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CRCT Review Packet
CRCT Review Packet

Plate Tectonics
Plate Tectonics

... Which feature would most likely be forming at converging continental tectonic plate boundaries? A. ...
Review
Review

... 35. What is the broadest division of environments on Earth, especially for larger organisms? 36. How does average temperature on Earth vary with latitude? 37. How do wind and air masses move in response to the coriolis effect in the northern hemisphere? 38. By what two broad criteria is climate defi ...
Continental Drift Hypothesis - states that the continents had once
Continental Drift Hypothesis - states that the continents had once

... Seafloor spreading produces new oceanic lithosphere. Continental Rifts - When spreading centers develop within a continent, the landmass may split into two or more smaller segments. Subduction zone - when one oceanic plate is forced down into the mantle beneath a second plate. ...
Lithosphere
Lithosphere

... What is a mid-ocean ridge ...
PHYSICAL GEOGRAPHY
PHYSICAL GEOGRAPHY

... c. Influence of Large Bodies of Water d. Ocean Currents 42. Climate Graph and Statistics 43. Microclimates 44. Air Masses  Bodies of air that develop over large areas  Take on the characteristics of where they are formed 45. Fronts ...
Continental-Drift-and-Seafloor-Spreading
Continental-Drift-and-Seafloor-Spreading

... 3. Glossopteris- plant fossils found on different continents- Plant fossils 4. Tropical plant fossils that were found on an island in Artic Ocean! (Scratches in rocks made by glaciers in South Africa) The continental drift theory was NOT accepted because Wegener could not explain HOW the continents ...
20130926123994
20130926123994

... • Pangaea – one large land mass • Africa & South America moved apart • India & Asia collided forming…. ...
Rock Type Puzzle
Rock Type Puzzle

... These can be broken down by These can be found all around weathering and moved by us and are collected by many erosion. people. ...
Plate Tectonic Learning Target Sheet
Plate Tectonic Learning Target Sheet

... thickness of each layer and its composition. Include Asthenosphere and Lithosphere. ...
Chapter 13 Earthquakes and Earth`s Interior
Chapter 13 Earthquakes and Earth`s Interior

Chapter 5
Chapter 5

Today`s Warm-Up Friday, January 10
Today`s Warm-Up Friday, January 10

... – Energy waves from earthquakes, change path and speed as they move through the Earth. Why? – Waves travel differently through different materials ...
Student Notes - Unit 3 (P.2)
Student Notes - Unit 3 (P.2)

... o Meteorite = fragments of asteroids and small early plants that broke upon impact with other bodies in space. o It is believed meteorites were formed the same way and are made from similar materials as Earth. o There are two kinds: 1. iron-nickel meteorites = similar to Earth’s core 2. stony meteor ...
The Earth - Humble ISD
The Earth - Humble ISD

... _______________ – soft layer of molten rock (magma) Crust – thin layer of rock on earth’s surface Continental Drift – __________________ first presented the theory. He claimed that in Earth’s early existence there was only one body of land, ______________. That supercontinent then slowly split and s ...
Mid-Atlantic Ridge
Mid-Atlantic Ridge

... 3. Similar fossils can be found on different continents ...
MINERAL COMPOSITION OF IGNEOUS ROCKS
MINERAL COMPOSITION OF IGNEOUS ROCKS

... (Mg). Intermediate compositions have an intermediate color, often gray or consisting of equal parts of dark and light mineral . Beware that even though an igneous rock may have a felsiccomposition (light color), the rock can contain dark colored minerals. Mafic rocks may contain light colored minera ...
Ch. 8 Vocab Study Guide
Ch. 8 Vocab Study Guide

... 2. The ________________________ is located directly under the lithosphere. This is a layer of hotter and softer rock in the mantle. 3. The switch in the Earth’s magnetic field is called: _______________________________________ 4. A solid sphere of metal at the Earth’s center: _______________________ ...
Physical Geology
Physical Geology

Answers
Answers

... (bottom 4 rocks). Mineral alignment is found in the first three rocks, and the mineral pyroxene is found in schist and gneiss. Since the question states that the rock does not have banding it is not Gneiss and must by Schist. 2. (3) Looking at the Rock Cycle chart on page 6 of the ESRT, the type of ...
File
File

... What is the fact that it was a freshwater creature separated today by the Atlantic Ocean and found where Africa and S. America would ...
Regional Processes 1.3.1
Regional Processes 1.3.1

... igneous rocks are quartz, orthoclase, and plagioclase feldspars, biotite and muscovite micas, amphibole, pyroxene, and olivine. State, with the aid of a diagram, the order in which the minerals listed above crystallise from a melt, and relate this order to the mineral composition of rocks. Explain h ...
Plate Boundaries - Valhalla High School
Plate Boundaries - Valhalla High School

... of plates that ride on top of the asthenosphere • The plates move due to convection currents in the mantle ...
5.12 A interpret how land forms are the result of a combination of
5.12 A interpret how land forms are the result of a combination of

... A. Erosion is the process of moving particles from one place to another. C. Deposition is the process in which sediments are dropped from one place to another. D. Wind is a force that produces weathering or erosion. ...
Geology: The Earth and Its Changes
Geology: The Earth and Its Changes

... Science 5.3.2.a: Analyze and interpret data identifying ways Earth’s surface is constantly changing through a variety of processes and forces such as plate tectonics, erosion, deposition, solar influences, climate, and human activity ...
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Tectonic–climatic interaction



Tectonic–climatic interaction is the interrelationship between tectonic processes and the climate system. The tectonic processes in question include orogenesis, volcanism, and erosion, while relevant climatic processes include atmospheric circulation, orographic lift, monsoon circulation and the rain shadow effect. As the geological record of past climate changes over millions of years is sparse and poorly resolved, many questions remain unresolved regarding the nature of tectonic-climate interaction, although it is an area of active research by geologists and palaeoclimatologists.
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