We are now back to volcanoes (: and although todays lessons was not thrilling it was definately a vast improvement upon that of Belfast. We have also been set an essay, nothing like ensuring we don't relax-- it hadnt even been 24 hours after the exam! oh well such as life.
Today was a lesson running through what we were doing before christmas:
There are 2 key types of magma Basaltic and Rhyolitic this is judged upon how much silica (SiO2) is found within the magma, see the table below.
Summary Table | |||||
Magma Type | Solidified Rock | Chemical Composition | Temperature | Viscosity | Gas Content |
Basaltic | Basalt | 45-55 SiO2 %, high in Fe, Mg, Ca, low in K, Na | 1000 - 1200 oC | Low | Low |
Rhyolitic | Rhyolite | 65-75 SiO2 %, low in Fe, Mg, Ca, high in K, Na. | 650 - 800 oC | High | High |
- Hawaiian - These are eruptions of low viscosity basaltic magma. Hawaiian Eruptions are considered non-explosive eruptions. Very little pyroclastic material is produced.
|
i feel there is a good chance i may add to it soon!
No comments:
Post a Comment