
So for the spreading center, it happens when the glyphum's spireate plates separate at the spreading center.
01:05
This is where hot plastic asphanosphere flows upwards, upward to fill the gap.
01:41
And as the as thin spires rises, the surrounding pressure drops and pressure release melting forms magna with a saltic position.
02:54
So that's that part.
03:02
Now we're going to get to, i'm going to talk about hot spots or mantle palm.
03:21
So how that happens and when the mantle form is a rising column of hot plastic...