Project – Interactive Rock Cycle
... Conglomerate – made of pebbles, stones, smaller particles pressed together by waves or water; usually found in large expanses or beds ...
... Conglomerate – made of pebbles, stones, smaller particles pressed together by waves or water; usually found in large expanses or beds ...
Rock Cycle Who Wants to be a Millionaire PowerPoint
... The igneous rock that forms when lava cools and crystallizes on the Earth’s surface is known as what type of rock? A – Extrusive Rock ...
... The igneous rock that forms when lava cools and crystallizes on the Earth’s surface is known as what type of rock? A – Extrusive Rock ...
Rock Type Puzzle
... These rocks are formed where This type transforms rocks into Shale, sandstone, and There are three types of these oceans, lakes or other bodies of new kinds using extreme heat limestone are examples of this on the earth. water once existed. and pressure. type of rock. These can begin as one type and ...
... These rocks are formed where This type transforms rocks into Shale, sandstone, and There are three types of these oceans, lakes or other bodies of new kinds using extreme heat limestone are examples of this on the earth. water once existed. and pressure. type of rock. These can begin as one type and ...
Which of the following attempts to explain the formation of the Solar
... 11. Explain why mafic igneous rocks weather faster than felsic igneous rocks. (2) Mafic minerals – high crystallization temps – therefore most unstable at surface temperatures and pressure They are the most “out of equilibrium” with surface conditions. 12. Describe the overall maturity you would exp ...
... 11. Explain why mafic igneous rocks weather faster than felsic igneous rocks. (2) Mafic minerals – high crystallization temps – therefore most unstable at surface temperatures and pressure They are the most “out of equilibrium” with surface conditions. 12. Describe the overall maturity you would exp ...
How are metamorphic rocks classified?
... Rocks may be flattened or bent or atoms may be exchanged to form new minerals. ...
... Rocks may be flattened or bent or atoms may be exchanged to form new minerals. ...
Rocks and the Rock Cycle
... type to another • Caused by forces within the Earth and at the surface ...
... type to another • Caused by forces within the Earth and at the surface ...
Non-Clastic Sedimentary Rocks
... too small to be seen without a microscope. Chalk is a type of limestone that is usually white. It consists almost entirely of the shells of tiny dead sea creatures. Limestone is a common building material. ...
... too small to be seen without a microscope. Chalk is a type of limestone that is usually white. It consists almost entirely of the shells of tiny dead sea creatures. Limestone is a common building material. ...
Rocks - mrsolomon
... Clastic Rocks - Formed from particles of other rocks which have accumulated and hardened. A mixture of other rocks. Weathering – process of breaking down larger rocks by wind, water and ice. These particles are transported to other locations where they join fragments from other rocks. These particle ...
... Clastic Rocks - Formed from particles of other rocks which have accumulated and hardened. A mixture of other rocks. Weathering – process of breaking down larger rocks by wind, water and ice. These particles are transported to other locations where they join fragments from other rocks. These particle ...
Geol100, Harbor Section, Review Session, 2012 p.
... Metamorphic (>diagenesis, < partial melting) type of metamorphism (regional, burial, contact, hydrothermal) pressure and temperature regimes grade of metamorphism, indicator minerals foliation and rock cleavage (slatey cleavage) effect of changing protolith (shale vs basalt vs carbonate vs ...
... Metamorphic (>diagenesis, < partial melting) type of metamorphism (regional, burial, contact, hydrothermal) pressure and temperature regimes grade of metamorphism, indicator minerals foliation and rock cleavage (slatey cleavage) effect of changing protolith (shale vs basalt vs carbonate vs ...
P1: Rock identification (I)
... number corresponds to the hardness of a particular mineral: 1, Talc; 2, Gypsum; 3, Calcite; 4, Fluorite; 5, Apatite; 6, Orthoclase; 7, Quartz; 8, Topaz; 9, Corundum; 10, Diamond. In the field, hardness can be estimated bearing in mind that a fingernail = 2.5, a copper coin = 3 and the blade of a poc ...
... number corresponds to the hardness of a particular mineral: 1, Talc; 2, Gypsum; 3, Calcite; 4, Fluorite; 5, Apatite; 6, Orthoclase; 7, Quartz; 8, Topaz; 9, Corundum; 10, Diamond. In the field, hardness can be estimated bearing in mind that a fingernail = 2.5, a copper coin = 3 and the blade of a poc ...
Oceanography Worksheet #1
... 3 density differences of ocean water 4 gravitational attraction of the Moon ...
... 3 density differences of ocean water 4 gravitational attraction of the Moon ...
Massachusetts - Swampscott Middle School
... Diagram of something learned What must have been in Massachusetts at some point for these rocks to exist? ...
... Diagram of something learned What must have been in Massachusetts at some point for these rocks to exist? ...
Metamorphic minerals
... Parent rock Temperature and pressure conditions Parent rocks (protoliths) control the elements that are available to form minerals: • Pelitic (shales and siltstones, Al rich) • Mafic (basalts, greywackes, Mg and Fe rich) • Carbonate or calc-silicate (limestones, Ca and Mg rich) ...
... Parent rock Temperature and pressure conditions Parent rocks (protoliths) control the elements that are available to form minerals: • Pelitic (shales and siltstones, Al rich) • Mafic (basalts, greywackes, Mg and Fe rich) • Carbonate or calc-silicate (limestones, Ca and Mg rich) ...
Topic 11
... - Minerals are classified according to their physical properties; rocks are classified according to their origin (how and where they form) ...
... - Minerals are classified according to their physical properties; rocks are classified according to their origin (how and where they form) ...
igneous rocks - Cloudfront.net
... Has SMALL microscopic crystals Crystals do not have time to form (because cooling happens very quickly) so they’re very small ...
... Has SMALL microscopic crystals Crystals do not have time to form (because cooling happens very quickly) so they’re very small ...
Rocky The Rock Cycle
... I'm now an intrusive igneous rock and can be exposed at the Earth's surface through uplift. But what would have happened if I had moved up to the Earth's surface as molten rock? ...
... I'm now an intrusive igneous rock and can be exposed at the Earth's surface through uplift. But what would have happened if I had moved up to the Earth's surface as molten rock? ...
GEOS1901 SKOU
... • Weathering and erosion, transportation, deposition, compaction, cementation • Clastic rocks: warn, broken material deposited by streams, wind, glaciers, marine currents etc o Conglomerate (coarse), sandstone (well exposed), mudstone (fine; shale) • Chemically precipitated rocks: limestone, gypsum ...
... • Weathering and erosion, transportation, deposition, compaction, cementation • Clastic rocks: warn, broken material deposited by streams, wind, glaciers, marine currents etc o Conglomerate (coarse), sandstone (well exposed), mudstone (fine; shale) • Chemically precipitated rocks: limestone, gypsum ...
Earthquakes
... An earthquake is the shaking or trembling of the earth caused by the _Sudden_ movement of the earth’s crust. They usually occur where rocks that have been fractured suddenly _Shift___. ...
... An earthquake is the shaking or trembling of the earth caused by the _Sudden_ movement of the earth’s crust. They usually occur where rocks that have been fractured suddenly _Shift___. ...
UP7.LP2.TypesofRocksGN
... __________ Found 10 kilometers beneath the Earth’s surface __________ Name implies that the rock has been changed/transformed __________ Starts off as a liquid __________ Heat and pressure can turn the other two types into this __________ Bits and pieces of the other two types can be found in this D ...
... __________ Found 10 kilometers beneath the Earth’s surface __________ Name implies that the rock has been changed/transformed __________ Starts off as a liquid __________ Heat and pressure can turn the other two types into this __________ Bits and pieces of the other two types can be found in this D ...
Rock Formations: How Igneous, Sedimentary, and Metamorphic
... There are 3 basic types of rock: igneous, sedimentary, and metamorphic rocks. Igneous rock Igneous rock is formed by the cooling and solidification of magma or lava, which is the liquid state of rock. Magma can result from the melting of existing rocks in the Earth’s mantle or crust. This melting us ...
... There are 3 basic types of rock: igneous, sedimentary, and metamorphic rocks. Igneous rock Igneous rock is formed by the cooling and solidification of magma or lava, which is the liquid state of rock. Magma can result from the melting of existing rocks in the Earth’s mantle or crust. This melting us ...
Rocks
... Wind and water break down the earth Bits of earth settle in lakes and rivers Layers are formed and build up Pressure and time turn the layers to rock ...
... Wind and water break down the earth Bits of earth settle in lakes and rivers Layers are formed and build up Pressure and time turn the layers to rock ...
Earth History
... in widely separated areas could be identified and correlated by their distinctive fossil content • This led to the "principle of fossil succession“ • Fossils succeed one another in a definite and determinable order, and therefore any time period can be recognized by its fossil content ...
... in widely separated areas could be identified and correlated by their distinctive fossil content • This led to the "principle of fossil succession“ • Fossils succeed one another in a definite and determinable order, and therefore any time period can be recognized by its fossil content ...
Geologic History
... in widely separated areas could be identified and correlated by their distinctive fossil content • This led to the "principle of fossil succession“ • Fossils succeed one another in a definite and determinable order, and therefore any time period can be recognized by its fossil content ...
... in widely separated areas could be identified and correlated by their distinctive fossil content • This led to the "principle of fossil succession“ • Fossils succeed one another in a definite and determinable order, and therefore any time period can be recognized by its fossil content ...
Classification of Sedimentary Rocks
... recognize that professional sedimentary geologists require more precise terms. Prefixes can also be added to indicate the dominant mineralogy. For example, a quartz-rich sandstone is a quartzose sandstone, a feldspar-rich sandstone is an arkose, a mica-rich sandstone is a micaceous sandstone, and a ...
... recognize that professional sedimentary geologists require more precise terms. Prefixes can also be added to indicate the dominant mineralogy. For example, a quartz-rich sandstone is a quartzose sandstone, a feldspar-rich sandstone is an arkose, a mica-rich sandstone is a micaceous sandstone, and a ...
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.