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Naming Metamorphic Rocks
Naming Metamorphic Rocks

... form ≥75% of the rock and both of which are present as major constituents; the amphibole constitutes ≥50% of the total mafic constituents and is present in an amount of ≥30%. Other common minerals include quartz, clinopyroxene, garnet, epidote-group minerals, biotite, titanite and scapolite. Granuli ...
Rules for Prefixing Rock Names with Minerals
Rules for Prefixing Rock Names with Minerals

... form ≥75% of the rock and both of which are present as major constituents; the amphibole constitutes ≥50% of the total mafic constituents and is present in an amount of ≥30%. Other common minerals include quartz, clinopyroxene, garnet, epidote-group minerals, biotite, titanite and scapolite. Granuli ...
The geology and mineral potential of Kenya
The geology and mineral potential of Kenya

... Mozambique Belt The Mozambique belt is a structural unit within which a wide variety of metasedimentary and meta-igneous rocks are found showing a broad concordance of structural style and metamorphic history. In most of these rocks, the degree of deformation is intense and is of high metamorphic gr ...
Metamorphic Rocks
Metamorphic Rocks

... A gabbro (igneous) intrusion can be seen above (black-colored rock). The surrounding gray rock is limestone. A thin layer of marble (white-colored rock) can be found between the two types of rocks. The marble formed as a result of contact metamorphism. ...
Lecture 2 Summer 2011
Lecture 2 Summer 2011

... 10. Kimberlite pipes are a major source of A.gold B.silver C.copper D.diamonds E.all of the above are equally abundant in kimberlite pipes 11. Most rocks on the Earth’s surface are ? rocks. A.igneous B.metamorphic C.sedimentary 12. Mantle rocks are of ? composition. A.felsic B.intermediate C.mafic D ...
principles of geologic time
principles of geologic time

... • Difficulties in dating the geologic time scale • Not all rocks can be dated by radiometric methods – Grains comprising clastic sedimentary rocks are not the same age as the rock in which they formed (have been derived from preexisting rocks) – The age of a particular mineral may not necessarily re ...
Short Course in Basic Geology Gregory A. Miles This short course
Short Course in Basic Geology Gregory A. Miles This short course

... Coal -- A rock that is composed of concentrated and compressed fossil plants remains. It is typically black, but some is brown. Conglomerate -- Rock composed mainly of rounded (water-worn) rock fragments larger than 2 mm (roughly the size of a BB); fragments are usually composed of harder rocks such ...
Organic sedimentary rocks
Organic sedimentary rocks

... Sometimes evaporites are precipitated on broad coastal salt flats called sabkhas. This specimen is from Tunisia in North Africa, where locals dig them out of the salt flats to sell to tourists. This one cost just 50 pence in 1986! ...
La crosta terrestre: minerali e rocce
La crosta terrestre: minerali e rocce

... hot aqueous solutions, by sublimation from hot vapour, evaporation of aqueous solutions, biological activity, and by transformations in the solid state. Rocks A rock is, in the majority of cases, a natural aggregate of several minerals, sometimes even non-crystalline substances, usually in a very co ...
igneous rocks
igneous rocks

... • Forms near bodies of water or where bodies of water use to be • Sedimentary rocks are made up of sediments. ...
Rock Cycle Powerpoint with pictures
Rock Cycle Powerpoint with pictures

... WITHOUT MELTING Crystals form (again) ...
California is mostly made up of Mesozoic and Cenozoic materials
California is mostly made up of Mesozoic and Cenozoic materials

... vertebrate fossils such as sharks, sea lions, turtles, whales, and other large life forms. The Bone Bed covers 47 square miles and is only about a foot thick. This bed is the most fossil-rich Middle Miocene bone bed in the world, having yielded at least 141 species of fauna and flora. How did the bo ...
Intrusive Activity
Intrusive Activity

... Intrusive Activity A. Magma can force the overlying rock apart and enter the newly formed fissures. B. Magma can also cause blocks of rock to break off and sink into the magma, where the rocks may eventually melt. C. Magma can melt the rock into which it intrudes. ...
Chapter 2: Non-tectonic Structures
Chapter 2: Non-tectonic Structures

...  These rocks flow more readily than any other common rock type and can form folded structures under surface temperature and pressure  These structures that move upward and gravitationally intrude overlying sediments are called diapirs. ...
8H booklet - Oxfordscience
8H booklet - Oxfordscience

... Examples of Rocks Schist Rocks: Schist rocks are metamorphic. These rocks can be formed from basalt (igneous rock), shale (sedimentary rock) or slate (metamorphic rock). Gneiss Rocks: Gneiss rocks are metamorphic rocks. These rocks have been granite (igneous rock). Grains in the rock flattened thro ...
rocks and minerals web scavenger hunt
rocks and minerals web scavenger hunt

... Rocks and Minerals Reference Sheet - Locate information about different minerals. ...
Metamorphic Rock - mrnicholsscience
Metamorphic Rock - mrnicholsscience

... Conglomerates—base of mountains Shale—mouth of rivers Rock salt—dried up sea ...
File
File

... Contrast the two major categories of metamorphic rocks: foliated and non-foliated. ...
To discuss igneous rocks as a type of rock formation
To discuss igneous rocks as a type of rock formation

... 1. ___________________________________________________________________ 2. ___________________________________________________________________ 3. ___________________________________________________________________ 4. ___________________________________________________________________ 5. _____________ ...
Rocks and Minerals Interactive Student Notebook
Rocks and Minerals Interactive Student Notebook

... 1. Sedimentary rocks are made up of ______________________. 2. _______________________ occurs when the weight of layers presses particles together. 3. A ______________ _______________ is a bed of rock. 4. The _________________ rock layers are at the top of the Grand Canyon. 5. ______________________ ...
8-3.4b - S2TEM Centers SC
8-3.4b - S2TEM Centers SC

... Sample 7 - Granite - Light-colored intrusive igneous rock. It came from magma deep within the earth and cooled before it reached the surface. Place dot on or next to the volcano where "intrusive igneous rocks" are shown. Sample 8 - Gabbro - Dark-colored intrusive igneous rock. It has a higher iron c ...
“Minerals that do things…” How to Bend a Rock
“Minerals that do things…” How to Bend a Rock

... sheet. They’ll find that they can bend the thin sheet. A notched drill core can be flexed by squeezing its ends together between a finger and the thumb. Specimens to test: Mica – get as large of plates as possible. Notched drill core of a competent rock. Equipment needed: How to make a fletched drill co ...
Unit Plan Sketch Part 1: Topic Content and Objectives
Unit Plan Sketch Part 1: Topic Content and Objectives

... folded mountains, hot spots, volcanoes. Related actions—earthquakes (see PWV-IV.4 m.6), volcanic activity, seafloor spreading, mountain building, convection in mantle. Evidence of “continental drift”—physical fit of continents, fossil evidence, measurements of movement, rock layer sequences, glacial ...
1 Every Pebble Tells a Story – Additional Materials 1 L. Braile
1 Every Pebble Tells a Story – Additional Materials 1 L. Braile

... small scale layering is almost always present as well so that small samples (pebbles) display layers. e. Mineral sorting (mechanical and chemical weathering of the less resistant minerals and particles) during erosion and transport often results in sedimentary rocks that are primarily made up of one ...
0_primary_structures
0_primary_structures

... Unconformities Conformable contact: The boundary between adjacent beds or units does not represent substantial gap in time A succession of beds of nearly the same age that represent ...
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Sedimentary rock



Sedimentary rocks are types of rock that are formed by the deposition of material at the Earth's surface and within bodies of water. Sedimentation is the collective name for processes that cause mineral and/or organic particles (detritus) to settle and accumulate or minerals to precipitate from a solution. Particles that form a sedimentary rock by accumulating are called sediment. Before being deposited, sediment was formed by weathering and erosion in a source area, and then transported to the place of deposition by water, wind, ice, mass movement or glaciers which are called agents of denudation.The sedimentary rock cover of the continents of the Earth's crust is extensive, but the total contribution of sedimentary rocks is estimated to be only 8% of the total volume of the crust. Sedimentary rocks are only a thin veneer over a crust consisting mainly of igneous and metamorphic rocks. Sedimentary rocks are deposited in layers as strata, forming a structure called bedding. The study of sedimentary rocks and rock strata provides information about the subsurface that is useful for civil engineering, for example in the construction of roads, houses, tunnels, canals or other structures. Sedimentary rocks are also important sources of natural resources like coal, fossil fuels, drinking water or ores.The study of the sequence of sedimentary rock strata is the main source for scientific knowledge about the Earth's history, including palaeogeography, paleoclimatology and the history of life. The scientific discipline that studies the properties and origin of sedimentary rocks is called sedimentology. Sedimentology is part of both geology and physical geography and overlaps partly with other disciplines in the Earth sciences, such as pedology, geomorphology, geochemistry and structural geology.
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