This is a drawing of magma changing chemical composition within the chamber.
Click on image for full size
Magma Chamber
Magma consists of remelted material from Earth's crust and fresh material from other regions near the Earth's surface.
When magma is erupted onto the surface in the form of lava, it becomes silicate rock. On subsequent eruptions of the volcano, magma leaves the chamber composed of slightly different chemicals.
Thus, magma inside the chamber is a little like something left in the refrigerator too long. Each time the door is opened, it looks a little different.
Scientists examine the layers of lava flows of a volcano to study the chemical history of the magma inside the chamber.
You might also be interested in:
Minerals are the building blocks of rocks. They are non-living, solid, and, like all matter, are made of atoms of elements. There are many different types of minerals and each type is made of particular
...more If you could travel to the center of the Earth, you would find that it gets hotter and hotter as you travel deeper. The heat is naturally produced when radioactive elements break apart. Within the Earth’s
...moreVolcanoes form when hot material from below risesand leaks into the crust. This hot material, called magma, comes either from a melt of subducted crustal material, and which is light and buoyant after
...moreMars Global Surveyor made a measurement of pyroxene on the surface of Mars. Scientists looking at results from the Mars Pathfinder Rover's study of the rocks of Mars could not find evidence of pyroxene
...moreAsh is made of millions of tiny fragments of rock and glass formed during a volcanic eruption. Volcanic ash particles are less than 2 mm in size and can be much smaller. Volcanic ash forms in several ways
...moreCinder cones are simple volcanoes which have a bowl-shaped crater at the summit and only grow to about a thousand feet, the size of a hill. They usually are created of eruptions from a single opening,
...moreLava can move in broad flat lava flows, or it can move through tight channels or tubes. Lava flows tend to cool quickly and flow slowly. The fastest lava outside of channels moves at about 6 mi/hr an easy
...more