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Are similar to sills in that they are concordant, but instead of being tabular, they havye a mushroom like geometry. Then tend to have a flat floor and are domed up.
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a cylindrical conduit kown as a volcanic pipe that connects its crater with an unerlying magma chamber.
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Consequently, much of the volcano is erdoded but the pipe remains as a remnant called a volcanic neck
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the largest of all plutons, must have at least 100km2 of surface area, and most are far larger.
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in contrast to a batholith it is similar but smaller.
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flows are essentially explosive 'avalance" of hot volcanic dust "Glowing avalance"
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A "crater" in the center of a composite volcano resulting from the collapse of the floor of the volcano
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A bulge in a volcano caused by intrusion of highly viscous magma
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pieces of rock shot into the air
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irregular blobs are masses; generally conform to a magam chamber, granite in comp
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If the intrusive feature cuts across the grain.
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IF the intrusive feature conforms the grain
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A disconcordant tabular body
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A concordant tabular body is concordant
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Areas of erosion, larger particle sizes, rounded grains, poor preservaion of fossil remains
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Areas of quiet deposition, low circulation maybe- anoxic conditions, Finer particle sizes, preservation of fossils is good.
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Rock materials pass directly into solution (EG Halite or Calcite) Carbonic acid is a big playa
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CHemical union of water with minerals. "Clays are hydrated silicates"
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Chemical combination with a oxygen and a mineral. Results in a totally different mineral.Eg. Hematite
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deposited in horizontal layers
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Ice, wind, water (turns big pieces to small) abrasion and frost wedging
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Dissolution- rocks are altered are dissolved by water.
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what system is the key to sedimentary rocks.
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| Fluvial (rivers), Alluvial Fans, Glaciers, Eolian |
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Name the continual systems.
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| Shorelines, deltas, beaches, barrier islands |
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What are transistional Depositonal systems
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| Compaction and Cementation; sediments compressed by its own weight; Material becomes cemented together, process is called... |
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Composed of grains or pieces of orginal rock material ( SIze of grains matter)
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Chemical or biochemical chemical composistion of the rock matters, usually a percipitate, evaporate, or shell material
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