Sedimentary rocks are rocks compossed of fragments that have been deposited compacted and cemented
Sedimentary rocks can be:
chemically weathered- Through carbon dioxide reacts with rainwater and pore water in soil to form carbonic acid
physically weathered- also known as mechanically weathering, exfoliation sometimes reffered as 'onion skin weathering'. in hot desserts there is marked difference beetween hot day time and cold night time temperatures. different minerals expand and contract by different amounts during heating and cooling, causing the rock to disintegrate.
biologically weathered- caused by plant roots braking rocks and from burrowing from animals such as rabbits and worms.
if there is any questions i would more than happy to answer
Sunday, 27 February 2011
Saturday, 26 February 2011
Types of volcanoes: shield volcanoes and strato
There are two types of volcanoes these are shield volcanoes and strata volcanoes, I will write about the two seperatly.
Shield volcano
Shield volcanoes have gentle slopes, which are less than 10 degrees, and have entirly basalt lava flow. They have fissure eruptions which means magma reaches the surface along , linear cracks or fissures. these fissures erupt almost constantly and are not explosive due to the low pressures.
Strato Volcanoes
Strato volcanoes form the largest percentage, over 60%, of the earths individual volcanoes. they are very explosive and look like your typical volcanoes with steep sides. The lava that is erupted has high viscosity as it slightly cooler than fissure eruptions. strato volcanoes also contain lots of felsic minerals such as feldspar and contains high amounts of sillica.
products of volcanoes igneous rocks
There are various products from volcanoes not just lava as you may think.
products are:
. volcanic gasses - from the volcanoes these include sulphur and co2
. lava flows
. pyroclastic materials- this happens when magma is forcefully or explosively ejected into the atmosphere as particles called pyroclasts . these include ash blocks of magma and lapilli which are beetween 2mm and 64mm
where do you find pyroclasts?
distabution by grain size - bombs and blocks of rock close to volcanoes and ash further away
distrabution by wind - the prevaling wind means the products of a volcanoe are mostly in that direction
products are:
. volcanic gasses - from the volcanoes these include sulphur and co2
. lava flows
. pyroclastic materials- this happens when magma is forcefully or explosively ejected into the atmosphere as particles called pyroclasts . these include ash blocks of magma and lapilli which are beetween 2mm and 64mm
where do you find pyroclasts?
distabution by grain size - bombs and blocks of rock close to volcanoes and ash further away
distrabution by wind - the prevaling wind means the products of a volcanoe are mostly in that direction
intrusive igneous rocks
intrusive means the rocks have been formed in the earth.
Minor intrustions - cool at the hypabyssal depth below the surface and includes sills and dykes
major intrusions - are plutonic and cool depth below the surface and include batholiths
chilled margins are where the ingneous rock has colled rapidly so have few chrystals, a baked margin is the country rock where it was heated by the intrustion and altered
Minor intrustions - cool at the hypabyssal depth below the surface and includes sills and dykes
major intrusions - are plutonic and cool depth below the surface and include batholiths
chilled margins are where the ingneous rock has colled rapidly so have few chrystals, a baked margin is the country rock where it was heated by the intrustion and altered
classification of rocks
sedimentry rocks - a rock compossed of fragmants that have been deposited compacted and cemented
igneous rocks - rocks formed from magma within the earth
metamorphic rocks - formed by the recrystallisation of other rocks in a solid state
classification of igneous rocks
chrystal grain size - bigger longer taken to cool
silica percentage % - the more silica a mineral contains the lighter it is
igneous rocks - rocks formed from magma within the earth
metamorphic rocks - formed by the recrystallisation of other rocks in a solid state
classification of igneous rocks
chrystal grain size - bigger longer taken to cool
silica percentage % - the more silica a mineral contains the lighter it is
characteristics of rock forming mineral
you can characterise a rock/mineral by several ways;
These are:
Habit- shape of minerals/rock
Colour - can be used for some minerals but is inacurate as mineral can be found in many colours
Hardness- mohos scale of hardness measures ressistance to scratching, the scale ranges from 1-10
Lustre- ability to reflect light
Specific gravity- ratio of mass of a mineral compared with the mass of an equal volume of water
These are:
Habit- shape of minerals/rock
Colour - can be used for some minerals but is inacurate as mineral can be found in many colours
Hardness- mohos scale of hardness measures ressistance to scratching, the scale ranges from 1-10
Lustre- ability to reflect light
Specific gravity- ratio of mass of a mineral compared with the mass of an equal volume of water
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