Magma Metamorphic Sedimentary Sediment Igneous
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Sediment Diagenesis
Sediment Diagenesis http://eps.mcgill.ca/~courses/c542/ SSdiedimen t Diagenes is Diagenesis refers to the sum of all the processes that bring about changes (e.g ., composition and texture) in a sediment or sedimentary rock subsequent to deposition in water. The processes may be physical, chemical, and/or biological in nature and may occur at any time subsequent to the arrival of a particle at the sediment‐water interface. The range of physical and chemical conditions included in diagenesis is 0 to 200oC, 1 to 2000 bars and water salinities from fresh water to concentrated brines. In fact, the range of diagenetic environments is potentially large and diagenesis can occur in any depositional or post‐depositional setting in which a sediment or rock may be placed by sedimentary or tectonic processes. This includes deep burial processes but excldludes more extensive hig h temperature or pressure metamorphic processes. Early diagenesis refers to changes occurring during burial up to a few hundred meters where elevated temperatures are not encountered (< 140oC) and where uplift above sea level does not occur, so that pore spaces of the sediment are continually filled with water. EElarly Diagenesi s 1. Physical effects: compaction. 2. Biological/physical/chemical influence of burrowing organisms: bioturbation and bioirrigation. 3. Formation of new minerals and modification of pre‐existing minerals. 4. Complete or partial dissolution of minerals. 5. Post‐depositional mobilization and migration of elements. 6. BtilBacterial ddtidegradation of organic matter. Physical effects and compaction (resulting from burial and overburden in the sediment column, most significant in fine-grained sediments – shale) Porosity = φ = volume of pore water/volume of total sediment EElarly Diagenesi s 1. -
Mineral Mania
The Rock Factory A Pre-Visit Information Guide for Teachers Meets Next Generation Science Standards: 5-PS1-3; MS LS4-1,2; MS ESS1-4; MS-ESS2-1 How does our Earth create so many different types of rocks? Learn about the different processes that form and reform rocks as you identify many types of rocks, minerals and fossils. Students will learn to think like geologists as they move through interactive investigation stations packed with specimens from the Museum’s collections. OBJECTIVES The Rock Cycle: Students will examine the three types of rocks - igneous, metamorphic and sedimentary – and discover the processes that create them. Tracing the connections between shale and slate, limestone and marble, students will discover how the rock cycle changes the very ground beneath our feet! Characteristics of Rocks Students will learn how to observe and identify rocks through their unique characteristics, looking for telling clues such as layering, crystal size, fossils, magnetism, and more. Students will practice their observational skills as they describe the Museum’s unique rock and mineral specimens. Investigation Stations: Students will explore Museum geology specimens up close at investigation stations to answer such questions as: “Why do fossils form only in certain rocks?” “How do rocks form from volcanic eruptions?” “How can I recognize different types of rocks?”. ACTIVITIES Teachers are encouraged to conduct pre-visit and post-visit classroom discussions and activities with their classes to make the most of their experience. Encourage your students to start a classroom rock collection, and create an exhibit with the rocks organized by type – igneous, sedimentary and metamorphic. -
Geologic Boulder Map of Campus Has Been Created As an Educational Educational an As Created Been Has Campus of Map Boulder Geologic The
Adam Larsen, Kevin Ansdell and Tim Prokopiuk Tim and Ansdell Kevin Larsen, Adam What is Geology? Igneous Geo-walk ing of marine creatures when the limestone was deposited. It also contains by edited and Written Geology is the study of the Earth, from the highest mountains to the core of The root of “igneous” is from the Latin word ignis meaning fire. Outlined in red, numerous fossils including gastropods, brachiopods, receptaculita and rugose the planet, and has traditionally been divided into physical geology and his- this path takes you across campus looking at these ancient “fire” rocks, some coral. The best example of these are in the Geology Building where the stone torical geology. Physical geology concentrates on the materials that compose of which may have been formed at great depths in the Earth’s crust. Created was hand-picked for its fossil display. Campus of the Earth and the natural processes that take place within the earth to shape by the cooling of magma or lava, they can widely vary in both grain size and Granite is another common building stone used on campus. When compa- its surface. Historical geology focuses on Earth history from its fiery begin- mineral composition. This walk stops at examples showing this variety to help nies sell granite, they do not use the same classification system as geologists. nings to the present. Geology also explores the interactions between the you understand what the change in circumstances will do to the appearance Granite is sold in many different colours and mineral compositions that a Map Boulder Geologic lithosphere (the solid Earth), the atmosphere, the biosphere (plants, animals of the rock. -
Part 629 – Glossary of Landform and Geologic Terms
Title 430 – National Soil Survey Handbook Part 629 – Glossary of Landform and Geologic Terms Subpart A – General Information 629.0 Definition and Purpose This glossary provides the NCSS soil survey program, soil scientists, and natural resource specialists with landform, geologic, and related terms and their definitions to— (1) Improve soil landscape description with a standard, single source landform and geologic glossary. (2) Enhance geomorphic content and clarity of soil map unit descriptions by use of accurate, defined terms. (3) Establish consistent geomorphic term usage in soil science and the National Cooperative Soil Survey (NCSS). (4) Provide standard geomorphic definitions for databases and soil survey technical publications. (5) Train soil scientists and related professionals in soils as landscape and geomorphic entities. 629.1 Responsibilities This glossary serves as the official NCSS reference for landform, geologic, and related terms. The staff of the National Soil Survey Center, located in Lincoln, NE, is responsible for maintaining and updating this glossary. Soil Science Division staff and NCSS participants are encouraged to propose additions and changes to the glossary for use in pedon descriptions, soil map unit descriptions, and soil survey publications. The Glossary of Geology (GG, 2005) serves as a major source for many glossary terms. The American Geologic Institute (AGI) granted the USDA Natural Resources Conservation Service (formerly the Soil Conservation Service) permission (in letters dated September 11, 1985, and September 22, 1993) to use existing definitions. Sources of, and modifications to, original definitions are explained immediately below. 629.2 Definitions A. Reference Codes Sources from which definitions were taken, whole or in part, are identified by a code (e.g., GG) following each definition. -
Exploring Origins of Pitted/Vesicular Rocks in Perseverance Valley, Endeavour Crater
50th Lunar and Planetary Science Conference 2019 (LPI Contrib. No. 2132) 2327.pdf EXPLORING ORIGINS OF PITTED/VESICULAR ROCKS IN PERSEVERANCE VALLEY, ENDEAVOUR CRATER. A. W. Tait1*, C. Schröder1, W. H Farrand2, J. W. Ashley3, B. A. Cohen4, R. Gellert5, J. Rice6, L. C. Crumpler7, B. Jolliff8, 1Biological and Environmental Sciences, University of Stirling, Stirling, FK9 4LA, UK ([email protected]), 2Space Science Institute, Boulder, CO, USA, 3Jet Propulsion Laboratory, California In- stitute of Technology, Pasadena, CA, USA, 4NASA Goddard Space Flight Centre, Greenbelt, MD, USA, 5Department of Physics, University of Guelph, Ontario, Canada, 6Planetary Science Institute, Tucson, AZ, USA, 7NM Museum of Natural History & Science, Albuquerque, NM, USA, 8Washington University in St. Louis, MO, USA. Introduction: Since sol 4780, the NASA Mars Ex- ploration Rover (MER) Opportunity has been traversing down Perseverance Valley (PV), a linear, negative-re- lief feature trending perpendicular to the western flank of Endeavour crater. The goal of the current investiga- tion is to understand PVs geomorphology and chemical composition to determine its mode of formation and ap- proximate age. Formation hypotheses include debris or fluid flow, and wind sculpting, all while intersecting possible Noachian lithologies [1]. Rover observations confirms orbital data that there exists a dextral off-set, indicating a structural origin to the valleys formation [2]. This faulting may have allowed for fluids to interact with the rocks [3]. On sol ~5000 Opportunity started to investigate a train of dark pitted/vesicular rocks with an unusual morphology, texture, and composition enriched in Al and Si. Here we describe the rock facies, and ex- plore preliminary formation/alteration hypotheses. -
Sedimentary Test 2 Review Guide Making Sedimentary Rocks 1
Name: KEY Unit III: Section 3: Sedimentary Processes Earth & Environmental Systems Science Test 2 Review Guide Sedimentary Test 2 Review Guide Making Sedimentary Rocks 1. What vocabulary word describes turning sediment into solid rock? Lithification = compaction + cementation 2. List and describe the processes to form sediment and then a sedimentary rock in order? - Weathering – breaking down - Erosion – moving/transporting sediment - Deposition – putting sediment into place Sediment MADE! Lithification: Turning sediment into a solid rock -Compaction – generally through burial and reduces pore space -Cementation – gluing sediment together using a mineral water solution Sedimentary Rock MADE! 3. What acts as glue to form Clastic and Bioclastic textured sedimentary rocks? Water moves through soil and rocks and dissolves minerals along the way. The mineral water solution settles in the sediment, the water evaporates, and the minerals are left behind to bind sediment. Uniformitarianism and Stratigraphy 4. What geological principle states that the same processes that operate today also operated in the past? Uniformitarianism – James Hutton 5. List and describe the 3 laws of Stratigraphy: -Law of Horizontal Deposition – Sediment is deposited and lithified in flat layers -Law of Superposition – oldest layers are on the bottom and youngest is on the top -Law of Cross-cutting – anything that cuts across sedimentary layers (faults or igneous intrusions) are younger than the layers that they cut across 6. What is an unconformity? Any process that disturbs sedimentary layers 7. List and describe the 3 types of unconformities: -Angular – beds are tilted (by plate tectonics), weathered and eroded, and new beds are placed on top at a different angle -Nonconformity – Igneous beds eat through sedimentary beds from the bottom -Disconformity – Sedimentary beds are missing due to weathering and erosion generally drawn as a straight squiggly line. -
Scientist Guide the Crayon Rock Cycle
Scientist Guide The Crayon Rock Cycle Introduction Soil is one of Earth’s most important natural resources. It is the bridge between the living and non- living worlds and ultimately where most of our food originates. Soil is composed of organic materi- al (humus), water, air and minerals. Rocks are mixtures of minerals such as quartz, feldspar, mica and calcite. They are the source of all soil mineral material and the origin of all plant nutrients with the exception of nitrogen, hydrogen and carbon. As rock is chemically and physically weathered, eroded and precipitated, it is trans- formed into soil. The rock cycle shows how rocks change over time by a variety of physical and chemical processes (see Figure 1). Natural processes that are part of the rock cycle include weathering, erosion, lithifi- cation, metamorphism, melting and cooling. • Weathering involves both the chemical and physical IGNEOUS ROCK Weathering breakdown of rock at or near the Earth’s surface. and Erosion Cooling This results in accumulation of sediments – loose materials, such as rock and mineral fragments, or Sediment Magma pieces of animal and plant remains that have been transported. Lithification (Compaction and Cementation) Melting • Erosion is the process by which soil and rock are removed from the Earth’s surface by exogenic SEDIMENTARY METAMORPHIC processes, such as wind or water flow, and then ROCK ROCK transported and deposited in other locations. Metamorphism (Heat and/or Pressure) • Lithification is the transformation of sediment into rock. The main processes involved in lithification are: Figure 1. o Cementation – large sediments are held together by natural cements. -
Structure of the Earth
And the ROCK CYCLE Structure of the Earth Compositional (Chemical) Layers Crust: Low density High in silicon (Si) and oxygen (O) Moho: Density boundary between crust and mantle Mantle: Higher density High in Magnesium (Mg) and Iron (Fe) Core: High in Nickel (Ni) and Iron (Fe) Heat Flow in the Earth Heat sources: latent heat from the formation of the Earth Radioactive decay in the core and mantle Temperature in the core: 3000- 5000° C Cooling processes: Convection currents: in outer core and asthenosphere transport heat to the surface Plate tectonics releases heat through the crust (volcanoes) Convection cells in the mantle and core transport heat from the interior of earth to the surface and also return cooler material back into the earth. Mechanical (Physical) Layers of the Earth Lithosphere: Crust and upper, solid part of the mantle; “plates” in plate tectonics Asthenosphere: Partially molten part of mantle; location of convection current that drive plates Outer core: Liquid Inner core: Solid Greatest temperatures, solid due to intense pressure Comparing Compositional Layers to Mechanical Layers Moho What is a Rock? A group of minerals bound together Three major groups: 1) Igneous: Solidified Molten Magma 2) Sedimentary: formed by cementing of sediments. Sediments come from the erosion of other rocks. 3) Metamorphic: Heat and pressure change a rock into something new, without melting. Rock Types Igneous: Solidified molten magma 2 types of Igneous: 1) Extrusive (volcanic) = erupted lava Cools more quickly, so only small crystals form. 2) Intrusive (plutonic) = never erupted magma Cools more slowly within the earth, so larger crystals can form. -
Extrusive Igneous Rocks- a Rock Formed on the Earth’S Surface
Rocks What is a rock? • Rock- naturally formed, consolidated materials composed of one or more minerals. • There are 3 types of rocks: • Igneous • Sedimentary • Metamorphic Igneous Rocks What are Igneous Rocks? • Magma vs. Lava • Magma- molten rock below the Earth’s surface. • Lava- magma on the Earth’s surface. • Igneous Rock- rocks made from cooling magma or lava. • They can be intrusive or extrusive. Intrusive vs. Extrusive • Intrusive Igneous Rocks- a rock that forms below the Earth’s surface. • Normally made from magma • Extrusive Igneous Rocks- a rock formed on the Earth’s surface. • Normally made from lava. Extrusive rock The white rock is intrusive. Intrusive Igneous Rocks • We cannot see these rocks be formed. • They typically have large crystal minerals. • The rock itself can give you a lot of information about how it was formed. Extrusive Igneous Rocks • You can see them form: • Lava flow • Ash Flow • Lava that cools down very quickly so all you see is ask coming out • Pyroclastic Flow • Clouds flowing downhill like a huge avalanche. • Data from these rocks can be used to interpret ancient volcanic activity. Igneous Rock Textures • The crystal size of the rock is related to the speed of the rock cooling. • Fast gives you small crystals and slow cooling gives you large crystals. • Also the rocks can appear: • Glassy- look like a piece of glass. • From the magma/lava cooling too quickly. • Vesicular- has air bubbles in it. This is vesicular. • From air bubbles getting trapped in the magma/lava. • Fragmental- they look jagged and angular. This is glassy and fragmental. -
Lavas. Understanding Volcanism Provides a Background for Theories
lavas. Understanding volcanism provides a background for theories relating to mountain building, the development and evolution of continental and oceanic crt~st,and how the crust is deformed. Our observations of volcanic activity fit nicely into plate-tectonic theory as described in chapter 11. The May 18, 1980 eruption of Mount St. Helens (box 10.1) was a spectacular release of energy from the earth's interior. The plate-tectonic explanation is that North America, moving weritwa~d,is overriding a portion of the Pacific Ocean Aoor. Melting of previously solid rock takes place at depth, just above the subduction zone. (Thii was described briefly in chapter 1 and more thoroughly in chapter 11.) At least some of the magma (molten rock or liquid that is mostly silica) works its way upward to the earth's surface to erupt. Magma does not always reach the earth's surface before solidifying, but when it does it is called lava. At Mount St. Helens the lava solidified quickly as it was blasted explosively by gases into the air, producing rock frag- ments known as pyrodasw (from the Greekpyro, "fire," and clart, "broken"). Pyroclastic debris is also known as tcphra. Elsewhere in the world (notably Hawaii) lava extrudes out of Flgulr 10.1 fissures in the ground as lava flows. Pyrodastic debris and Volcanic eruptions in Hawaii, 1969. A lava fountain is supply11 rock formed by solidification of lava are collectively regarded the lava cascading over the cliff. as emwive rock, surface rock resulting from volcanic Photo by D A Swanson, US Geolog~calSurvey acrivity. -
Igneous Petrology
IGNEOUS PETROLOGY PRESENTED BY Dr.A.BALUKKARASU Associate Professor Centre for Remote Sensing Bharathidasan University Thiruchirappalli-620 023 India. mail id:[email protected] MTIGT0403: IGNEOUS & METAMORPHIC PETROLOGY 1. Forms and Structures of Igneous rocks - Intrusives and their relation to Geological Structures (Concordant and Discordant forms - Multiple Intrusions – Composite Intrusions) - Composition and Constitution of Magmas - Structure and Texture of Igneous Rocks- Formation of Igneous rocks: Crystallization of Unicomponent Magma -Phase Equilibria studies of Binary and Ternary Silicate system - Crystallisation of Basaltic magma. 12 Hrs. 2. Classification of Igneous rocks – Microtextures and Structures of Igneous rocks and their Petrogenetic Significance - Petrography of Igneous rocks – Tabular Classification - Petrography of Acid-Intermediate - Basic and Ultrabasic rocks - Diversity of Igneous rocks - Reaction Principle - Magmatic Crystallization – Assimilation – Petrographic province and various diagrams - Plate Tectonics and Magmatic Evolution – Fluid Inclusion studies of Igneous rocks. Evolution of Basalts -Petrogenesis of Granites, Pegmatities, Alkaline rocks, Monomineralic rocks, Charnockites and Ultramafics. 14 Hrs. 3. Definition of Metamorphism - Scope of Metamorphism – Controlling factors of Metamorphism - Kinds of Metamorphism and its Products - Classification and Nomenclature - Petrography of Metamorphic rocks (Schists – Gneisses – Granulites) - Metamorphic textures and Microstructures and their relation to Metamorphic -
SUBMERGENCE and EMERGENCE of Rock Layers with Respect to Sea Level
SUBMERGENCE AND EMERGENCE of Rock Layers With Respect to Sea Level The building up and wearing away of Earth's Crust. Follow the progression of illustrations to see the roles that submergence and emergence of rock layers play in both the addition of rock material to earth's surface as well as its removal. The Key: Be sure to look at the key before observing the Illustration 1: Sedimentary Rocks are typically layered series of illustrations. horizontally and the Law of Superposition dictates that, Notice that not only do symbols exist for sandstone, shale unless overturning of rock layers has occurred, the oldest and conglomerate, but also for the loose sediments that rock layers are towards the bottom of a rock column while will eventually lithify to become these rock types. the youngest layers are at the top. This illustration depicts layers of sedimentary shale, sandstone and limestone, exposed at earth's surface. Illustration 2: The rock layers have been submerged, Illustration 3: Over time the processes of compaction possibly due to crustal movement or to a rise in sea level. and cementation will lithify these loose sediments turning All rock layers are now underwater and there exists the them into sedimentary rocks. The newly lithified rock possibility for additional, loose sediments to be deposited layer will be on top of the original layers shown in on top of the preexisting layers. Illustration 1 and it will be the youngest layer by L. Immoor 2006 Geoteach.com 1 comparison. Notice the unconformity in this illustration. The unconformity is evidenced by the wavy, eroded top surface of a rock layer.