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REGIONAL GEOLOGY
REGIONAL GEOLOGY

... Pediment and derived deposits consist of boulder-and cobble- • sized near the steep zones and of gravel, sand and silt into flat area. These materials cover vast areas at the landward edge of the coastal plains. Sand and gravel form the floors of all main wadis and their • tributaries. These deposit ...
Are You suprised ?
Are You suprised ?

... phenomenon is usually observed in minerals that contain foreign ions called activators. These activators absorb ultraviolet light and give off visible light rays. Some minerals fluoresce under short wave UV, some under long wave UV and others under either wavelength. The property is unpredictable, t ...
Distribution of velocities of longitudinal body waves (P waves) in an
Distribution of velocities of longitudinal body waves (P waves) in an

... Chemically and mineralogically gabbro is equivalent to basalt. It is only in grain size that it differs from it. Basalt is aphanitic, whereas gabbro is phaneritic. Basalt occurs as lava; gabbro occurs as plutonic rock. So we call gabbros the deepseated equialents of basat. The intermediate grain-siz ...
Chautauqua Hills: Rocks and Minerals
Chautauqua Hills: Rocks and Minerals

... sandstones of the Douglas Group. During the Pennsylvanian Period, about 286 million to 320 million years ago, rivers and streams flowed into the sea in this area. Sand and other sediments collected in the estuaries and at the mouths of the rivers in deltas. When the seas dried up, the sediments were ...
Wind direction
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... is moved along the bottom of a stream bed. ...
Rock Cycle Drama - Georgia Standards
Rock Cycle Drama - Georgia Standards

... Convergent plate movement: This type of movement causes the folding of rock and mountain building. Group #5 should rattle their desks. Students playing the rock will walk back up to join the crust (Group #1). Together with Group #1, the rock students will raise their arms up in the shape of a mounta ...
metamorphic rocks - Math/Science Nucleus
metamorphic rocks - Math/Science Nucleus

... are forming today, it is difficult to see. Increasing temperature and pressure occurs inside the crust of the Earth, which is impossible for humans to observe. Hold up a sedimentary or igneous rock. Ask the students to imagine what the rock would look like if it was squished. Accept any reasonable a ...
Ore Bin / Oregon Geology magazine / journal
Ore Bin / Oregon Geology magazine / journal

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Chapter 18: Granitoid Rocks
Chapter 18: Granitoid Rocks

... “Granitoids” (sensu lato): loosely applied to a wide range of felsic plutonic rocks Focus on non-continental arc intrusives ...
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Weathering and Erosion
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... sediment is carried by water, the smoother the sand grains get. No water is involved when wind transports sediment. The sand grains bang into each other, creating a frosted surface (a surface that is dull instead of shiny). Beach sand, river sand, and dune sand are all similar in at least one way—th ...
questions - hrsbstaff.ednet.ns.ca
questions - hrsbstaff.ednet.ns.ca

... Minerals, Elements and the Earth’s Crust Introduction Minerals are substances formed naturally in the Earth. They have a definite chemical composition and structure. There are over 3000 minerals known on Earth. Some are rare such as gold and diamond, while others are more ordinary, such as quartz. L ...
Geology - Geoschol
Geology - Geoschol

... that also occurs in North Mayo, Donegal and through into western Scotland. There are even older Precambrian rocks in a very few places exposed by massive faults. Many large areas, such as Connemara, are defined as terranes. These are sequences of rocks that were formed in one place and are now along ...
PHYSICAL GEOLOGY LECTURE NOTES, PAGE I. Introduction
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... Ions = charged atoms; atoms with too few or too many electrons; includes cations (positively charged atoms) and anions (with negative electrical charges) Ionic Bonding - cations and anions attract one another; Ex. = sodium and chloride join to form salt Covalent Bonding - sharing of electrons betwee ...
The Greenhouse Effect on Earth
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GEOLOGY OF THE BLACK ROCK DESERT By Cathy Busby
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... In Middle Paleozoic time, the oceanic/island arc approached and then got pushed up onto Nevada along THRUST FAULTS, causing the Antler Orogeny (~370 to 340 Ma). ...
Minerals of Uganda
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... 10. Responsibility of the Course Lecturer Constant and punctual teaching, guide students during practicals, accompany and explain issues during field demonstrations and outer fieldwork, accurate and prompt grading of assignments, practicals, field reports, tests and ...
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... > biotite > quartz, muscovite, K-feldspar.  Continuous series: Ca-rich plagioclase > Na-rich plagioclase where Ca+ ions are in the mineral lattice structure at high temps and Na+ ions at lower temps. Forces driving magma movement o Viscosity  Temperature (heat breaks bonds between molecules)  Sil ...
Processes of Change
Processes of Change

... • Ice wedging is a form of mechanical weathering in which water seeps into rock cracks and then freezes and expands. • Wind, water, and gravity cause mechanical weathering by abrasion. • Animals and plants cause mechanical weathering by turning the soil and breaking apart rocks. • Water, acids, and ...
Untitled - Vermont Fish and Wildlife
Untitled - Vermont Fish and Wildlife

... closer to neutral in reaction and have high concentrations of calcium and other plant nutrients. Figure 1 is a simplified map of Vermont’s bedrock geology, emphasizing the ecological significance of the different rock types. Note that rocks of very different ages, like the Ordovician limestones of t ...
Chapter 11 Tertiary Volcanic rocks
Chapter 11 Tertiary Volcanic rocks

... Group strata. Rather than a well-worked conglomerate, this basal unit is more likely a talus or an alluvial fan deposit. A similar-looking lithology occurs with steeply faulted contacts on the north side of Engineer Mountain, but at this locality it could be fault breccia. One of the best developed ...
Igneous Rocks and Intrusive Igneous Activity
Igneous Rocks and Intrusive Igneous Activity

... highlighting the composition of the rocks, the texture of the rock, and the location (depth) where the rocks formed. ...
Physical Geology Practice Final Exam – Spring 2011 Part A. The
Physical Geology Practice Final Exam – Spring 2011 Part A. The

... 98. What is the difference between the saturated and unsaturated zones of groundwater? A) The saturated zone has a higher porosity than the unsaturated zone. B) The saturated zone has a lower porosity than the unsaturated zone. C) The pore spaces in the saturated zone are full of water; the pore sp ...
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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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