Chp2 Forces Building the Land
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The document discusses plate tectonics and how it has shaped the Earth's surface over geologic time. It describes how the Earth's crust is made up of large plates that move over convection currents in the mantle. When plates diverge new crust forms as magma rises, and when they converge mountains can form through collision or subduction zones can create volcanoes. It then outlines the four eras of geologic time - Precambrian, Paleozoic, Mesozoic, and Cenozoic - and some of the key events and lifeforms that emerged during each era, which ultimately gave the Earth its current shape and features through mountain building and erosion.
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Similar to Chp2 Forces Building the Land
Chapter1
The document provides an overview of the geological history of Montana from over 4 billion years ago to present day. It describes how continents collided and volcanic activity shaped the landscape, leaving behind fossils and mineral deposits. Glaciers advanced and retreated across the land during ice ages in the Cenozoic era. Geologists can study the layers of rock and fossils to piece together how the physical features of Montana were formed by various geological processes over millions of years.
Environmental studies notes for Marine students
The document summarizes the formation of Earth from a cloud of dust and gas to the planet we know today. Billions of years ago, a disturbance in a giant cloud caused it to collapse and form a spinning disc that became the Sun and planets. Earth formed as matter collided and accumulated. Early Earth was molten, and oceans formed as it cooled over hundreds of millions of years. Asteroid impacts also contributed water and allowed life to evolve in the oceans over billions of years.
2012 updated plate tectonics new one use this one backup
Plate tectonics theory proposes that Earth's outermost layer is broken into rigid tectonic plates that constantly move atop the asthenosphere in response to convection currents in the mantle, interacting along plate boundaries through divergent, convergent, and transform motion that creates geologic features like mid-ocean ridges, trenches, volcanoes, and earthquakes. Mapping of the seafloor revealed evidence like magnetic stripes and the ages of rocks that supported seafloor spreading and subduction, leading scientists in the 1960s to combine these ideas with continental drift into the unified theory of plate tectonics.
2013 updated plate tectonics new one use this one
The document summarizes plate tectonics and the development of the theory. It describes how early scientists like Wegener proposed continental drift but lacked evidence. Later, mapping of the ocean floor revealed patterns of magnetic stripes and rock ages indicating the seafloor spreads from mid-ocean ridges. This led scientists in the 1960s to develop the modern theory of plate tectonics, which proposes that Earth's crust is divided into plates that move due to convection currents in the mantle.
Plate Tectonics 9
1) Earth's lithosphere is made up of tectonic plates that rest on the mantle and slowly move, dragging the plates along the surface.
2) There are three types of plate boundaries - divergent where plates move apart, convergent where plates collide, and transform where plates slide past each other horizontally.
3) Evidence like matching rock formations and fossils found on separated continents support Alfred Wegener's theory of continental drift that all land was once part of a single supercontinent called Pangea that has drifted apart over time.
Fold mountain mystery
Alfred found fossils of sea creatures high in the Alps mountains. Geosynclines were large depressions that often contained seas and sea life. The Alps formed at a collision boundary where tectonic plates pushed sedimentary rocks and their fossils upwards over millions of years. Alfred discovered an out of place fossil that led him to research plate tectonics and how movement at plate boundaries explained the presence of marine fossils in the Alps mountains.
3.2
Continental drift theory developed by Alfred Wegener in 1912 proposes that the Earth's continents were once joined together and have been slowly moving apart over geologic time. Evidence for this includes matching fossil and rock formations found on different continents, as well as evidence that climates have changed in certain areas. The theory of plate tectonics expanded on this, stating that the Earth's lithosphere is made up of plates that move over Earth's surface, causing geologic events where they meet.
Earth science. Plate Tectonics ppt
The document summarizes plate tectonics and the structure and dynamics of the Earth. It describes the four main layers of the Earth and explains that plate tectonics involves the constant motion of tectonic plates due to convection currents in the mantle. It provides evidence that supported the theory of continental drift and discusses how sea floor spreading and subduction at trenches cause the plates to move over time.
Marine 11 4-11
The document discusses evidence for seafloor spreading and plate tectonics including:
1) Radiometric dating shows seafloor rock is younger than continental rock, indicating seafloor is constantly being created at mid-ocean ridges and destroyed in trenches.
2) Sediment samples show the most buildup near trenches where the oldest seafloor is located.
3) Magnetometer data on basalt minerals revealed a pattern of magnetic pole reversals indicating seafloor is continually being created and moved away from ridges by convection currents in the mantle.
Cooking Up Crude
Over millions of years, microscopic marine plants and animals that lived in an ancient sea covering Oklahoma died and sank to the ocean floor. Sediment gradually buried them, subjecting the remains to intense heat and pressure over time. This transformed the organic material into oil and natural gas trapped within sedimentary rock formations. Today, these fossil fuels are extracted from 71 of Oklahoma's 77 counties.
Plate Tectonics is the driving force of geologic structures th.docx
Plate Tectonics is the driving force of geologic structures that shape the world that we live in. The
first indication that continents might have been linked physically took place as soon as there was
mapping. It was known by the sixteenth and seventeenth century that the continents fitted together like
pieces of a puzzle. This and other proofs listed below lead to the concept of continental drift, that the
large continents had once been linked together. The scale movements of continents across the across
the surface of the planet was mind boggling.
By the close of the nineteenth century the geologist Edward Suess postulated that the southern
continents were joined together. This was from evidence seen by fossil animal distribution. Ancient life
forms have ranges just as modern animals. Tigers are found in India and Siberia, not in North America.
These ancient animals couldn’t get from South America to Africa, from Antarctica to Australia to India.
There were rock layers both sedimentary and igneous that were continuous on all of the five continents.
He christened this large continent Gondwanaland.
In 1915 Alfred Wegener wrote a book on continental drift. He proposed another super continent
called Pangaea. This continent included all of the modern continents. His mechanism for the movement
of the continents was that the continents moved through ocean crust, drifting until they joined then
breaking apart again. Wegener and others argued for their evidence pointing out rock similarities
type, similarities in rock trends and ages using all of the information gathered from Steno's laws and
fossil assemblages. They also showed that certain distant continents had similar plants and animals that
entered a different evolutionary path after the continents separated. An example of this is the fresh
water fish the Arowana found in both South America and Australia. Another example of this is the large
amount of marsupial
fossils found in South
America and Australia.
Placental mammals
were the dominant
mammalian life forms
in Eurasia, North
America and Africa.
Only in South America
and Australia were
marsupial fossils
dominated. It wasn't
until 3 million years ago
North and South
America joined
allowing placental
mammals to gain
dominance in South America. Despite this evidence Wegener and his followers mechanism for
continental movement was badly flawed. They proposed that the tidal forces from the Sun and Moon
like the tides in the ocean. This force is much too weak to move a continent so the theory was rejected.
Fossil plants and animal distribution on southern continents
In 1928 a geologist Arthur Holmes proposed the convection currents split the continents and that
these currents were in the mantel. Remember the knowledge of a mantel was already known at this
time. Ironically this was a mechanism had been proposed by Benjamin Franklin in 1782. Many
geologi.
Earth&PlateTectonics_Butler_ERBmod.ppt
The document discusses plate tectonics and provides evidence that supports the theory of continental drift. It describes how the Earth's crust is broken into plates that move relative to each other. The plates interact in different ways as they move, including colliding, pulling apart, and scraping past one another, which causes geological features like mountains and volcanoes to form. It also explains Alfred Wegener's early theory of continental drift and the fossil, geological, and geographical evidence he used to support the idea that the continents were once joined together in a supercontinent called Pangaea.
CSEC GEOGRAPHY
This is the entire CSEC geography syllabus (some things might be missing). The information was collected from various websites and textbooks. The topics are:
- Internal forces
-External forces
-Rivers
-Limestone
-Coasts
-Coral reefs and Mangroves
-Weather and Climate
- Ecosystems (vegetation and soils)
-Natural hazards
- Urbanization
-Economic activity
-Environmental degradation
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.
Landforms thislandisourland-111022123136-phpapp01
This document discusses different landforms found on Earth. It describes landforms that are found on continents, such as mountains, canyons, hills and valleys, as well as undersea landforms like seamounts, trenches, and ridges. It explains how landforms are created by both constructive forces that build up land through processes like plate tectonics, and destructive forces like weathering and erosion that wear down land over time. Plate tectonics and the movement of tectonic plates are key to forming many landforms at plate boundaries.
Plate Tectonics
The document provides an overview of the structure and composition of the Earth's layers, including the crust, mantle, and core. It then discusses plate tectonics and evidence that supports the theory of continental drift, such as matching geological formations and fossil distributions between continents before they drifted apart. The development of the modern theory of plate tectonics to explain continental movement is also outlined.
Chapter 1 plate tectonics power point
The document summarizes key aspects of plate tectonics theory, including:
1) Earth is made up of layers with different densities and properties, including the crust, mantle, outer core, and inner core.
2) The lithosphere is made of tectonic plates that move over time, splitting and colliding in various ways. This explains continental drift and the movement of continents.
3) Tectonic plates interact at three main types of boundaries - divergent where plates move apart, convergent where they push together, and transform where they slide past each other. These boundary interactions shape Earth's surface over geological time.
Geology Complete (Earth Science Topic)
This document discusses the theory of continental drift and plate tectonics. It explains that continental drift is the movement of continents across Earth's surface over geologic time. The theory was first proposed in the early 20th century by Alfred Wegener and helped explain the formation of supercontinents like Pangaea and the matching of continental margins. It also introduced the concept of plates and how their movement causes geologic phenomena like earthquakes and volcanoes.
Plate Tectonics
The movement of earth's plate is responsible for the formation of continents.How it works ? what are the principle's?
Study of plate tectonics of the earth, or plate movement,
a) Wegener’s Evidence (Continental Drift)
b) History of Plate Tectonics
c) Breakup and Appearence of Pangea
WHAT IS A PLATE?
Major continental and oceanic plates include:
Types of Earth’s Crust:
Plate tectonics (from the Late Latin tectonicus) is a scientific theory which describes the large scale motions of Earth's lithosphere.
THE DYNAMIC EARTH:
The earth is a dynamic planet, continuously changing both externally and internally. The earth’s surface is constantly being changed by endo-genetic processes resulting in volcanism and tectonism, and exogenetic processes such as erosion and deposition. These processes have been active throughout geological history. The processes that change the surface feature are normally very slow (erosion and deposition) except some catastrophic changes that occur instantaneously as in the case of volcanism or earthquakes. The interior of the earth is also in motion. Deeper inside the earth, the liquid core probably flows at a geologically rapid rate of a few tenths of mm/s. Several hypotheses attempted to explain the dynamism of the earth.
+ Horizontal movement hypothesis
+ Continental drift, displacement hypothesis
Development of the plate tectonic theory.
Plate tectonic theory arose out of the hypothesis of continental drift proposed by Alfred Wegener in 1912. He suggested that the present continents once formed a single land mass that drifted apart, thus releasing the continents from the Earth's core and likening them to "icebergs" of low density granite floating on a sea of denser basalt.
Seafloor Spreading
The first evidence that the lithospheric plates did move came with the discovery of variable magnetic field direction in rocks of differing ages.
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2012 updated plate tectonics new one use this one backup
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Plate Tectonics is the driving force of geologic structures th.docx
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Study of plate tectonics of the earth, or plate movement,
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Syllabus
Chapter-1
Introduction to objective, scope and outcome the subject
Chapter 2
Introduction: Scope and Specialization of Civil Engineering, Role of civil Engineer in Society, Impact of infrastructural development on economy of country.
Chapter 3
Surveying: Object Principles & Types of Surveying; Site Plans, Plans & Maps; Scales & Unit of different Measurements.
Linear Measurements: Instruments used. Linear Measurement by Tape, Ranging out Survey Lines and overcoming Obstructions; Measurements on sloping ground; Tape corrections, conventional symbols. Angular Measurements: Instruments used; Introduction to Compass Surveying, Bearings and Longitude & Latitude of a Line, Introduction to total station.
Levelling: Instrument used Object of levelling, Methods of levelling in brief, and Contour maps.
Chapter 4
Buildings: Selection of site for Buildings, Layout of Building Plan, Types of buildings, Plinth area, carpet area, floor space index, Introduction to building byelaws, concept of sun light & ventilation. Components of Buildings & their functions, Basic concept of R.C.C., Introduction to types of foundation
Chapter 5
Transportation: Introduction to Transportation Engineering; Traffic and Road Safety: Types and Characteristics of Various Modes of Transportation; Various Road Traffic Signs, Causes of Accidents and Road Safety Measures.
Chapter 6
Environmental Engineering: Environmental Pollution, Environmental Acts and Regulations, Functional Concepts of Ecology, Basics of Species, Biodiversity, Ecosystem, Hydrological Cycle; Chemical Cycles: Carbon, Nitrogen & Phosphorus; Energy Flow in Ecosystems.
Water Pollution: Water Quality standards, Introduction to Treatment & Disposal of Waste Water. Reuse and Saving of Water, Rain Water Harvesting. Solid Waste Management: Classification of Solid Waste, Collection, Transportation and Disposal of Solid. Recycling of Solid Waste: Energy Recovery, Sanitary Landfill, On-Site Sanitation. Air & Noise Pollution: Primary and Secondary air pollutants, Harmful effects of Air Pollution, Control of Air Pollution. . Noise Pollution Harmful Effects of noise pollution, control of noise pollution, Global warming & Climate Change, Ozone depletion, Greenhouse effect
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2. Satheesh Gopi, Basic Civil Engineering, Pearson Publishers.
3. Ketki Rangwala Dalal, Essentials of Civil Engineering, Charotar Publishing House.
4. BCP, Surveying volume 1
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Chp2 Forces Building the Land
- 1. Forces Building the Land Chapter 2
- 4. What we are going to look at in this chapter… The Geologic age of the Earth The ability of parts of the Earth’s crust to move around How volcanoes and earthquakes are formed by plate tectonics
- 8. Show slide show of plate tectonics (2) Teachers domain Plate Tectonics: Alfred Wegener
- 13. The Big Nickel, Sudbury ON
- 16. Geologic Eras
- 17. Take a trip into the Earth’s History http://www.scotese.com/
- 19. Precambrian Era
- 22. Animals in the Mesozoic Era
- 26. The Four Eras of Geologic Time What do you notice? First Invertebrates First land plants First fish First reptiles First amphibians First dinosaurs, mammals, birds End of dinosaurs Millions of years ago 0- 100- 200- 300- 400- 500- 600- 700- 4600-
- 28. Label the Landform regions and create a legend wb. P. 12