Plate techtonics
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Plate tectonics involves the movement of tectonic plates. When plates meet, they can push together causing folding and mountain building, or one plate can subduct under another forming deep ocean trenches. The friction from plates moving against each other causes volcanoes and earthquakes. Evidence for plate tectonics includes matching coastlines, specific fossil and rock distributions, and lines of volcanoes along plate boundaries like the mid-Atlantic ridge.
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This document discusses the key concepts of plate tectonics including the types of plate boundaries and their associated features and hazards. There are three main types of plate boundaries: divergent boundaries where plates move apart, convergent boundaries where plates move together, and conservative boundaries where plates slide past each other laterally. Divergent boundaries form mid-ocean ridges and rift valleys, convergent boundaries involve subduction and result in volcanoes and earthquakes, and conservative boundaries include transform faults like the San Andreas Fault. The document also covers plate tectonic evidence, hotspots, and examples like the Himalayas and Hawaii to illustrate the concepts.
Notes on living with tectonic hazards 0 levels
Tectonic hazards such as earthquakes and volcanic eruptions are caused by movements of the Earth's crustal plates. The internal structure of the Earth consists of a crust, mantle, outer core, and inner core. The crust is broken into plates that move due to convection currents in the mantle and the sinking of denser plates. Plate boundaries include divergent boundaries where plates move apart, convergent boundaries where they move together, and transform boundaries where they slide past each other. Landforms associated with plate tectonics include mid-ocean ridges, rift valleys, fold mountains, trenches, and volcanoes. Earthquakes occur along plate boundaries when built-up stress is suddenly released during plate movement.
Notes on living with tectonic hazards n levels
1. Tectonic hazards such as earthquakes and volcanic eruptions are caused by movements of the Earth's crust along tectonic plates. The plates move due to convection currents in the upper mantle and subduction of denser oceanic plates under lighter continental plates.
2. Where plates diverge, mid-ocean ridges and rift valleys are formed. As plates converge, fold mountains like the Himalayas or Andes are formed. Transform boundaries like the San Andreas Fault cause earthquakes as the plates slide past each other.
3. Volcanoes form at plate boundaries due to upwelling of magma. Shield volcanoes have low, broad slopes while stratovolcanoes
4.forceof change
The document summarizes how the internal structure of the Earth, including its core, mantle, and crust, drives forces like volcanoes and earthquakes. It then discusses how the movement of tectonic plates over millions of years has shaped the Earth's surface features, splitting supercontinents like Pangaea and forming mountain ranges. External forces like weathering, wind erosion, water erosion, and glacial activity also slowly change the Earth's landscape over long periods of time.
Restless Earth 2 PowerPoint Presentation
The document discusses plate tectonics and the structure of the Earth. It describes the four main layers of the Earth - the inner core, outer core, mantle, and crust. The crust is broken into plates that move due to convection currents in the mantle. There are three main types of plate boundaries - constructive where plates move apart and new crust is formed, destructive where one plate is subducted under another, and conservative where plates slide past each other. Volcanoes and earthquakes often occur at plate boundaries as a result of this plate movement.
Plate margins
There are two types of crust - continental and oceanic - and three directions of plate movement - converging, diverging, and passive. This results in six plate boundary types: destructive (oceanic-continental convergence), destructive (oceanic-oceanic convergence), destructive (continental-continental collision), constructive (diverging at ocean ridges), constructive (continental rifting), and conservative (passive movement). Each boundary type creates different landforms and hazards due to the associated geological processes.
GEOGRAPHY IGCSE: PLATE TECTONICS
GEOGRAPHY IGCSE: PLATE TECTONICS. Earth's layers. Inner core, outer core, mantle, crust, the structure of Earth, plate boundaries and interactions, magma and igneous rocks, forming a volcano, compressional boundaries, folding.
Plate Boundaries
The document discusses the structure and composition of the Earth, including the crust, mantle, outer core, and inner core. It also discusses plate tectonics and the different types of plate boundaries: constructive, destructive, conservative, and collision. At destructive boundaries, oceanic plates are subducted under continental plates, forming volcanoes. At collision boundaries, continental plates push together to form mountain ranges. At constructive boundaries, plates move apart and new crust is formed.
Plate Tectonics
The document discusses plate tectonics and the structure and dynamics of the Earth's interior. It describes how the crust is broken into plates that move atop the mantle due to convection currents, and the three types of plate boundaries: divergent where plates move apart, convergent where they move together, and transform where they slide past each other. It provides examples of associated geological features like mid-ocean ridges, subduction zones, volcanoes, and earthquakes.
Plate Tectonics
This document provides information about plate tectonics and is designed to meet South Carolina science standards. It discusses the layers of the Earth, tectonic plates and their movement, and the three types of plate boundaries - convergent where plates collide, divergent where they separate, and transform where they slide past each other. Specific examples are given for each boundary type, including discussions of sea floor spreading at mid-ocean ridges, subduction zones creating volcanoes and trenches, and the San Andreas Fault as a transform boundary.
Chapter 2.in geomorphology
This document provides an overview of structural geomorphology and the key surface and subsurface processes that shape the Earth's landscapes. It discusses global geomorphology and the intersection between climatic, hydrologic, and biologic surface processes with underlying geologic processes. Specific topics covered include plate tectonics and the different landforms that form at divergent, convergent and transform plate boundaries. The document also discusses weathering processes, the factors that influence them, and characteristic landforms formed by weathering such as exfoliation domes and rock basins. Finally, it covers slope stability and the different types of landslides that can occur based on material type and movement.
Geography Chapter 2 PowerPoint
The document summarizes how various physical factors influence Earth's climate:
1) The sun is the main driver of climate, with latitude affecting the angle of sunlight and creating different climate zones.
2) Wind patterns like prevailing winds and monsoons also impact climate by affecting temperatures and rainfall. Local winds form near land and water boundaries.
3) Oceans and ocean currents influence climate by transporting warm and cool waters to land areas, while high elevations and mountain ranges can create "rain shadows" with drier climates on one side.
Tectonics: Plate tectonics Introduction
This document discusses key evidence for plate tectonics including matching fossils, rocks, and climate patterns found in different parts of the world. It describes plate boundaries like divergent boundaries where new crust forms at mid-ocean ridges, and convergent boundaries where plates collide including ocean-ocean, ocean-continent, and continent-continent collisions. It also discusses mantle plumes and hotspot volcanism. The key takeaways are that convection currents in the mantle drive plate motions, there are three main types of plate boundaries with different associated features and hazards, and hotspots represent fixed mantle plumes unrelated to boundaries.
Ch 03 - 05
Plate tectonics involves the movement of rigid crustal plates over a weak layer in the upper mantle. There are three main types of plate boundaries - divergent where plates move apart and new crust is formed, convergent where plates collide and one subducts, and transform boundaries where plates slide past each other. Different boundaries produce different surface features like mid-ocean ridges, coastal mountains, and faults. Volcanoes are associated with plate boundaries and come in different compositions from mafic to felsic depending on their location and the materials they form from. Volcanic hazards include lava flows, pyroclastic flows, ash falls, gases, lahars, and large eruptions can impact climate on a global
The sea floor
The Earth is made up of four ocean basins - Pacific, Atlantic, Indian, Arctic - which cover 71% of the planet. The ocean floor is composed of tectonic plates that are constantly shifting and spreading at mid-ocean ridges. As new crust is formed at ridges, old crust is destroyed through subduction at trenches. This process of sea floor spreading and plate tectonics explains continental drift over millions of years, from the single supercontinent Pangaea to the current configuration of lands and oceans.
The sea floor
The Earth is made up primarily of oceans that cover 71% of the planet. The oceans are divided into four major basins - Pacific, Atlantic, Indian, Arctic - as well as smaller connected seas. The structure of the Earth includes a dense iron core, swirling liquid outer core, mantle, and thin crust atop the mantle. There are differences between the oceanic crust, made of basalt, and continental crust, made of granite. Plate tectonics explains how the Earth's crust is broken into plates that move over time, causing continents to drift apart.
The sea floor
The Earth is made up of four ocean basins - Pacific, Atlantic, Indian, Arctic - which cover 71% of the planet. The ocean floor is composed of tectonic plates that are constantly shifting and spreading at mid-ocean ridges. As new crust is formed at ridges, old crust is destroyed through subduction at trenches. This process of sea floor spreading and plate tectonics explains continental drift over millions of years, from the single supercontinent Pangaea to the current configuration of lands and oceans.
CSEC Geography- Internal Forces - Plate Tectonics and Earthquakes
This document looks at the Earth's internal forces. The main layers of the earth are described. The history surrounding plate tectonics is discussed. The different types of plate boundaries is also explained.
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