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How Do You Study the Past? (The Rock Record: Absolute
How Do You Study the Past? (The Rock Record: Absolute

... A. Unaltered Remains 1. Description: plant or animal remains that have not undergone change since death. a. Uncommon because frozen, extremely dry, or oxygenfree environments are required to form these fossils b. Examples: • Mummified humans • Frozen organisms (Ice Man) • Mammoths & cats in La Brea ...
Rocks
Rocks

... Sedimentary Rock (cont) • Clastic sedimentary rocks – Rock fragments are carried by wind, water and ice become compacted and cemented together = classified by size – Conglomerate = rounded, gravel-sized pebbles cemented by minerals – Breccia = gravel-sized fragments (angular with sharp edges) – San ...
3.4 How are the rock classes Rocks and Rock
3.4 How are the rock classes Rocks and Rock

... Clastic sed. rocks form from the fragments, and chemical sed rocks from the dissolved portion... Metamorphic rocks form by the reaction of preexisting rocks in the presence of heat, pressure, fluids, or combinations thereof, producing new minerals and rocks. ...
Igneous rock glossary
Igneous rock glossary

... magma. The water either comes from the surface (ocean water, groundwater derived from precipitation) or from the magma itself. intermediate composition of magma/lava Used to describe magma or igneous rock containing an intermediate (52–65%) proportion of silica (SiO2). intrusive igneous rock A rock ...
Igneous glossary- Word version
Igneous glossary- Word version

... magma. The water either comes from the surface (ocean water, groundwater derived from precipitation) or from the magma itself. intermediate composition of magma/lava Used to describe magma or igneous rock containing an intermediate (52–65%) proportion of silica (SiO2). intrusive igneous rock A rock ...
Chapter 8: Geologic Time
Chapter 8: Geologic Time

... Not divided into smaller time units because the events of Precambrian history are not known in great enough ...
Igneous Rocks Notes
Igneous Rocks Notes

... that magma formed. Lava repeatedly flowed over the surface and hardened, forming a rocky crust. That crust sank into Earth’s interior, allowing more lava to erupt over the surface and harden to form rock. ...
Course Specifications General Information
Course Specifications General Information

... This course introduces the basic knowledge about the origin , development, component, material, and structure of the solid Earth ...
07_Metamorphic-Rocks_Lab7_10thEd_FW2017
07_Metamorphic-Rocks_Lab7_10thEd_FW2017

... thermal conditions. This is also the most likely place to experience rapid pressure increase or directed stresses. While rocks also uplift, cool off and decompress; by this time fluids have been driven off and there is little permeability to bring new ones in. As a result regional metamorphic rocks ...
Types of Rocks
Types of Rocks

... • Metamorphic rocks are formed by: 1. Taking sedimentary or igneous under earth’s surface 2. Add extreme temperature (from below crust) 3. Add pressure from above and below 4. This same process over a period of time can create new rocks ...
Fossils - Mrs. Sandoval Science
Fossils - Mrs. Sandoval Science

... II. Molds and Casts  Molds are a hollow impression of a once living thing found in a rock.  Form when an organism is buried by sediments and the sediments change to rock.  The organism decays and leaves a cavity, or opening, in the rock.  The cavity is the mold.  Casts occur when a mold is fil ...
TAYSIDE – A LAND MOULDED FROM ROCK AND ICE
TAYSIDE – A LAND MOULDED FROM ROCK AND ICE

... The limestones are locally thick and extensive enough to give rise to rare limestone pavements around Schiehallion and Blair Atholl. The limestone areas weather to deep brown lime-rich soils which support species-rich calcareous grassland. The succeeding ‘Argyll Group’ rocks are also a mixture of m ...
igneous rocks - Faculty Perry, Oklahoma
igneous rocks - Faculty Perry, Oklahoma

... surface. Basalt, pumice and obsidian are common extrusive rocks. Intrusive igneous rocks are formed when magma cools and hardens below the Earth’s surface. Granite and gabbro are the most common intrusive rocks. The texture of igneous rocks depends on the size of their mineral crystals. Rapidly cool ...
Lecture 8
Lecture 8

... Fig. 8.16a ...
Geology Content from the Frameworks
Geology Content from the Frameworks

...  Igneous rocks are "fire-formed". They crystallized from hot, molten lava or magma as it cooled.  Igneous rocks are dominated by silicate minerals.  Igneous rock undergoes weathering (or breakdown) to form sediment. The sediment is transported and deposited somewhere (such as at the beach or in a ...
Minerals, basic component of rocks Minerals One Rock Common
Minerals, basic component of rocks Minerals One Rock Common

... • For freezing water to play an important role in weathering, it has to thaw as well • Freeze, thaw cycles accelerate weathering process ...
Coosa County
Coosa County

... Gneiss – a coarse-textured complex metamorphic rock. Gneiss is a type of rock with a great variety of large mineral grains arranged in wide bands which originally may have been of either igneous or sedimentary origin. Common and widely distributed, it makes up the largest part of the earth's lower ...
Packet #7
Packet #7

... 5.   Which type of climate has the greatest amount of  rock weathering caused by frost action? 1 a wet climate in which temperatures remain  below freezing 2 a wet climate in which temperatures alternate  from below freezing to above freezing 3 a dry climate in which temperatures remain  below freez ...
Geological Terms
Geological Terms

... Granite – a type of intrusive igneous rock that forms from the slow crystallization of magma below Earth’s surface. Granite is composed mainly of quartz and feldspar with minor amounts of micas, amphiboles and other minerals such as hornblende or augite. This mineral composition usually gives granit ...
Midterm 1, Winter 2012 with answers
Midterm 1, Winter 2012 with answers

... 5. The relatively young age (200 million years) of the oceanic crust and old age (up to 4 billion years) of the continental crust supports the notion that: *A. oceanic crust is continuously being recycled by the process of subduction and that continental crust is almost never subducted B. ocean basi ...
The History of Life: Study Guide
The History of Life: Study Guide

... 17. Animals use oxygen for respiration, and plants use carbon dioxide for photosynthesis. 20. The principle of “Uniformitarianism” is fundamental to an understanding of modern day Geology, it was introduced to the scientific community in the 18th century, 18. Bacteria, plants and fungi have been alt ...
Formation of Gems and Minerals
Formation of Gems and Minerals

... becomes concentrated in the molten rock because it does not get incorporated into most minerals that crystallize. Consequently, the last, uncrystallized fraction is rich water and other unusual elements that also do not like to go into ordinary minerals. – When this water-rich magma is expelled in t ...
Slide 1
Slide 1

... Mostly happens at Plate Boundaries. ...
here - Gloucestershire Geology Trust
here - Gloucestershire Geology Trust

... event some 390 – 310 million years ago. In places, the beds can be seen to thicken in the centre. It is thought that this is due to the rocks accommodating the huge forces acting on them. At this time, the main fault (Blaisdon Fault) seen at this site was also formed. It resulted in the Huntley Quar ...
File - Science with Mrs. Ramirez
File - Science with Mrs. Ramirez

... • Extrusive rocks form when the lava cools and crystallizes (hardens) on the surface of the Earth. Igneous rocks that are formed above ground are called volcanic. If magma makes it to the surface, it is known as lava and it will erupt or explode from a volcano and then cool and crystallize to form a ...
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Clastic rock



Clastic rocks are composed of fragments, or clasts, of pre-existing minerals and rock. A clast is a fragment of geological detritus, chunks and smaller grains of rock broken off other rocks by physical weathering. Geologists use the term clastic with reference to sedimentary rocks as well as to particles in sediment transport whether in suspension or as bed load, and in sediment deposits.
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