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Section 7.3 Student note
Section 7.3 Student note

... -crystal size depends on how slow it cooled -Intrusive igneous rocks formed well below the surface, ‘intruded into the rock’ -Extrusive rocks formed on the Earth’s surface (exited the Earth) -reach the surface through cracks in the crust/plates, or through erosion and uplift of layers of rock -figur ...
Rocks types
Rocks types

...  they are cemented by fine groundmass  It is more resistant ...
Untitled
Untitled

... Sandstone 'New Red Sandstone' Permian ...
Geology of Howth
Geology of Howth

... Their shells and bones which were made up of the mineral calcium carbonate built up to form sedimentary rocks known as limestones. There are different types of limestones in the Howth and Sutton areas because the sea in which they were deposited changed through time. Most of the limestones are rich ...
PLATE MOVEMENT AND CONTINENTAL GROWTH
PLATE MOVEMENT AND CONTINENTAL GROWTH

... APPALACHAIN AND URAL MTNS. – AGE OF ROCKS IN OCEAN BASINS – FOSSILS – LAND AREAS – TROPICAL AND POLAR REVERSES ...
Coal Measures
Coal Measures

... Coal Measures In the United Kingdom, ‘Coal Measures’ refer to layers of rock specifically from a time that geologists call the Upper Carboniferous period. The Coal Measures were deposited about 310 million years ago, and these layers of rock contain many coal seams. At this time in the Earth’s histo ...
Week 13: Earth Changes W-E-D
Week 13: Earth Changes W-E-D

... forces that build up land such as deposition ...
Geological Past - Government of New Brunswick
Geological Past - Government of New Brunswick

... of the deposits are being mined today, whereas others remain to be discovered. But how and when did they form? New Brunswick's geological past began about 1 billion years ago when the world was already 3.5 billion years old. The continents as we know them did not exist. Instead, there was a giant su ...
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Geology of Great Britain



The geology of Great Britain is renowned for its diversity. As a result of its eventful geological history, Great Britain shows a rich variety of landscapes across the constituent countries of England, Wales and Scotland. Rocks of almost all geological ages are represented at outcrop, from the Archaean onwards.
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