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The document contains information about different types of rocks presented across 12 cards. It discusses the classification of rocks by their textures, how they are formed from minerals and sediments, and key characteristics. Igneous rocks such as granite form from cooling magma and volcanism. Sedimentary rocks like limestone and sandstone form through compaction and cementation of sediments. Metamorphic rocks change form due to heat and pressure acting on existing rocks.
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Igneous rocks form from the cooling and solidification of magma or lava. There are two main types - extrusive rocks which cool at the surface and intrusive rocks which cool underground. Crystal size depends on the cooling rate, with rapid surface cooling producing microscopic crystals and slow underground cooling producing larger crystals. Texture and mineral composition further classify igneous rocks into categories like rhyolite, granite, gabbro and basalt. Pyroclastic rocks form from explosive eruptions and include tuffs, agglomerates and volcanic bombs.
Lecture # 02, 03 316 geology and earth quake engineering 5th
The document discusses different types of rocks:
1. Igneous rocks form from cooling magma and include intrusive granitic rocks, extrusive volcanic rocks like basalt, and hypabyssal rocks.
2. Sedimentary rocks form through the lithification of sediments and include clastic rocks like sandstone, chemical rocks like limestone, and organic rocks like coal.
3. Metamorphic rocks form from the alteration of existing rocks under heat, pressure, and fluids, changing their texture and minerals. Foliated rocks include schist and gneiss, while non-foliated rocks include marble and quartzite.
Introduction and classification of rocks
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This document provides an overview of minerals, rocks, and the rock cycle presented by a student from Suez University. It discusses the main topics of minerals, igneous rocks, sedimentary rocks, and metamorphic rocks. Specifically, it describes the composition and properties of minerals, how the three main rock types are formed through igneous, sedimentary, and metamorphic processes, and provides examples of common rock types for each category. The document aims to educate the reader on basic concepts in petrology and the classification of earth materials.
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Igneous rocks form from the cooling and solidification of magma or lava. There are two main types - extrusive rocks which cool at the surface and intrusive rocks which cool underground. Crystal size depends on the cooling rate, with rapid surface cooling producing microscopic crystals and slow underground cooling producing larger crystals. Texture and mineral composition further classify igneous rocks into categories like rhyolite, granite, gabbro and basalt. Pyroclastic rocks form from explosive eruptions and include tuffs, agglomerates and volcanic bombs.
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The document discusses different types of rocks:
1. Igneous rocks form from cooling magma and include intrusive granitic rocks, extrusive volcanic rocks like basalt, and hypabyssal rocks.
2. Sedimentary rocks form through the lithification of sediments and include clastic rocks like sandstone, chemical rocks like limestone, and organic rocks like coal.
3. Metamorphic rocks form from the alteration of existing rocks under heat, pressure, and fluids, changing their texture and minerals. Foliated rocks include schist and gneiss, while non-foliated rocks include marble and quartzite.
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Rocks form the basis of the Earth's surface and have been here longer than humans. There are three main types of rocks - sedimentary, metamorphic, and igneous - which are distinguished by their formation process. Sedimentary rocks form from compression of soil and sediments and may contain fossils. Metamorphic rocks form from changes to existing rocks through heat, pressure, and chemical activity. Igneous rocks form from cooling lava or magma, and their grain size depends on the cooling rate at their formation site.
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This document provides an overview of minerals, rocks, and the rock cycle presented by a student from Suez University. It discusses the main topics of minerals, igneous rocks, sedimentary rocks, and metamorphic rocks. Specifically, it describes the composition and properties of minerals, how the three main rock types are formed through igneous, sedimentary, and metamorphic processes, and provides examples of common rock types for each category. The document aims to educate the reader on basic concepts in petrology and the classification of earth materials.
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1. The document describes a sedimentary sandstone rock found in Sequoia Park. It is gray and black with tiny black crystal dots and grass growing in parts of it.
2. A metamorphic hornfels rock is described as dark gray to black, hard, and breaking into sharp angular pieces. It formed under heat and pressure near magma or intrusions.
3. A siltstone rock is pale colored with small holes and black dots. It was found near a small lake in Santa Cruz Boardwalk.
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The document describes the process of identifying different types of rocks found in California. It discusses going to geological maps and researching the local area to find igneous, metamorphic, and sedimentary rocks. Samples were collected from places like Yosemite National Park and analyzed using a scientific process to determine their classifications. Key details like appearance, texture, and location helped identify the rocks as granite, andesite, gneiss, phyllite, conglomerate, and siltstone.
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Rocks have different chemical and physical properties that make them useful in our everyday lives. We use rocks for construction, fuel, art, and other purposes. Rocks are classified into three main groups based on their method of formation: igneous, sedimentary, and metamorphic. Igneous rocks form from the cooling and hardening of molten material from within the Earth. Their texture, mineral composition, and other features provide clues to how quickly or slowly they cooled.
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This document discusses the density, resistivity, susceptibility, and physical properties of common rocks. It defines density as mass divided by volume and lists the densities of various rock types such as basalt, granite, and limestone. Resistivity is the ability of a material to resist electric current and is measured in ohm meters. Factors like pore fluid, fractures, and clay content affect a rock's resistivity. Susceptibility measures how a material is affected by a magnetic field. Temperature, time, and rock type influence a rock's susceptibility. Physical properties described include luster, texture, shape, color, streak, weight, crystal form, and hardness. Hardness is measured using Mohs scale from talc to
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This document discusses igneous rock textures. It explains that texture refers to the size, shape, and arrangement of mineral grains in a rock. Cooling rate controls igneous rock texture, with rapid cooling resulting in fine-grained textures and slow cooling producing coarse-grained rocks. Extrusive igneous rocks like lava have fine-grained textures due to rapid surface cooling, while intrusive plutonic rocks exhibit a variety of coarse-grained textures due to slower cooling underground. Examples of different igneous rock textures are described, including aphanitic, porphyritic, vesicular, glassy, phaneritic, and pegmatitic.
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Pumice rock is the lightest and only rock that can float on water due to cooling very fast underground, which left it very light with many holes. It has a rough texture and is used to rub off dead skin. Granite is one of the most common rocks on Earth's surface, used for countertops and buildings. It cooled slowly, resulting in similarly sized crystals as marble. Basalt is very hard and forms from lava; it cooled quickly but with small crystals. Obsidian forms from volcanic glass and was historically used for tools since it is very sharp when fractured. Scoria is a volcanic rock that cooled partially underwater, leaving it with holes like pumice.
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The document provides information about sedimentary rocks, including their formation, classification, characteristics, and types. It discusses how sedimentary rocks form through the compaction and cementation of sediments. It classifies sedimentary rocks based on the nature of sediments (mechanically, chemically, or organically formed) and transporting agents (aqueous, aeolian, glacial). It provides details on specific sedimentary rock types like sandstones, conglomerates, limestone, and their properties. The document also covers concepts like bedding, stratification, unconformities in sedimentary rocks.
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The document describes an amethyst rock and its journey through the rock cycle. The amethyst rock, named Violet, started as an igneous rock formed from lava bubbles, transformed into a metamorphic rock through heat and pressure, then became a sedimentary rock through weathering and deposition before being mined and polished.
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Igneous rocks form from the cooling and solidification of magma or lava. They can be intrusive or extrusive, depending on where the magma cools. Intrusive igneous rocks cool slowly underground, resulting in large mineral grains, while extrusive rocks cool rapidly at the surface, resulting in small mineral grains or a glassy texture. The mineral assemblage and texture of an igneous rock provides clues about its composition and conditions of formation. Bowen's reaction series describes the order in which minerals crystallize as magma cools.
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The document discusses igneous rocks, which form when magma cools and crystallizes. There are three main types - intrusive rocks that cool slowly underground and have large crystals, extrusive rocks that cool quickly above ground and have small crystals, and volcanic glass that cools instantly. The rate of cooling affects crystal size and rock texture. Igneous rocks contain minerals that crystallize in a specific order as the magma cools, and can be classified as mafic or felsic based on their mineral composition. Common igneous rocks include granite, basalt, and obsidian.
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Rocks found in India are classified into three broad categories, viz. igneous, sedimentary and metamorphic rocks.
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The three main types, or classes, of rock are sedimentary, metamorphic, and igneous and the differences among them have to do with how they are formed. Sedimentary rocks are formed from particles of sand, shells, pebbles, and other fragments of material.
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Rock Cycle PowerPoint
The document discusses the three main rock groups: igneous, sedimentary, and metamorphic. Igneous rocks form from cooling magma, either underground (intrusive) or above ground (extrusive). Sedimentary rocks form through the compaction and cementation of sediments. Metamorphic rocks are formed from existing rocks undergoing heat and pressure without melting. The rock cycle diagram shows how rocks continuously change between these three types through various geologic processes.
igneous rocks classification #6.pdf
Classification of igneous rocks on the basis of texture and composition including IUGS classification.
Geo chemistry of metamorphic rock in pakistan
This document provides an introduction to the geochemistry of metamorphic rocks. It discusses the two main types of metamorphism - contact metamorphism and regional metamorphism. Contact metamorphism occurs near igneous intrusions and forms non-foliated rocks like marble, quartzite, and hornfels. Regional metamorphism occurs at greater depths and forms foliated rocks like slate, phyllite, schist, gneiss, and amphibolite. Examples of different metamorphic rocks are provided.
Science reporting
There are three main types of rocks: igneous, sedimentary, and metamorphic. Igneous rocks form from cooling magma and their crystal size depends on cooling rate. Sedimentary rocks form from compression of particles and sediments into new rocks like sandstone and limestone. Metamorphic rocks form from existing rocks undergoing heat and pressure within the earth, changing their composition and forming rocks like gneiss, marble, and quartzite.
Intro To Natural Stone Design I - Quick Look
Natural stone forms through three main processes: sedimentary, metamorphic, and igneous. Sedimentary stone forms from compression of sediments, metamorphic forms from changes to existing rock by heat and pressure, and igneous forms from cooling magma. Common types include limestone, marble, sandstone, slate, quartzite, and granite. Each has distinct characteristics based on its mineral composition and formation process.
Building Materials And Construction
This document discusses igneous rocks, including their formation from cooling magma, textures determined by cooling rate, and compositions. Igneous rocks can be classified based on their mineral makeup, which indicates their magma source and tectonic setting. Texture provides information about the cooling history, with fine-grained aphanitic rocks indicating rapid cooling and coarse-grained phaneritic rocks showing slow cooling. Composition depends on silica content, with granitic rocks having over 25% quartz and basaltic rocks mainly composed of pyroxene and plagioclase feldspar.
Metamorphic rocks
Metamorphic rocks are formed from existing rock types that have been altered by heat, pressure, and chemical processes usually while buried deep underground. There are two basic types - foliated rocks that have a banded or layered appearance due to heat and pressure, and non-foliated rocks that do not have distinct layers. Some common metamorphic rocks include gneiss, slate, schist, quartzite, and marble.
Rocks for class 2011
This document defines rocks and describes the three main types of rocks: igneous, sedimentary, and metamorphic. It explains that rocks are divided based on how they were formed and can change between types through geological processes. The rock cycle diagram shows how rocks continuously change between igneous, sedimentary and metamorphic forms over millions of years through melting, cooling, burial and erosion.
Rocks
Rocks are constantly changing and being transformed through various geological processes. Weathering breaks down rocks into sediments which are then eroded and transported by water, wind or ice. The sediments may settle and become compacted into sedimentary rocks through cementation. Heat and pressure metamorphose sedimentary and igneous rocks into different types of metamorphic rocks. Extreme heat melts rocks into magma and their subsequent cooling forms new igneous rocks, completing the continuous rock cycle.
rocks and minerals.pdf
Rocks form the Earth's outer layer and are composed of minerals. There are three main types of rocks: igneous rocks which form from cooling magma, sedimentary rocks which form from compressed sediments, and metamorphic rocks which form from changes to existing igneous and sedimentary rocks. Igneous rocks such as granite are used in construction while sedimentary rocks such as limestone can be used as a building material. The mining industry extracts various rocks and minerals for use in construction and other applications but can also negatively impact the environment.
Geology
1) Gneiss is a common metamorphic rock formed from igneous or sedimentary rocks under high-grade regional metamorphism. It is medium- to coarse-foliated with little mica or other platy minerals.
2) Marble is a non-foliated metamorphic rock formed from limestone composed primarily of calcite. It is widely used as a building material.
3) Migmatite forms under extreme heat during metamorphism, where partial melting occurs in pre-existing rocks resulting in a mixture of newly crystallized and older resistant materials.
Ch 4-Igneous Rocks.ppt
This document discusses igneous rocks and magma. It describes how igneous rocks form from the cooling and solidification of magma. Magma is the molten rock located either at the surface as lava or at depth. Factors like cooling rate and composition determine the texture of the igneous rock. The document also examines the compositions of different igneous rocks and how magmas evolve during crystallization through processes like differentiation and assimilation.
Ch 4-Igneous Rocks (1).ppt
This document discusses igneous rocks and magma. It describes how igneous rocks form from the cooling and solidification of magma. Magma is the molten rock found underground or lava if at the surface. Factors like cooling rate affect the texture of the igneous rock. Composition depends on minerals present, with granitic rocks being felsic and basaltic rocks being mafic. Magma evolves as it cools via processes like differentiation, assimilation, and mixing.
II.A Minerals and Rocks
Core Subject: Earth and Life Science
II. Earth Materials and Processes
A. Minerals and Rocks
The learners
demonstrate an
understanding of:
1. the three main categories of rocks
2. the origin and environment of formation of common minerals and rocks
The learners:
1. identify common rock-forming minerals using their physical and chemical properties
2. classify rocks into igneous, sedimentary, and metamorphic
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This document outlines a rock unit rubric with different tiers of assignments about igneous, metamorphic, and sedimentary rocks. Tier 1 focuses on vocabulary and includes creating definition cards or completing charts. Tier 2 builds on this with activities like diagrams, articles, and puzzles. Tier 3 involves more extensive projects like a children's book or presentation using a digital tool to communicate information about rocks and the rock cycle. Assessments include a required lab on the rock cycle and a rocks test.
Rocks tiers 2011
This document outlines assignments for a unit on rocks and the rock cycle. It includes three tiers of optional assignments with increasing difficulty. Tier 1 focuses on vocabulary and includes creating vocabulary cards and completing charts. Tier 2 includes creating educational materials like a Venn diagram, crossword puzzle, or magazine article. Tier 3 involves more creative assignments like a children's book or using a digital tool to teach about rocks. Labs and quizzes/tests are also mentioned to assess learning throughout the unit.
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Two truths 1 lie
- 1. Card #1 Card #2 Card #3 • Igneous rocks may be • Coal is not a rock • A rock is classified by formed from lava or because it’s made of it’s texture magma plant life • Foliate rocks have • Granite is an example • Limestone is made banded layers of an extrusive igneous from shells rock • Gravel is a form of • Sandstone is a form of sediment • Volcanic activity on clastic sedimentary earth’s surface most rock likely results as extrusive igneous rocks Card #4 Card #5 Card #6 • Minerals have to be • A Mineral has a • Metamorphic rocks are inorganic definite mineral formed by the buildup structure of sand grains • To reduce the impact of mining people • Erosion breaks down • We classify should increase the use the sediment metamorphic rocks of minerals according to the • Sedimentary rocks can arrangement of the • Reclamation is the best be formed from grains in the rock way to reduce chemicals on the environmental effects bottoms of lake and • A rock formed from of mining oceans magma that cools is a form of an intrusive rock Card #7 Card #8 Card #9 • The most abundant • Rocks can be formed • Congolormerate is a intrusive rock is granite from other rocks metamorphic rock • When igneous rocks • Small crystals are from • Obsedian is an igneous cool rapidly they slow cooling rock create a fine grained texture • Metamorphic rock are • WEDCC helps formed by extreme remember the steps to • Deposition carries the heat and pressure lithification sediments Card #10 Card #11 Card #12
- 2. • Clastic rocks are • Batholith is a large • Rocks are formed from metamorophic rocks deposit of granite minerals • Contact • Great heat and • Minerals are mostly metamorphism covers pressure create metals a small area metamorphic rocks • To be a mineral, it • Mineral composition is • Compaction glues the must be inorganic a characteristic used to sediments together identify a rock