To easily read my blog and not miss a post--SUBSCRIBE VIA E-MAIL

You can always comment using the "ANONYMOUS BUTTON."

Or just CLICK ON ONE OF THE LITTLE SQUARES at the bottom of my posts to let me know what you think. Easy-Peasy!

And Don't Forget To FEED MY FISH!!!! (at the bottom of the side column)

Monday, October 18, 2010

Cinder, Composite, Shield or Lava Dome?

When geologists group volcanoes, it’s usually into four main kinds.

The Hawaiian islands are made up of shield volcanoes.

You may hear a variety of terms used when people talk about volcanoes. What’s the difference between the terms? Here are a few definitions that may help you.

Caldera—The large basin-shaped depression formed when the roof of the magma chamber collapses because massive amounts of magma have erupted. Some are formed when a huge explosion removes the upper part of the volcano.

Crater—A depression around the orifice of a volcano.

Magma—Molten rock within the earth’s crust that is capable of extrusion onto the surface.

Lava—Molten rock that has extruded onto the surface.

Lava Tube—A tunnel formed under a lava flow.

Pahoehoe—As the lava flows along the tube, a top crust will form. As the lava flows underneath, the top begins to wrinkle. This is pahoehoe.

Aa—Sometimes the pahoehoe will shift as it cools and loses gas, forming sharp edges and spiny projections.

If you would like to see some photos of pahoehoe and aa flows, or would like to read more about the Hawaiian volcanoes, here is a site to visit.

Thank you for visiting. Please visit again on Thursday and don't forget to check a box below or leave a comment!

No comments:

Post a Comment

I love hearing from my readers! Mahalo for visiting and commenting. Aloha! --Cheryl