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World Tectonic Mapping Activity
World Tectonic Mapping Activity

3-1 Notes: Mountains Think About… How can a solid (like rock) fold
3-1 Notes: Mountains Think About… How can a solid (like rock) fold

...  Even the most _________________________ earthquakes only move rocks a small number of meters.  It takes millions of years and earthquakes to build up large fault-block mountain ranges, like the Sierra Nevada range in California.  All mountains take millions of year to ____________________. Revie ...
Chapter 4: geography and earth questions
Chapter 4: geography and earth questions

... What is the leading factor in outgassing? (volcanic activity) What percent of the freshwater is in the polar ice caps? (69% or 2/3) What is the maximum density of sea water? (2C) Which is more dense: basalt or granite? (basalt) Which type of crust is characteristic of basalt? (oceanic) What process ...
Chapter 4: geography and earth questions
Chapter 4: geography and earth questions

... What is the leading factor in outgassing? (volcanic activity) What percent of the freshwater is in the polar ice caps? (69% or 2/3) What is the maximum density of sea water? (2C) Which is more dense: basalt or granite? (basalt) Which type of crust is characteristic of basalt? (oceanic) What process ...
class_intro
class_intro

... • While at University of Marburg in 1911, Wegener was browsing in the library when he came across a paper that listed fossils of identical plants and animals found on opposite sides of the Atlantic (Brazil and Africa) • Intrigued, Wegener began to look for, and find, more cases of similar fossils se ...
Types of Plate Boundaries
Types of Plate Boundaries

... • Ocean crust is destroyed at convergent plate boundaries or landmasses collide. • Each depends on the type of crust involved: • There are three types of Convergent Plate Boundaries – Ocean vs. Ocean crust (subduction zone) – Continental vs. Ocean crust (subduction zone) – Continent vs. Continent cr ...
Earth systems plate tectonics homework
Earth systems plate tectonics homework

... and the theory of plate tectonics to explain the ages of crustal rocks. Success Criteria:  Identify the three general categories of plate boundaries recognized by scientists: convergent, divergent, and transform  Compare and contrast continental and oceanic crust in terms of composition, density, ...
REVISED EXAM 3 STUDY GUIDE – PHYSICAL GEOGRAPHY
REVISED EXAM 3 STUDY GUIDE – PHYSICAL GEOGRAPHY

... The greatest concentration of destructive earthquakes occur: a. Along the mid-ocean ridges b. Around the Pacific Ring of Fire c. In California d. In the Appalachians ...
Translate the text from English into Russian.
Translate the text from English into Russian.

... is driven by the heat due to decay of radioactive potassium, thorium, and uranium, which were selectively incorporated in the crystal lattices of the lower-density minerals that form the mantle. There are several independent sources of evidence of this motion. First, there are gravitation anomalies; ...
ZERNOLA: Irene Lopez, Leire Guerrico, Nagore Azkue
ZERNOLA: Irene Lopez, Leire Guerrico, Nagore Azkue

... Notable minor plates include the Arabian Plate, the Caribbean Plate, the Juan de Fuca Plate, the Cocos Plate, the Nazca Plate, the Philippine Plate and the Scotia Plate. The movement of plates has caused the formation and break-up of continents over time, including occasional formation of a super co ...
Sequencing Activity
Sequencing Activity

... Note to the teacher. Cut the text into strips and give to pairs of students to sequence. The students place the text into the text box. Step 1 has been given. Alternatively, students could write the sentences in the text boxes as the text is already in jumbled order. -------------------------------- ...
Sea-Floor Spreading
Sea-Floor Spreading

... and then records the echoes of these sound waves. Sonar mapped midocean ridges. ...
Convection in the Mantle: Using a Lava Lamp as a
Convection in the Mantle: Using a Lava Lamp as a

... particularly in the softer, taffy-like asthenosphere of the upper mantle that carries the earth’s lithospheric plates. 5. What makes the earth’s core so hot (give two reasons)? ____________________________________________________________________________ 6. Think about the three types of heat transfe ...
The Theory of Plate Tectonics
The Theory of Plate Tectonics

... will thin in the middle until it is stressed so much that it breaks. • Happens on land & under H2O ...
Student Notes
Student Notes

... -Examples: Hawaiian Islands on the Pacific Plate and ____________________ on the North American Plate 2. When will the new Hawaiian island, Loihi appear? -50,000 to 100,000 years from now, it’s accumulating layer after layer from the ocean floor at 8,000 feet from the ocean floor M. The Breakup of P ...
Plate Boundaries and Faults Notes
Plate Boundaries and Faults Notes

... a) Plate Boundaries – are the point where two tectonic plates meet and are divided into three types – convergent, divergent, and transform. Plates are classified into one of the three types based on the movement that they have. Remember: convection currents are the engines that drive plate movement. ...
Chapter 3 Plate Tectonics
Chapter 3 Plate Tectonics

... along the bottom of the oceans, they are the deepest parts of the oceans close to continents or near strings of islands such as Alaska’s Aleutian Islands . • Why is the location of these trenches significant? • The trenches create the Ring of Fire. ...
The theory of plate tectonics
The theory of plate tectonics

... last 70 years and start all over again," said another American scientist. Anyone who "valued his reputation for scientific sanity" would never dare support such a theory, said a British geologist. ...
Chapter 1 Introduction to Earth Science Chapter Test Earth Science
Chapter 1 Introduction to Earth Science Chapter Test Earth Science

... 6. What are the three main parts of the geosphere? a. atmosphere, crust, core b. lithosphere, mantle, core c. crust, mantle, core d. asthenosphere, lithosphere, atmosphere Name ___________________________ Class ___________________ Date _____________ 7. The theory of plate tectonics helps scientists ...
Lecture 4
Lecture 4

... The location beneath the surface where the earthquake begins is called the focus, this should not be confused with the epicenter which is the point on the surface of the Earth that lies directly over the focus. ...
Juniata College Science in Motion Introduction: The theory of plate
Juniata College Science in Motion Introduction: The theory of plate

... The theory of plate tectonic grew out of the theory of Continental Drift. The continental drift theory proposed that the continents were drifting like ships on an ocean. It was based on a few facts such as fossil remains, glacial scaring and the connection of mountain ranges in various parts of the ...
The Movement of Mountains | Questions on Islam
The Movement of Mountains | Questions on Islam

... constant motion. What does the movement of mountains like clouds mean? What do scientists say about this fact informed by the Quran 1.400 years ago? Now, let us see what science says about it: For the first time in history, a German scientist called Alfred Wegener proposed that the continents of the ...
Divergent Plate Boundaries
Divergent Plate Boundaries

... inches/year - about the same rate as your fingernails grow! ...
Urška Slivšek, 1.E GIMB PACIFIC NORTHWEST OVERDUE FOR A
Urška Slivšek, 1.E GIMB PACIFIC NORTHWEST OVERDUE FOR A

... southern portion along Oregon and California breaks every 230 years on average .This paper is important because it is an excellent synthesis of two widely divergent fields of Earth science," . One field is what's called microstratigraphy, which is what allowed for the deciphering of the tidal marshe ...
PPT-Int-Plate Tectonics - Interactive Science Teacher
PPT-Int-Plate Tectonics - Interactive Science Teacher

... bottom. Cut the pieces apart. See: The pieces separated, but the black line shows how they used to fit. What’s Happening: Coal deposits from different continents line up, suggesting there once was a super continent called Pangaea. There’s also the puzzle-like fit, fossils, climate, and other rock cl ...
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Plate tectonics



Plate tectonics (from the Late Latin tectonicus, from the Greek: τεκτονικός ""pertaining to building"") is a scientific theory that describes the large-scale motion of Earth's lithosphere. This theoretical model builds on the concept of continental drift which was developed during the first few decades of the 20th century. The geoscientific community accepted the theory after the concepts of seafloor spreading were later developed in the late 1950s and early 1960s.The lithosphere, which is the rigid outermost shell of a planet (on Earth, the crust and upper mantle), is broken up into tectonic plates. On Earth, there are seven or eight major plates (depending on how they are defined) and many minor plates. Where plates meet, their relative motion determines the type of boundary; convergent, divergent, or transform. Earthquakes, volcanic activity, mountain-building, and oceanic trench formation occur along these plate boundaries. The lateral relative movement of the plates typically varies from zero to 100 mm annually.Tectonic plates are composed of oceanic lithosphere and thicker continental lithosphere, each topped by its own kind of crust. Along convergent boundaries, subduction carries plates into the mantle; the material lost is roughly balanced by the formation of new (oceanic) crust along divergent margins by seafloor spreading. In this way, the total surface of the globe remains the same. This prediction of plate tectonics is also referred to as the conveyor belt principle. Earlier theories (that still have some supporters) propose gradual shrinking (contraction) or gradual expansion of the globe.Tectonic plates are able to move because the Earth's lithosphere has greater strength than the underlying asthenosphere. Lateral density variations in the mantle result in convection. Plate movement is thought to be driven by a combination of the motion of the seafloor away from the spreading ridge (due to variations in topography and density of the crust, which result in differences in gravitational forces) and drag, with downward suction, at the subduction zones. Another explanation lies in the different forces generated by the rotation of the globe and the tidal forces of the Sun and Moon. The relative importance of each of these factors and their relationship to each other is unclear, and still the subject of much debate.
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