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EQ AND INTERIOR online
EQ AND INTERIOR online

... If so, what is the likely tectonic setting? (that is, at what type of plate boundary did the earthquake occur?) 15. For each of the earthquakes, determine if the quake occurred along a plate boundary or in the middle of a plate (an intraplate earthquake). If the quake was along a plate boundary, nam ...
Volcano Teacher`s Guide - Northern Stars Planetarium
Volcano Teacher`s Guide - Northern Stars Planetarium

... Ash Fine particles blown from volcanoes by explosive gas expansions that pulverize the frothing lava and solid rock into a fine dust. Basalt The type of rock that comprises nearly all lava. Caldera What we call volcanic craters over two kilometers in diameter. Composite Volcano An explosive type of ...
The Vesuvius Science Lab Training Packet
The Vesuvius Science Lab Training Packet

Volcanoes by Marida Torosyan and Ani Tashyan
Volcanoes by Marida Torosyan and Ani Tashyan

...  One important volcanic belt is the Ring of Fire.  Plates are immense pieces of crust that cause volcanic eruptions.  Volcanoes are made on plate boundaries that also cause volcanic eruptions. ...
The Classification of Metamorphic Rocks
The Classification of Metamorphic Rocks

... Metamorphic rocks are one of the three types of rock classifications, the other two being igneous and sedimentary. Rocks are classified by the processes under which they were formed. The differences in formation account for variations in the appearance of the rocks and, with some practice, you can l ...
Chapter 17: Plate Tectonics
Chapter 17: Plate Tectonics

... maps of the seafloor. You’ll learn more about magnetism and how it supports the hypothesis of continental drift later in this section. ...
18 Which geologic event is inferred to have occurred most recently
18 Which geologic event is inferred to have occurred most recently

... (1) oldest bedrock is located in the Churchill formation (2) youngest bedrock is located in the Wyoming formation (3) younger bedrock has been added to the east and west coasts of the continent (4) age of bedrock increases from west to east across the continent Base your answer to question 8 on the ...
Science SOL Review
Science SOL Review

... Coal ...
plate tectonics
plate tectonics

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Plate Tectonics Graham Cracker Lab File
Plate Tectonics Graham Cracker Lab File

... 1. How does this relate to the real Earth? 2. Name a specific location on the Earth where this kind of boundary activity takes place. 3. What actually happens to crust material that is subducted (pushed below other crustal plates)? 4. What features are formed on the continent along this boundary? 5. ...
INTRUSIVE IGNEOUS ROCKS, PART 2
INTRUSIVE IGNEOUS ROCKS, PART 2

... tin, tungsten, uranium, zirconium, and the rare earth elements. The presence of some of these minerals may make the pegmatite an ore. Pegmatites commonly form at the margins of batholiths and represent the last, most hydrous portions of the magma to crystallize. Although generally of granitic compos ...
Name: Volcano and Earthquake Simulation Lab Instructions for
Name: Volcano and Earthquake Simulation Lab Instructions for

... 1. Why do you think earthquakes and volcanoes are rarer at locations away from plate boundaries? ...
I. Earth spheres A. Three major spheres 1. atmosphere, thin
I. Earth spheres A. Three major spheres 1. atmosphere, thin

... 1) brittle, solid, broken into plates 2) averages 100 km thick—from 5 to 250 km 3) includes all of crust, and upper part of mantle b. asthenosphere ...
4 Absolute Ages of Rocks
4 Absolute Ages of Rocks

... To be able to discuss Earth history, scientists needed some way to refer to the time periods in which events happened and organisms lived. With the information they collected from fossil evidence and using Steno’s principles, they created a listing of rock layers from oldest to youngest. Then they d ...
Theory of Plate Tectonics and Convection Currents
Theory of Plate Tectonics and Convection Currents

... is heated and rises again. If this sinking and rising motion continues, it is called a convection current a motion that transfers heat in a material. Convection currents in the mantle are much slower than those in boiling water. The rock creeps only a few centimeters a year. The diagram below shows ...
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It`s getting hot in here

... Large volcanic eruptions can reflect radiation from the Sun and drop average temperatures on Earth by around half a degree. There have been several examples of this over the last century(25). ...
Volcanoes
Volcanoes

... flows as lava from an opening in earth’s surface and builds up a volcanic cone. • These openings are called vents. • Volcanoes release molten rock, ash, and poisonous gases. All these products result from melting in the mantle or in the crust. ...
Heterogeneous sources for Pleistocene lavas of Marie Byrd Land
Heterogeneous sources for Pleistocene lavas of Marie Byrd Land

... component as ancient, subducted oceanic crust. The HIMU mantle source is primarily sampled by melting in the mantle plumes that feed ocean island volcanism. However, HIMU and similar mantle sources are also sampled in regions that are not affected by plume activity (e.g., Gaffney et al., 2007); magm ...
File - Vagabond Geology
File - Vagabond Geology

... Mantle convection cells define the crustal plates of the earth ...
Rocks and Their Origins
Rocks and Their Origins

... Classification- is the grouping of objects by certain characteristics. Scientist classify objects to make them easier to study. * Petrologist classify rocks based on how they form. • Igneous rock- rock formed by the crystallization of hot molten rocks or minerals. ...
Earth Communication
Earth Communication

... This packet is your weeklong guide for reviewing our unit on plate tectonics. You are to complete each section in its entirety the day it is given to you. You will complete one section each day. Each section will include three parts: vocabulary definitions, inquiry based questions based on your own ...
Volcanoes - City of Redwood City
Volcanoes - City of Redwood City

... A volcano is a vent through which molten rock escapes to the Earth’s surface. Unlike other mountains, which are pushed up from below, volcanoes are built by surface accumulation of their eruptive products—layers of lava, ashflows, and ash. When pressure from gases within the molten rock becomes too ...
Earth Communication
Earth Communication

... This packet is your weeklong guide for reviewing our unit on plate tectonics. You are to complete each section in its entirety the day it is given to you. You will complete one section each day. Each section will include three parts: vocabulary definitions, inquiry based questions based on your own ...
Volcano and Earthquake Simulation Lab
Volcano and Earthquake Simulation Lab

... 1. Why do you think earthquakes and volcanoes are rarer at locations away from plate boundaries? ...
Dismantling the Deep Earth:  Geochemical
Dismantling the Deep Earth: Geochemical

... Large dataset, so filter it to include only samples that best represent the high 3He/4He mantle: A.) Interested in the 87Sr/86Sr (and Nd, Pb) of only the high 3He/4He mantle, so examine only the lavas with the highest 3He/4He from hotspots that have high 3He/4He. B.) High 3He/4He lavas from some env ...
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Large igneous province



A large igneous province (LIP) is an extremely large accumulation of igneous rocks, including liquid rock (intrusive) or volcanic rock formations (extrusive), when hot magma extrudes from inside the Earth and flows out. The source of many or all LIPs is variously attributed to mantle plumes or to processes associated with plate tectonics. Types of LIPs can include large volcanic provinces (LVP), created through flood basalt and large plutonic provinces (LPP). Eleven distinct flood basalt episodes occurred in the past 250 million years, creating volcanic provinces, which coincided with mass extinctions in prehistoric times. Formation depends on a range of factors, such as continental configuration, latitude, volume, rate, duration of eruption, style and setting (continental vs. oceanic), the preexisting climate state, and the biota resilience to change.
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