Term
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Definition
Naturally occurring Inorganic solid Orderly internal structure Definite chemical composition |
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A solid aggregate of minerals Rocks are composed of one or more minerals |
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Definition
• Made of one or more elements: 112 elements, 92 naturally occurring • Sometimes one single element-gold, silver |
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Which rocks are composed of non-minerals? |
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Definition
Pumice (frothy volcanic glass) Obsidian (non-crystalline substances) Coal (organic debris) |
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Definition
• By definition every specimen of mineral has the same internal structure • Internal structure can be expressed by external crystal structure |
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• Two different minerals can have the same composition but have different structures. |
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What is the atomic structure? |
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Definition
Nucleus Electrons Chemical bonding |
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Definition
• Consists of protons (+ charges) and neutrons |
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• Negatively (-) charged particles around the nucleus |
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• Forms a compound by combining two or more elements • Both ionic and covalent bonds typically occur in the same compound |
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What are the two types of bonding? |
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Definition
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Definition
• Atoms gain or lose outermost electrons to form oppositely charged ions |
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Definition
• Atoms share electrons to achieve electrical neutrality • Generally stronger than ionic bonds |
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What are the physical properties of minerals? |
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Definition
Crystal form Luster Color Streak Hardness Cleavage Fracture Specific Gravity |
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• External expression of a mineral’s internal structure • Often interrupted due to competition for space and rapid loss of heat |
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• The appearance or quality of light reflected off a mineral. • Metallic: pyrite or galena • Non-metallic can range from earthy to waxy to glassy. |
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• Unreliable because small impurities can alter colors. • Exotic (altered) • Inherent (natural/normal) coloration |
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• The color of the mineral powder when rubbed across a unpolished porcelain plate. • Streak does not vary as much as the color of minerals. |
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• Mohs hardness scale from 1 to 10. |
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• Tendency to break along planes of weak bonding • Produces flat, shiny surfaces |
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• Minerals that do not exhibit cleavage have a fracture • Most common are irregular, concoidal (like glass), fiberous, and splintering. |
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• Measured in grams per cubic centimeter |
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There are approx 4000 minerals, only a few dozen are abundant and only a few make up most rocks. |
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Most common rock forming minerals are silicates |
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Definition
Quartz K-spar, Plagioclase Feldspar Micas: Biotite and Muscovite Amphibole Pyroxene Olivine |
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Definition
Quartz Feldspar group Muscovite |
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Composed entirely of oxygen and silicon Very strong bonds Conchoidal fracture, no cleavage Hard and resistant to weathering Often forms hexagonal crystals |
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common mineral group Exhibit two directions of cleavage at 90 degrees Orthoclase (potassium feldspar), salmon/pink Plagioclase (sodium and calcium feldspar), white to gray with striations |
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• Light gray brown in color • Common member of the mica family • Excellent cleavage in one direction • Produces the “glimmering” often seen in beach sand |
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Biotite Amphibole group Pyroxene group Olivine group |
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• Black in color • Common member of the mica family • Excellent cleavage in one direction • Produces the “glimmering” often seen in beach sand |
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• Double chain structures • Dark gray brown to black • Two perfect • Hornblende is the most common mineral in the amphibole group |
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• Single chain structures involving iron and magnesium • Dark gray brown to black • Two distinctive cleavages at nearly 90 degrees • Augite is the most common mineral in the pyroxene group |
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Definition
• High temperature Fe-Mg silicates • Green to dark green, small, rounded crystals • Individual tetrahedra (4 oxygen with 1 silica) linked together by iron and magnesium ions • Very strong uniform bonds, concoidal fracture with no cleavage |
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Definition
Typically divided into classes based on anions. Only a small part (about 8%) of Earth’s crust • Oxides • Sulfides • Sulfates • Natives • Halides • Carbonates |
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Definition
• A rock or mineral that has solidified from molten material • Slower cooling times generally have larger crystals • The order of crystallization is determined by Bowen’s reaction series-more later |
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Definitions of igneous rocks |
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Definition
Magma Intrusive or plutonic rocks Lava, extrusive or volcanic rocks |
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Definition
• Composed of melt (liquid portion), crystals, and volatiles. • Volatiles: dissolved gases including water vapor, carbon dioxide, and sulfur dioxide |
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Intrusive or platonic rocks |
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Definition
• When emplaced at depth magma forms intrusive, or plutonic rocks and has larger crystals. Ex: Plutonic (intrusive): Sierra Nevada (granites) |
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Lava, extrusive, or volcanic rocks |
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Definition
• When magma comes to surface it is called lava and forms extrusive, or volcanic rocks and has finer crystals Ex: Volcanic (extrusive): Hawaii (basalt) and Cascades (andesite) |
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Definition
• Cooling rate (how fast) dominant factor but also amount of silica and dissolved gas • Slow rate = fewer but larger crystals • Fast rate = many small crystals • Very fast rate forms glass |
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Types of igneous textures |
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Definition
1. Aphanitic (a-not phaner-visible) 2. Phaneritic 3. Porphyritic 4. Glassy 5. Pyroclastic 6. Pegmatites |
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Definition
• Rapidly cooled magmas • Common with extrusive igneous rocks • Very fine grained, Crystals not visible w naked eye, • May contain vesicles (holes from gas bubbles) |
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Definition
• Solidified slowly at depth • Common with intrusive igneous rocks • Medium to large visible grains • Crystals visible w naked eye |
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Definition
• Fine matrix (groundmass) with large embedded visible crystals. • Initially, slowly cooled and forms large visible crystals. • Then flash cooled maybe extruded to surface and forms fine matrix |
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Definition
• Ejected from violent volcanic eruptions as fine ash, molten chunks, or large angular blocks. • Tuff: welded volcanic glass • Often look like a sedimentary rock |
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Definition
• Very large (and sometimes rare) crystals • Form in late stage crystallization of granitic magmas • High fluid content • Slowly cooled |
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Igneous compositions and names |
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Definition
• Felsic (light color) • Intermediate • Mafic (dark color) • Ultramafic |
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Definition
Granite (intrusive) Rhyolite (extrusive) • Light-colored, High silica • Mostly composed of Quartz, Potassium Feldspar (K-spar) and Plagioclase Feldspar |
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Definition
• Phaneritic • Major constituent of continental crust • Very abundant: often associated with mountain building • The term granite includes a wide range of mineral compositions |
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What is an an example of granite? |
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Definition
Sierra Nevada and Southern California Batholiths |
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Definition
• Aphanitic, commonly pinkish • These form thick lavas and are very explosive • Rhyolite is less common and less voluminous than granite |
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Definition
Diorite (intrusive) Andesite (Extrusive) • Mostly composed of Plagioclase Feldspar and some Amphibole • These rocks are medium gray (intermediate!) in color |
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Definition
• Phaneritic, coarse grained • Looks like gray granite |
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Definition
• Aphanitic texture, intermediate in color • Named after Andes Mountains • Commonly produced from subduction zones • Thick explosive lavas |
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Definition
• Dark in color • Composed of Plagioclase Feldspar, Pyroxene, and Olivine • Termed mafic (magnesium and iron-Fe) in composition • Higher density than granitic rocks • Significant % of oceanic crust |
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Term
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Definition
Basalt (Extrusive) Gabbro (Intrusive) |
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Definition
• Aphanitic texture • Fluid, hot lava • Comprise the ocean floor and many volcanic islands • Most common extrusive igneous rock |
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Definition
• Phaneritic • Not very common on surface b/c the magma is very fluid and hot (easy to come to surface) • Intrusive equivalent of basalt |
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Definition
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Definition
When confining pressures drop, decompression melting can occur |
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Definition
• As you increase volatiles (like water) you decrease melting temperature • Important factor where oceanic lithosphere (mixed with water rich sediment) descends into the mantle |
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Definition
• One magma may produce rocks of very different compositions • Minerals crystallize in a systematic fashion based on their melting points • During crystallization, the composition of the liquid portion of the magma (melt) continually changes |
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Term
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Definition
• Ultra-mafic has highest melting temp and felsic the lowest • Ultra-mafic minerals form 1st and the felsic minerals form last. • Discontinuous and continuous reaction series |
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Term
Changing a magma's composition |
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Definition
1 Magmatic differentiation 2 Assimilation 3 Magma mixing 4 Partial melting and magma formation |
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Term
Factors which affect volcanic eruptions |
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Definition
Silica, temperature, and volatiles all effect lava viscosity. |
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Definition
Measures a materials resistance to flow |
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Definition
• Increase silica • Increase volatiles (water vapor, and gas) • Decrease temperature |
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Term
Intermediate/Felsic Lava (Andesite/Rhyolite) |
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Definition
High viscosity: explosive • High silica, high volatiles, low temperature |
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Definition
Lower viscosity: mild eruptions • Lower silica, low volatiles, higher temperature |
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Extruded materials from volcanoes |
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Definition
Lava Gases Pyroclastic Materials |
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Term
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Definition
• Pahoehoe-smooth flows, resembles a twisted or ropey texture • Aa-broken up rocky, rough, jagged blocky texture • Pillow Lavas: basalts flowing into sea |
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Term
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Definition
• Most lava ranges from 1 to 6 % gas • Mostly water vapor, carbon dioxide, and sulfur dioxide, • Gases expand within a magma as it nears the earth’s surface due to decreasing pressure • The violence of an eruption is partially related to how easily gases escape from magma • Natural source of air pollution |
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Definition
• Material thrown out of a volcano • High volatiles, high silica, and low temp lava the more explosive and the more pyroclastic potential |
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Term
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Definition
• Scoria-vesicular basaltic black to reddish • Pumice- lighter in color porous rock from “frothy” lava |
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Definition
Conduit (pipe) Vent Crater Caldera Shield Parasitic Cone |
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Definition
Shield Composite (stratovolcano) Cinder cones |
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Term
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Definition
Gigantic in size • Mafic in composition: mostly Basalt • Very fluid lavas: hot, low silica • Broad domed structures resemble a warriors shield • Mostly under oceanic but some under continental crust • Calderas can form at top crest of the volcano from roof collapse |
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Example of shield volcano |
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Definition
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Term
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Definition
Medium in size • Form from near subduction zones • Intermediate, andesitic in composition • Explosive, viscous lavas: high silica, low temp • Large, classic shaped, nearly symmetrical volcano • Composed of interbedded lava flows and lots of pyroclastic material |
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Example of composite volcanoes |
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Definition
Cascade Range Vesuvius Atlantis |
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Term
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Definition
Very small • Forms scoria, a dark red-brown vesicular fragment • Product of gas rich, basaltic magma • Small 300-700 meters in height, steep slope angle • Frequently occur in groups, normally one time eruptions |
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Definition
• Volcanic mudflow from melting snow and ice • Mixture of volcanic debris and water |
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Definition
Fissure eruptions and lava plateaus Lava domes Volcanic pipes and necks |
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Definition
Batholith Plutons Dike Sill Laccolith |
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Definition
• Largest intrusive body • Surface exposure > 100+ km2 • Frequently form the cores of mountains |
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Definition
Sierra Nevada and Southern California Batholith |
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Definition
• Cooled, solidified magma emplaced at depth • Uplifted and material on top eroded off • Tabular (sheetlike) or massive • Concordant or discordant |
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Definition
• An intrusive tabular, discordant body |
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Definition
• An intrusive, tabular, concordant body |
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Definition
• Similar to a sill • Lens or mushroom-shaped mass • Arches overlying strata upward |
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Term
Plate tectonics and igneous activity |
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Definition
• Global distribution of igneous activity is not random • Most volcanoes are located within or near ocean basins |
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Term
Igneous activity at plate margins |
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Definition
Spreading centers Subduction zones |
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Term
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Definition
• Greatest volume of volcanic rock is produced along the oceanic ridge system • Decompressional melting of the mantle occurs as the lithosphere is pulled apart • Large quantities of basaltic magma are produced |
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Definition
• Occur in conjunction with deep oceanic trenches • Partially melting of descending plate and upper mantle • Region around the margin of Pacific Ocean is known as the “Ring of Fire” • Majority of world’s explosive volcanoes |
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Definition
• Associated with mantle plumes called hotspots • Localized volcanic regions in the overriding plate • Produces basaltic magma sources in oceanic crust • Produces felsic/intermediate magma sources in continental crust |
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Definition
• Explosive eruptions emit huge quantities of gases and fine-grained debris • A portion of the incoming solar radiation can be reflected and filtered out |
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Examples of volcanism affecting climate |
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Definition
Mount Tambora, Indonesia – 1815 Krakatau, Indonesia – 1883 Mount Pinatubo, Phillippines - 1991 |
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Definition
• Decomposition and disintegration of rocks and minerals at the earth's surface. • Results in the formation of sediment and sedimentary rocks |
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Definition
Physical (mechanical) Chemical |
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Definition
The mechanical disintegration of rocks and minerals into smaller pieces. |
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Types of mechanical weathering |
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Definition
• Frost wedging: freeze thaw cycle, water expands when it freezes and cracks rocks • Unloading: From less pressure as igneous rock is uplifted, creates onion-skin like exfoliation domes. • Thermal expansion: Repetitive heating and cooling, now thought to be a minor effect. • Biologic activity: Plant roots, burrowing organisms and human activity |
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Definition
• The decomposition of rock by the chemical breakdown of minerals. • Results in a change in rock composition |
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Types of chemical weathering |
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Definition
• Dissolution: Some components of rocks can be soluble and essentially dissolve. • Hydrolysis: Reaction of a substance with water. Feldspar changes to kaolinite clay • Oxidation: Loss of oxygen molecules to oxygen, rusting. |
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Term
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Definition
• Essentially minerals weather in the same sequence as they crystallize (Bowens) • Rocks that contain abundant fractures are typically weathered more rapidly than equivalent un-fractured rocks. • The more extreme the climate the more weathering will occur. • Rocks composed of minerals that are relatively unaffected by chemical weathering are generally the most resistant to weathering. Ex: Quartz on beach in San Diego County. |
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Definition
• Sedimentary rocks are the most abundant rock type exposed at the surface of the earth • Provide information about sediment transport and past environments • Often contain fossils |
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Sedimentary rocks are important for economic reasons because they may contain |
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Definition
• Coal • Petroleum and natural gas • Sources of iron, aluminum, and manganese |
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Definition
• Solid material that has settled from a state of suspension in a fluid. ie: water, air, or ice. Many changes occur to sediment after it has been deposited. |
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Definition
• Sediment turned into sedimentary rock • Compaction from weight of overlying rock • Cementation from precipitation of minerals between sediment grains: calcite, silica, and iron oxide |
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Definition
Detrital: transported sediment as solid particles Chemical/Biochemical: sediment that was once in solution or produced from organisms |
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Definition
• Small pieces of broken rock transported by wind, rivers, glaciers, erosion, turbidity currents etc.) • Mostly composed of quartz, very resistant to weathering • Particle size distinguishes between detrital rocks |
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Term
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Definition
• Fine grained sediment (generally formed in low energy environments. • From clay (finest), and silts • Fluids do not penetrate shales very easily and can “trap” petroleum and water within reservoirs. • Can be massive or fissile (layered) |
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Definition
• Mostly quartz grains. • Think of beach-sized material (really 1/16 to 2 mm) • Generally in high energy environments with rapid deposition things like beaches, deltas, turbidites, sand dunes etc. • Described as rounded to angular-depends on distance it was transported. • Described as well-sorted (same grain sizes) to poorly sorted (mixture of grain sizes)-tells us about the depositing currents. |
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Term
Conglomorate and breccias |
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Definition
• Both are gravel sized material. • Conglomerate has rounded clasts: like in a stream • Breccia: composed mainly of large angular particles • Matrix usually of sand or mud/clay sized material. |
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Definition
Shale Sandstone Conglomorate and breccias |
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Chemical/Biochemical sedimentary rocks |
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Definition
Limestones Cherts Evaporites Coal |
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Definition
Called carbonates • Most abundant chemical/biochemical rock • Usually a mixture of inorganic (precipitated) and biochemical sediments (shell fragments). |
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Biochemical limestones (coral reefs) |
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Definition
• Must have clear, warm shallow water • Grow rapidly in high-energy environment • Contain the world's largest petroleum reserves |
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Definition
• Not as common • Travertine is deposited in caves • Oolites: little balls that precipitate out in warm, shallow water |
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Definition
A coarse mixture of cemented shell fragments |
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Definition
• Chalk is a soft porous rock composed of fine-grained organisms with very small shells |
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Definition
• Composed of microcrystalline (very fine) quartz • Usually interbedded with Limestone • Very, very hard and difficult to drill through. |
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Definition
• Precipitated from seawater or freshwater • Sea Salt • Manganese nodules: most in Pacific, grow very slowly |
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Definition
• Composed of plant fragments in oxygen deficient environment • Peat, then Lignite (soft, brown coal) and finally Bituminous Coal (hard, black), becomes anthracite if metamorphosed |
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Sedimentary structure (definition) |
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Definition
• Sedimentary structures form in the basin of deposition from the action of natural processes. • Can indicate climatic, environmental, and current conditions |
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Term
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Definition
Cross-bedding Graded beds Ripple marks Mud cracks |
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Definition
• Individual beds are inclined to the horizontal • Can indicate current direction • Form with sand dunes, streams, deltas etc. |
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Definition
• Where energy is lost rapidly • Fining up sequences, largest particles first • Common in turbidites, and streams |
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Definition
Form where a current (wind or water) flows across a sediment surface |
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Definition
Current (asymmetrical) ripples; current direction at right angle to ripples, rivers etc. Oscillation (symmetrical) ripples; back and forth current movement, surf zone, lakeshore etc |
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Definition
• sediment is exposed to dry climate, it shrinks and mud cracks form • common in tidal flats, shallow lakes, and desert basins |
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Definition
Terrestrial environments (continents) Marine and transitional environments |
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Definition
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Marine and transitional enviorments |
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Definition
Deltas Beaches Turbidites Planktonic Oozes |
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Definition
• Fossils, rock types and internal structures provides evidence for climate and environment of an individual rock unit or sequence • A single bed can tell the history at one point in time. • A sequence of beds can tell the developmental history of the area/basin Ex: West African Rift Basin |
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Metamorphic rocks (definition) |
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Definition
• Rocks that have been altered or changed (but not melted) from heat and pressure. • Mineral assemblage change as you increase temps and pressures • Rocks become ductile at depth and can tend to “flow” • Parent material determines the final metamorphic composition. |
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Types of metamporphic rocks |
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Definition
1) Foliated metamorphic rocks: 2) Non-foliated metamorphic rocks |
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Foliated metamorphic rocks (definition) |
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Definition
Layered appearance, flat arrangement of mineral grains from compressional force. |
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Definition
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Term
Non-foliated metamorphic rocks (definition) |
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Definition
• Typically have only one mineral • Massive, no visible layers |
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Example of non-foliated rocks |
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Definition
Marble: from limestone or dolostone Quartzite: from sandstones |
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Term
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Definition
Low temp and pressure. • Fine grained rock, dull resembles shale. • Comprised of small mica and chlorite grains too fine to be seen with naked eye. • Phyllites: between slate and schist |
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Definition
more extreme temp and pressure. • Mica and chlorite grains start to grow from slate. • Platy structure can be seen with the naked eye. |
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Term
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Definition
• High-grade metamorphism. • Looks like a banded igneous rock. • Banding occurs when minerals become oriented due to intense temperature and pressure |
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Term
Common types of metamorphism |
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Definition
Contact Hydrothermal Regional Impact |
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Term
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Definition
High temp, low pressure • Igneous body contacts country (existing) rock. • Rocks are usually not foliated, b/c of low pressure. |
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Term
Hydrothermal metamorphism |
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Definition
• Heated fluids containing ions move through rocks and initiate a chemical change in the rock’s minerals • Can occur on continents near volcanic and igneous activity |
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Term
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Definition
• Produces the greatest amount of metamorphic rock. • Mostly from mountain building process at convergent plate boundaries • Migmatites: between igneous and metamorphic rocks. |
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Definition
• From meteorites (parts of comets or asteroids) |
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