Rock Identification

Geology Field Trip

Igneous Rocks

Plutonic
When magma solidifies, it becomes igneous rock.  The magma may cool and solidify under the Earth's surface, creating an intrusive igneous rock.  The grains of minerals are large enough to see because they cooled slowly underground.  Rocks that formed far underground, very slowly, are also called plutonic.  Granite is one of the most common igneous rocks.  It makes up the continental crust and many mountains are made of granite that has been forced upwards.  

Granite
Granite 

Uses of Granite

Mount Rushmore granite

Diorite contains less quartz than granite (or none at all) and is darker in color.  
Gabbro is a very dark intrusive igneous rock containing no quartz and forms at the bottom of the magma chamber. 

Volcanic Rocks
Extrusive (or volcanic) rocks, form when magma cools above the Earth's surface.  The rapid cooling means that the crystals usually cannot be seen with the naked eye.  Basalt is probably the most common volcanic rock and is mainly composed of iron and magnesium-rich minerals.  It makes up most of the oceanic crust.  The magma flows from Kilaeua Volcano in Hawaii cool rapidly into basalt.  

Andesite also contains these minerals, but has a higher percentage of feldspars, aluminum silicates.  
Rhyolite is light in color with a chemical composition equivalent to granite.

Other volcanic rocks:


Sedimentary Rocks  

Sediment comes from igneous rocks that have been exposed to weathering and erosion.  If the sediment becomes lithified (bonded together), it forms a sedimentary rock.  These are the most common, known as detrital sedimentary rocks, in order from the most coarse to finest particle size:
The Garden of the Gods

Chemical sedimentary rocks form by precipitation of minerals from solution:
Rocks formed from plant or animal remains are called organic or biochemical sedimentary rocks:


Metamorphic Rocks


Some rocks, either igneous or sedimentary, may be transformed into a metamorphic rock.  The changes take place under the earth's surface.  The variation in color and chemical composition is due to the conditions in which the rocks formed, including heat, pressure, tectonic forces, effects from water and time.  Metamorphic rocks may be either foliated or nonfoliated.  The foliated rocks have a platy, sheet-like, or parallel appearance.  

Foliated
Schist 
Schist

Non-Foliated
                                        

  

Sammy Rocks


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