Metamorphic rocks
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Metamorphic rocks are rocks that have changed from their original form due to heat, pressure, and fluids. There are two main types of metamorphism - contact metamorphism which occurs in small local areas, and regional metamorphism which affects large areas. Metamorphic rocks form through heat from the mantle, pressure from overlying rock layers, and fluids which can change a rock's chemistry and minerals. Metamorphic rocks are classified as either foliated (layered) such as gneiss and slate, or nonfoliated (nonlayered) such as marble and quartzite.
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Metamorphic rock
Metamorphic rocks are rocks that have changed composition and structure due to heat and pressure. They can form from sedimentary, igneous, or other metamorphic rocks deep within the Earth's crust under the right conditions of heat and pressure over long periods of time. Metamorphic rocks may be foliated, with a banded or layered appearance due to the alignment of minerals, or non-foliated without clear banding.
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Metamorphism and metamorphic rocks ppt
This document discusses metamorphism and metamorphic rocks. Metamorphic rocks form from existing igneous, sedimentary, or other metamorphic rocks through heat, pressure, and chemically reactive fluids. Metamorphism progresses incrementally and involves the growth of new minerals and deformation of existing ones. Metamorphism occurs in various settings like contact, regional, and burial metamorphism. Factors like heat, pressure, and fluids drive changes in mineralogy and texture. Metamorphic grade is indicated by index minerals and results in foliated and non-foliated rock types.
Engineering Geology
This document provides an overview of engineering geology and its scope. It discusses how geology relates to civil engineering projects in areas like construction, water resource development, and town planning. Key points covered include:
- Engineering geology deals with applying geology principles to safe and economic design of civil engineering projects.
- Geological maps, hydrological maps, and topographical maps are important for planning projects.
- Geological characteristics like bedrock, mechanical properties, and seismic activity influence project design.
- Geological knowledge aids in quality control of construction materials and sensitive construction areas.
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This document outlines homework, classwork, and lab/quiz activities for students to complete related to four topics: relative age, absolute age, fossilization, and geologic time. For each topic, students can choose between vocabulary cards, reading sections from textbooks or workbooks, or completing diagrams and writing assignments. For classwork, activities include diagrams, paragraphs, foldables, and quizzes. For labs or quizzes, students can choose to create timelines, charts, essays or comparisons. The document provides assignment options for students at different skill levels for each of the four geology topics.
Geologic dating
Rocks and fossils can provide information about geological events and changing life forms in the past. The principles of original horizontality and superposition allow scientists to determine the relative order and age of rock layers, though not precise dates. Absolute dating methods like radiocarbon dating measure radioactive decay to determine the specific ages of rocks and fossils.
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This document discusses how to determine whether a word problem requires using the greatest common factor (GCF) or least common multiple (LCM) to solve. It provides examples of GCF and LCM problems and walks through the step-by-step solutions. It also includes a quiz with word problems where the reader must identify whether each problem could be solved using GCF or LCM. Key factors that indicate a problem requires GCF include splitting things into smaller equal groups, arranging items into rows, and figuring out how many people can be invited. Problems that require LCM involve events repeating over time, purchasing multiple items, or determining when two repeating events will occur simultaneously again.
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Rocks can have varying properties and are not always hard, solid, natural, or composed solely of minerals as initially thought. Rocks are classified based on their formation process, with the main types being igneous (formed from cooling magma), metamorphic (formed from existing rocks undergoing heat and pressure), and sedimentary (formed from compression of sediments over time). The document serves to dispel preconceptions about rocks and introduce how they are scientifically classified according to their formation.
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Earth science overview
This document provides an overview of the curriculum for an Earth and Space science class. The year will be divided into four parts - geology, oceanography, meteorology, and astronomy. Geology will cover topics like minerals, rocks, fossils and plate tectonics. Oceanography will explore the ocean environment including waves, currents, and marine life. Meteorology will study the atmosphere, weather patterns, and severe weather. Finally, astronomy will examine objects in our solar system and beyond, such as stars, galaxies, and nebulae.
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The document discusses the relationships between organisms in a food web. It defines producers as organisms that make their own food, mostly plants. Consumers must find their own food and include all animals. Decomposers like worms and fungi break down dead and decaying matter. Consumers are classified as herbivores that eat only plants, carnivores that eat only meat, and omnivores that eat both plants and meat. A food chain shows the transfer of energy from producers to consumers as one organism eats another. A food web depicts overlapping food chains and shows how all animals in a community obtain food. An energy pyramid illustrates the decreasing amount of energy at each trophic level in a food web.
Relationships in Ecosystems
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Quiz bowl review for interim ii accelerated
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