• 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
Sea Floor Spreading Plate Tectonics Review Game
Sea Floor Spreading Plate Tectonics Review Game

Plate Tectonics 2
Plate Tectonics 2

... •Continental fit can also be used to piece together previous continental (and thus plate) positions. Regions where the continents do not fit together perfectly can often be explained through subsequent erosion or other activity (the formation of deltas and deepsea fans, creation of volcanic rocks at ...
Pacific Northwest
Pacific Northwest

... 13. A _______ is a concentrated area of major, long-term volcanic activity fed by a rising plume of magma. This area can cause landmass changes within a tectonic plate and is not necessarily associated with a plate boundary. The island of Hawai'i is a classic example. A. transform boundary B. mid-oc ...
Extinction Hypothesis B – Continental Drift
Extinction Hypothesis B – Continental Drift

... Volcanism: We are quite certain that the end of the Cretaceous period that there was increased volcanic activity. Over a period of several million years, this increased volcanism could have created enough dust and soot to block out sunlight; producing the climatic change. In India during the Late Cr ...
final_exam - Winthrop Chemistry, Physics, and Geology
final_exam - Winthrop Chemistry, Physics, and Geology

... 7. [True or False] The Sun radiates only in the visible spectrum. 8. [True or False] The Hawaiian Islands are a textbook example of a volcanic island arc formed from subduction. 9. [True or False] High pressure systems are generally associated with the development of large weather systems like warm ...
Convection homework
Convection homework

... creates pockets of circulation within the mantle called _, which are thought to be the force behind the movement of tectonic plates over the asthenosphere. A. magma flows C. convection cells B. density cells D. conduction points 12. Geologists trying to drill into the mantle would most likely drill ...
volcanoreview
volcanoreview

... Mt Rainier and Mt St Helens are good examples of __________ composite cones, with explosive eruptions and erupted materials such as ash, bombs, and blocks. ...
Earth and Space Science (Volcanoes)
Earth and Space Science (Volcanoes)

... Content Statement ESS.1.2 Earth’s crust consists of major and minor tectonic plates that move relative to each other. ESS.1.2.c There are three main types of plate boundaries: divergent, convergent and transform. Each type of boundary results in specific motion and causes events (such as earthquakes ...
File - Leaving Certificate Geography
File - Leaving Certificate Geography

... apart by convection currents in the mantle below Caused by heat released from natural radioactive processes At the mid Atlantic ridge molten rock from below rises up to fill the gap with new basaltic rock ...
GEOLOGY 11 EXAM 3 STUDY QUESTIONS
GEOLOGY 11 EXAM 3 STUDY QUESTIONS

12.13-plate-tectonics
12.13-plate-tectonics

... 1. A – earth’s core is mostly Iron and Nickel 2. C- subduction is one plate passing under another 3. B- Hawaii was formed at a hot spot (a weakness in the pacific ocean plate where magma was allowed to leak out) 4. B- see whiteboard 5. E- metamorphic rock is formed at high temp/pressure 6. C- earthq ...
I. Convergent plate boundaries (destructive margins) (colliding
I. Convergent plate boundaries (destructive margins) (colliding

... b. Age of deepest sediments in any area (those upon basalt sea floor) 1) Youngest are near the ridges 2) Older are at a distance from the ridge c. Supports tectonic hypothesis prediction that ocean basins are geologically young 1. oldest sea floor sediments found are 180 m.a. 2. continental crust, b ...
Document
Document

... the plates pull away from each other. 2. Convergent boundaries -- where crust is destroyed as one plate dives under another. 3. Transform boundaries -- where crust is neither produced nor destroyed as the plates slide horizontally past each other. 4. Plate boundary zones -- broad belts in which boun ...
tectonic plates
tectonic plates

... What are mid-ocean ridges? Divergent = spreading boundaries  Mid-ocean ridge- An undersea mountain range with a rift valley running through the center of it ...
Examples posted for the midterm test.
Examples posted for the midterm test.

... 35 questions, all of which can be answered on a SCANTRON sheet. In each case select the answer that is the MOST correct. 1. The San Andreas fault experiences an average annual movement of: a) b) c) d) e) ...
How Are Landforms Created and Changed Handout
How Are Landforms Created and Changed Handout

... The plates __________ constantly. Their movement is ____________ by convection flows underneath them. Convection flow is the circular motion that occurs when warmer material rises and is replaced by cooler material. The plates ___________ on the asthenosphere, which is a layer of semi-molten rock un ...
Jordan`s Science Rap
Jordan`s Science Rap

... Crust, mantle, core That’s not all that I heard Crust is the thinnest And mantle is the thickest Don’t forget poor little core The core is the hottest The hottest of them all ...
File
File

... 7. What was the name of the supercontinent that the person in the above question came up with? ...
PPT - Chapter 2: Plate Tectonics & The Ocean Floor
PPT - Chapter 2: Plate Tectonics & The Ocean Floor

... Transform Faults/Boundaries • Plates slide past one another along faults in the lithospheric plate • Crustal material is neither created nor destroyed Ex: San Andreas Fault ...
Announcements
Announcements

Tectonic plates, Earthquakes, and the Earth`s guts
Tectonic plates, Earthquakes, and the Earth`s guts

... demonstrate this. Melted cheese, melted chocolate, or thick gravy heated in a saucepan will form a crust on top that cracks and moves as the goop is heated. Note that the goop does not have to boil in order for “convection currents” to move the surface! Very slow convection currents in the mantle (r ...
File - Leaving Certificate Geography
File - Leaving Certificate Geography

... lithosphere are moved around by the underlying hot mantle convection cells ...
Plate Tectonics Vocabulary PPP- Sidney
Plate Tectonics Vocabulary PPP- Sidney

...  A circulation pattern in which material is heated and rises in one area, then cools and sinks in another area  The mantle is made of much denser, thicker material, because of this the plates "float" on it like oil floats on water.  Many geologists believe that the mantle "flows" because of conve ...
Class notes ()
Class notes ()

... Melting point as a function of pressure, water content and composition Partial melting of magma-generating rocks Fractional crystallization Shapes of magmatic bodies – sills, dykes, batholiths Hot spots and volcanoes (mafic composition) Volcanoes at convergent margins ( mafic to felsic composition) ...
Internal Structure of the Earth
Internal Structure of the Earth

< 1 ... 697 698 699 700 701 702 703 704 705 ... 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 © 2026
  • DMCA
  • Privacy
  • Terms
  • Report