geology mineral (definition) 1. naturally occurring, 2. inorganic solid 3. with a specific chemical...
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Geology
Mineral (definition)1. naturally occurring, 2. inorganic solid 3. with a specific chemical composition 4. a definite crystalline structure
Minerals can form from the cooling of magma which is the molten material found beneath Earth’s surface as magma rises closer to the surface the molten compounds no longer move freely and they begin to interact chemically to form minerals
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Geology
Minerals form by combining elements together to create compounds. Each compound is unique and has specific properties that separate it from other compounds
Minerals are like rocks because all rocks are made of minerals
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Mineral Properties
Streak is easily determined by rubbing the mineral across an unglazed porcelain plate
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Mineral Properties
Streak is used to distinguish pyrite from gold
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Mineral Properties
Luster is the way a mineral reflects light from its surface and is caused by differences in mineral chemical compositions
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Mineral Properties
Either metallic or nonmetallic (dull, pearly, waxy, silky)
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Mineral Properties
Texture describes how a mineral feels to the touch Rough, smooth, ragged, greasy, soapy,
glassy
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Mineral Properties
Hardness is a measure of how easily a mineral can be scratched and is determined by the arrangement of it’s atoms.
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Mineral Properties
The Mohs hardness scale is used to compare a sample to the hardness of ten known minerals
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Mineral Properties
Cleavage determines whether a mineral will split easily and evenly along one or more flat planes
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Mineral Properties
Mica has perfect cleavage in one direction
Halite has cubic cleavage (3 planes)
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Mineral Properties
Fracture means the mineral is tightly bonded and breaks with rough or jagged edges Quartz has fracture
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Mineral Properties
Specific Gravity compares the weight of the mineral to an equal volume of water at 4 degrees C
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Mineral Properties
Special Properties such as light reflection and reactions to acids are also useful tools
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Mineral Properties
Calcite fizzles when in contact with HCl
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Mineral Properties
Calcite also can cause double images
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Mineral Properties
Magnetite will attract iron
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Mineral Properties
Sulfur produces a rotten egg odor
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Geology
Small crystals means the magma cooled rapidly
Large crystals means the magma cooled more slowly
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Geology
Silicates are the most abundant group (96%) containing the two most abundant elements in the crust Silicon (Si) and Oxygen (O)
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Geology
Quartz and Feldspar are the most abundant minerals found in Earth’s crust
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Geology Carbonates are minerals composed of
one or more metallic elements with the carbonate compound CO3 ( 1 atom of carbon and 3 atoms off oxygen)
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Geology
Carbonates are the primary minerals in rocks such as limestone, coquina, and marble
Limestone Coquina Marble
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Uses for Earth Materials
Nearly every single thing we use today comes from Earth directly or indirectly. The following is a list of minerals and ores
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Uses for Earth Materials
Name of mineral/ore Use(s)Quartz (mineral) Glass, watches
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Uses for Earth Materials
Feldspar (mineral) Toothpaste
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Uses for Earth Materials
Calcite (mineral) Neutralizing acids
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Uses for Earth Materials
Mica (mineral) Lampshades, insulation, makeup
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Uses for Earth Materials
Pyrite (ore) Iron
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Uses for Earth Materials
Talc Baby powder
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Uses for Earth Materials
Bauxite Aluminum
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Virginia’s Important Resources Coal Energy
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Virginia’s Important Resources Gravel/stone (all) Road
Construction
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Virginia’s Important Resources Limestone Concrete
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Virginia’s Important Resources Granite Building materials
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Virginia’s Important Resources silica electronics
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Virginia’s Important Resources zirconium & titanium advanced
metallurgy
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What are Rocks?
A rock is a naturally occurring solid mixture of one or more minerals, or organic matter
Rocks are classified by how they are formed, their composition, and texture
Rocks change over time through the rock cycle
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Igneous Rocks
Igneous rock begins as magma. Magma can form:
When rock is heated When pressure is released When rock changes composition
Magma freezes between 700 °C and 1,250 °C
Magma is a mixture of many minerals
http://www.fi.edu/fellows/payton/rocks/create/igneous.htm
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Igneous Rocks
Felsic: light colored rocks that are rich in elements such as aluminum, potassium, silicon, and sodium
Mafic: dark colored rocks that are rich in calcium, iron, and magnesium, poor in silicon
Coarse-grained: takes longer to cool, giving mineral crystals more time to grow
Fine-grained: cools quickly with little to no crystals
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Igneous Rocks
Felsic
Mafic
Coarse-Grained
Fine-Grained
Granite
Gabbro Basalt
Rhyolite
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Igneous Rocks
Intrusive Igneous Rocks: magma pushes into surrounding rock below the Earth’s surface
Extrusive Rocks: forms when magma erupts onto the Earth’s surface (lava), cools quickly with very small or no crystals formed
http://www.windows.ucar.edu/tour/link=/earth/geology/ig_intrusive.html&edu=high&fr=t
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Igneous Rocks
Obsidian
What is Obsidian?
Obsidian is a dark-colored volcanic glass that forms from the very rapid cooling of molten rock material. It cools so rapidly that crystals do not form.
Obsidian is a dark-colored volcanic glass that forms from the very rapid cooling of molten rock material. It cools so rapidly that crystals do not form.
Is this rock Felsic or Mafic?
Is it fine-grained or coarse-grained?
Is this rock Intrusive or Extrusive?
Mafic, fine grained, extrusive
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Sedimentary Rocks
http://www.fi.edu/fellows/payton/rocks/create/sediment.htm
Sedimentary rock is formed by erosion
Sediments are moved from one place to another
Sediments are deposited in layers, with the older ones on the bottom
The layers become compacted and cemented together
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Sedimentary Rock
Sedimentary Rocks are formed at or near the Earth’s surface
No heat and pressure involved
Strata – layers of rock
Stratification – the process in which sedimentary rocks are arranged in layers
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Sedimentary Rock
Clastic – made of fragments of rock cemented together with calcite or quartzBreccia is a term most
often used for clastic sedimentary rocks that are composed of large angular fragments (over two millimeters in diameter).
The spaces between the large angular fragments can be filled with a matrix of smaller particles or a mineral cement that binds the rock together.
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Sedimentary Rock
Chemical sedimentary – minerals crystallize out of solution to become rock
Rock Salt is a chemical sedimentary rock that forms from the evaporation of ocean or saline lake waters. It is also known by the mineral name "halite". It is rarely found at Earth's surface, except in areas of very arid climate. It is often mined for use in the chemical industry or for use as a winter highway treatment. Some halite is processed for use as a seasoning for food. The specimen shown above is about two inches (five centimeters) across.
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Sedimentary Rock
Limestone is a sedimentary rock composed primarily of calcium carbonate (CaCO3) in the form of the mineral calcite. It most commonly forms in clear, warm, shallow marine waters.
It is usually an organic sedimentary rock that forms from the accumulation of shell, coral, algal and fecal debris.
Organic sedimentary – remains of plants and animals
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Sedimentary Rock
Organic sedimentary – remains of plants and animals
Coal is an organic sedimentary rock that forms from the accumulation and preservation of plant materials, usually in a swamp environment.
Coal is a combustible rock and along with oil and natural gas it is one of the three most important fossil fuels.
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Metamorphic Rock
http://www.fi.edu/fellows/payton/rocks/create/metamorph.htm
Meaning to change shape
Changes with temperature and pressure, but remains solid
Usually takes place deep in the Earth
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Metamorphic Rocks
Contact Metamorphism – heated by nearby magma
Increased temperature changes the composition of the rock, minerals are changed into new minerals
Hornfels is a fine-grained non-foliated metamorphic rock produced by contact metamorphism http://www.windows.ucar.edu/tour/link=/earth/geology/meta_contact.html&ed
u=h igh&fr=t
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Metamorphic Rocks
Regional Metamorphism – pressure builds up in rocks that is deep within the Earth
Large pieces of the Earth’s crust collide and the rock is deformed and chemically changed by heat and pressure
http://www.windows.ucar.edu/tour/link=/earth/geology/meta_regional.html&edu=high&fr=t
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Metamorphic Rock
Foliated - contain aligned grains of flat minerals
Gneiss is foliated metamorphic rock that has a banded appearance and is made up of granular mineral grains.
It typically contains abundant quartz or feldspar minerals.
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Metamorphic Rock
Non-Foliated – mineral grains are not arranged in plains or bands
Marble is a non-foliated metamorphic rock that is produced from the metamorphism of limestone.
It is composed primarily of calcium carbonate.
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Metamorphic Rock
Determine if the following rock samples are foliated or non-foliated:
Amphibolite Quartzite Phyllite
Foliated