• Study Resource
  • Explore Categories
    • Arts & Humanities
    • Business
    • Engineering & Technology
    • Foreign Language
    • History
    • Math
    • Science
    • Social Science

    Top subcategories

    • Advanced Math
    • Algebra
    • Basic Math
    • Calculus
    • Geometry
    • Linear Algebra
    • Pre-Algebra
    • Pre-Calculus
    • Statistics And Probability
    • Trigonometry
    • other →

    Top subcategories

    • Astronomy
    • Astrophysics
    • Biology
    • Chemistry
    • Earth Science
    • Environmental Science
    • Health Science
    • Physics
    • other →

    Top subcategories

    • Anthropology
    • Law
    • Political Science
    • Psychology
    • Sociology
    • other →

    Top subcategories

    • Accounting
    • Economics
    • Finance
    • Management
    • other →

    Top subcategories

    • Aerospace Engineering
    • Bioengineering
    • Chemical Engineering
    • Civil Engineering
    • Computer Science
    • Electrical Engineering
    • Industrial Engineering
    • Mechanical Engineering
    • Web Design
    • other →

    Top subcategories

    • Architecture
    • Communications
    • English
    • Gender Studies
    • Music
    • Performing Arts
    • Philosophy
    • Religious Studies
    • Writing
    • other →

    Top subcategories

    • Ancient History
    • European History
    • US History
    • World History
    • other →

    Top subcategories

    • Croatian
    • Czech
    • Finnish
    • Greek
    • Hindi
    • Japanese
    • Korean
    • Persian
    • Swedish
    • Turkish
    • other →
 
Profile Documents Logout
Upload
Earthquake – violent shaking of the ground
Earthquake – violent shaking of the ground

... crust – solid outer shell of the Earth, lithosphere continental crust – granitic, less dense, thicker oceanic crust – basaltic, more dense, thinner Moho – interface between more dense and less dense mantle and crust mantle – layer below crust that plates move across, where convection occurs meteorit ...
California Geology - Porterville Unified School District
California Geology - Porterville Unified School District

... California Geology ...
Geology- Module 7
Geology- Module 7

... approximately 240 million years ago. • Alfred Wegner first created continental drift theory which stated that the continents drifted apart from this land mass into their present day location. He used plant/animal fossil evidence to help support his theory. • Eventually, Plate Tectonic theory was dev ...
Igneous Rocks
Igneous Rocks

... the Earth’s surface (lava), cools quickly with very small or no crystals formed • An igneous rock that forms within Earth’s crust is called an intrusive rock, magma pushes into surrounding rock below the Earth’s surface Which rocks are more likely to have large crystals? ...
Layers Directed Reading
Layers Directed Reading

... Why do scientists study the ocean floor to research the mantle? ...
Continental Drift, Mountain Building, and Plate Tectonics
Continental Drift, Mountain Building, and Plate Tectonics

... Magnetic minerals (mainly magnetite) is magnetized and aligned with earth’s mag. Field below the CURIE POINT. These fossil magnets reflect changes in the magnetic field through time. INCLINATION is the angle the magnetic makes with the earth’s surface = latitiude DECLINATION is the angle between the ...
Hot Spot Volcanism on Venus, Earth and Mars
Hot Spot Volcanism on Venus, Earth and Mars

... exhibit characteristics consistent with the general predictions of the interaction of a mantle plume with a planet’s surface, including a topographic swell, abundant volcanism, and a positive gravity anomaly. More recently, the hotspot or mantle plume origin for a number of features on Earth has com ...
Unit 2 Vocabulary – Plate Tectonics
Unit 2 Vocabulary – Plate Tectonics

... asthenosphere – the plastic-like, but solid, layer in the mantle which allows the lithosphere above to move continental drift hypothesis – the continents once formed a giant landmass (Pangaea), broke apart, and then drifted to their current locations mid-ocean ridge – a continuous mountain chain on ...
Plate tectonics
Plate tectonics

... Where continental crust meets continental crust Both continental crusts are too light to subduct so a continent-continent collision occurs, creating especially large mountain ranges. The most spectacular example of this is the Himalayas. ...
Types of Rock - Leon County Schools
Types of Rock - Leon County Schools

... beneath Earth’s surface and hardens. The most abundant intrusive rock on Earth’s continents is granite. Granite forms the core of many mountains ranges. ...
Igneous Rocks
Igneous Rocks

... beneath Earth’s surface and hardens. The most abundant intrusive rock on Earth’s continents is granite. Granite forms the core of many mountains ranges. ...
Continental Drift and Plate Tectonics
Continental Drift and Plate Tectonics

... called subduction. (example: Andes Mtns.)This molten material, which is under great pressure can escape through weak spots in the Earth’s crust. What can happen? Erupting volcanoes. 3. Ocean Plate to Ocean Plate: two plates come together and one slides under the other (subduction) When this happens ...
AMGEN SUMMER SCIENCE INSTITUTE 2003
AMGEN SUMMER SCIENCE INSTITUTE 2003

... Assessment of the topics • Assessment will be done following ways: – Quizzes – Tests – Group work Two sample quizzes and a puzzle activity is given on the following pages. ...
oceanic ridges
oceanic ridges

... To test this hypothesis, scientists determined the eruptive ages AND the polarity of young basalts using the newly developed technique of K-Ar radiometric ...
Chapter 10 Notes Blank
Chapter 10 Notes Blank

...  Less dense __________flows sideways dragging the seafloor along.  As the seafloor spread apart, magma flows up through __________ in at the ridge forming new rock. ...
Earth`s Interior (+ Magnetism section from Plate Tectonics Chapter
Earth`s Interior (+ Magnetism section from Plate Tectonics Chapter

... MAFIC – igneous rocks whose composition is low in Si and high in Fe, Mg, and Ca – usually found in oceanic volcanic settings like seafloor spreading centers and ocean hotspots. Example: Basalt. FELSIC – igneous rocks whose composition is high in Si and low in Fe, Mg, and Ca – usually found in contin ...
Plate Tectonics
Plate Tectonics

...  Continental drift is Wegener’s theory that all continents had once been joined together in a single landmass and have drifted apart since.  Wegener named this supercontinent Pangaea.  Wegener’s theory was rejected by scientists because he could not explain what force pushes or pulls continents. ...
Ocean-Continent Convergent Plate Boundaries Quiz
Ocean-Continent Convergent Plate Boundaries Quiz

... How is subduction important in the rock cycle? The oceanic crust brings rock back to the mantle when it collides and sinks under the continental crust and turn it back into magma. The magma may erupt through a volcano or cool beneath the surface turning the magma into igneous rock. ...
CHAPTER 3 TECTONICS Vatnajokull Glacier- Iceland
CHAPTER 3 TECTONICS Vatnajokull Glacier- Iceland

... The Earth is density stratified: each deeper layer is more dense than the layers above. Densities: Water = 1g/cc or a specific gravity of 1 Granite = 2.7 g/cc or 2.7 G Basalt = 3 g/cc or 3 G Drilling Records Land- Kola Peninsula-1992-12,063m (7.5 miles) (T there = 245 degrees C (or 473 degrees F) Pr ...
INTERNATIONAL INDIAN Sub: SCIENCE I NAME : :V ____ RO
INTERNATIONAL INDIAN Sub: SCIENCE I NAME : :V ____ RO

... III. Fill in the blanks:1. Minerals are mostly found in rocks as ___________________________. 2. Coal is obtained from________________________________________.. 3. Hidden fuels in the crust of the earth are ______________and______________. 4. Redfort in Delhi is made up of red______________________ ...
Name: Igneous Rocks Homework Extrusive Igneous Rocks: #23
Name: Igneous Rocks Homework Extrusive Igneous Rocks: #23

... #23. What is the luster of this igneous rock sample ? _________________ Do you see any mineral grains in this rock ? What is the name of this igneous rock ? ...
Plate Tectonics
Plate Tectonics

... that lived 270 million years ago • remains (fossils) found in South America and Africa • impossible for these reptiles to have crossed the Atlantic ...
Plate Tectonics
Plate Tectonics

... that lived 270 million years ago • remains (fossils) found in South America and Africa • impossible for these reptiles to have crossed the Atlantic ...
Melting of the mantle
Melting of the mantle

... ‰Strong link between convergent plate boundaries and CalcCalc alkaline volcanism (and associated intrusives). ‰Andesite is the dominant rock type found in most island arcs; more common in older, more mature arcs, such as Japan; while basalts and basaltic-andesite are more common on younger, younger ...
Skills Worksheet
Skills Worksheet

... a. uplift. c. faulting. b. folding. d. subsidence. _____ 9. The type of fault in which the hanging wall moves up relative to the footwall is called a a. strike-slip fault. c. normal fault. b. fault-block fault. d. reverse fault. _____ 10. The type of mountain that forms when rock layers are squeezed ...
< 1 ... 758 759 760 761 762 763 764 765 766 ... 791 >

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.
  • studyres.com © 2025
  • DMCA
  • Privacy
  • Terms
  • Report