answersLogoWhite

0


Best Answer

When magma comes in contact with water first the water will stem because the magma is so hot the water is at or past its boiling point them the magma will harden fast because instead of its slow cooling prossess it is spead up from the waters temperature it is a big mess :) luvhh jasmine chanda

User Avatar

Wiki User

13y ago
This answer is:
User Avatar
More answers
User Avatar

Wiki User

15y ago

It is called a Volcano. The hot lava (magma) would flow to the areas surrounding the point from which it burst causing extensive damage to life and property.

This answer is:
User Avatar

User Avatar

Wiki User

12y ago

Formation of ocenic rigde

This answer is:
User Avatar

Add your answer:

Earn +20 pts
Q: What happens when rising magma breaks through the earth's crust?
Write your answer...
Submit
Still have questions?
magnify glass
imp
Related questions

What is the rising of regions of earths crust?

uplift


The rising and falling of Earths waters are the?

tides


What is a large elevation of the earths rising abruptly from the surrounding land?

hill


What is the rising of regions of the earths crust to higher elevations?

tectonic plates


What is the rising of regions of the earths crust higher elevation?

tectonic plates


What happens to air pressure when the barometer is rising?

The air pressure is rising.


What process breaks the fat globules and prevents them from rising to the top as cream?

Homogenization


What causes volcanoes and earthquacks?

Volcanoes are caused by the rising of magma in the earths mantle and earthquakes are caused by the colliding of the earths tectonic plates against one another.


What happens at the end of the book phoenix rising?

i dont no what happens i hated the book


What is most of the energy that heats earths atmosphere?

Heat from the sun rising as infrared radiation from the surface of the earth.


What happens on April 1836?

theeaster rising i think


What happens at constructive boundaries?

Creation of new crust through up swelling and out rising of magma to cover areas of sea floor spreading or lithospheric seperation.