Welcome!

Why hello there and welcome to my Geography blog. I'm an A-level student from Somerset studying Environmental Science, Geography and Archaeology. I should probably explain how this blog has come about. During my first lesson of the new year my teacher exclaimed that I should start a “What I learnt this week…” blog. I thought this would actually be a good idea to help for revision and “consolidate my learning” which is what the teachers always tell me to do and it might (hopefully) help other people doing geography as well. So this is my geography blog.

There are two of us!

So i am a geography geek and got added so i can blog too. what can i say, i love it absolutely love it! i'm not really that clever (that's a lie she is!) but it doesnt stop a love i have for the subject, i also study environmental science and geology.

My portrait photo should reflect what topic I'm studying at the time. If I remember to change it... If you have any questions or want to talk to us about anything Earth Sciences related please don't hesitate to ask!

Saturday, 5 February 2011

volcanoes

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 TypeSolidified RockChemical CompositionTemperatureViscosityGas Content
BasalticBasalt45-55 SiO2 %, high in Fe, Mg, Ca, low in K, Na1000 - 1200 oCLowLow


RhyoliticRhyolite65-75 SiO2 %, low in Fe, Mg, Ca, high in K, Na.650 - 800 oCHighHigh


 
  • Hawaiian - These are eruptions of low viscosity basaltic magma. Hawaiian Eruptions are considered non-explosive eruptions.  Very little pyroclastic material is produced.

  • Strombolian - These eruptions are characterized by distinct blasts of basaltic to andesitic magma from the vent. Strombolian eruptions are considered mildly explosive.

  • Vulcanian - These eruptions are characterized by sustained explosions of solidified or highly viscous andesite or rhyolite magma from a the vent.  Eruption columns can reach several km above the vent, and often collapse to produce pyroclastic flows.  Widespread tephra falls are common.  Vulcanian eruptions are considered very explosive.

  • Pelean - These eruptions result from the collapse of an andesitic or rhyolitic  lava dome. Pelean eruptions are considered violently explosive.

  • Plinian - These eruptions result from a sustained ejection of andesitic to rhyolitic magma into eruption columns that may extend up to 45 km above the vent.  Eruption columns produce wide-spread fall deposits with thickness decreasing away from the vent, and may exhibit eruption column collapse to produce pyroclastic flows.  Plinian ash clouds can circle the Earth in a matter of days. Plinian eruptions are considered violently explosive.


i feel there is a good chance i may add to it soon!

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