This document provides information about plate tectonics through 5 sections:
1) It defines plate tectonics and provides diagrams of Earth's layers.
2) It describes where plate tectonics is occurring globally and locally through examples.
3) It discusses how plate tectonics has affected life on Earth through changing environments and fossil evidence.
4) It notes there are still issues and debates around fully understanding the mechanisms driving plate tectonics and predicting impacts.
5) It argues more research across scientific fields is needed to better comprehend plate tectonics and issues like its relationship to volcanism and climate change.
Plate tectonics refers to the theory that the Earth's crust is composed of large rigid plates that slowly move over the mantle. There are 7 major and many minor tectonic plates that are constantly changing through processes like combining, becoming crushed, or being subducted beneath another plate. When the plates shift it can cause earthquakes, tsunamis, elevation changes to land, and structural damage costing lives and property. Scientists are working to better predict plate shifts but preparing for possible impacts through building codes and emergency plans is currently the best approach.
An earthquake occurs when two blocks of the earth's crust slip past one another, causing the ground to shake. Most earthquakes happen along the edges of tectonic plates that slowly move and bump against each other deep underground. Earthquakes can cause massive damage and loss of life, such as the 1556 Shaanxi earthquake in China that killed over 800,000 people. Modern solutions aim to better predict, withstand, and prepare for earthquakes to minimize harm.
The document discusses earthquakes, including their causes, measurement, effects, and preparedness. Earthquakes occur due to the sudden release of built-up stress along fault lines in the earth's crust, causing seismic waves. Their magnitude is measured using scales like the Richter scale or moment magnitude scale. Earthquakes can damage infrastructure and the environment through ground shaking and secondary events like tsunamis or landslides. While earthquakes cannot be prevented, preparation through emergency planning and building design can reduce risks.
Earthquakes, landslides, volcanic eruptions and other disturbances can cause tsunamis by displacing large amounts of water. Tsunamis are a series of long sea waves that can travel across entire oceans within hours. Three-quarters of tsunamis occur in the Pacific Ocean due to high seismic activity along subduction zones that make up the Pacific Ring of Fire. When tsunamis reach land, they can devastate coastal areas by destroying homes and infrastructure and endangering human life. On average, two tsunamis occur globally each year, with about 80% originating in the Pacific Ocean.
1) Earthquakes are caused by the sudden release of energy from movement along geological faults in the earth's crust, generating seismic waves.
2) Larger earthquakes can trigger tsunamis if located offshore by displacing seabed, as well as landslides and volcanic eruptions.
3) Earthquake shaking causes loss of life and property destruction from building collapse and landslides burying infrastructure.
This presentation is for my Geography 110 class. Just an FYI if you are curious, the second to last slide that is captioned "Problems?" is about Red Tides
The document summarizes key aspects of Earth's internal structure, surface features, tectonic plates, earthquakes, volcanoes, and landforms. The Earth has a solid crust on top of a thick mantle and liquid outer and solid inner cores. Over 70% of the surface is ocean, covering underwater volcanoes, mountains and trenches. The remaining 30% includes various landforms like forests and deserts. Tectonic plates float on the mantle and interact, causing earthquakes and forming volcanoes and mountains. Earthquakes generate seismic waves and tsunamis. Volcanoes form at plate boundaries and erupt molten magma from the crust. Important landforms include mountains, valleys, plains and coastal features.
1) Tectonic plates slowly move across the Earth's surface over the course of a year, occasionally crashing into each other. When they crash, it can cause natural disasters like volcanic eruptions and earthquakes.
2) Volcanoes form as magma cools and piles up from cracks in the Earth's crust caused by the movement of tectonic plates and resulting earthquakes.
3) Tectonic plate collisions, though slow, continually form new landforms like mountains and volcanoes as the plates interact within the limited space available.
Plate tectonics refers to the theory that the Earth's crust is composed of large rigid plates that slowly move over the mantle. There are 7 major and many minor tectonic plates that are constantly changing through processes like combining, becoming crushed, or being subducted beneath another plate. When the plates shift it can cause earthquakes, tsunamis, elevation changes to land, and structural damage costing lives and property. Scientists are working to better predict plate shifts but preparing for possible impacts through building codes and emergency plans is currently the best approach.
An earthquake occurs when two blocks of the earth's crust slip past one another, causing the ground to shake. Most earthquakes happen along the edges of tectonic plates that slowly move and bump against each other deep underground. Earthquakes can cause massive damage and loss of life, such as the 1556 Shaanxi earthquake in China that killed over 800,000 people. Modern solutions aim to better predict, withstand, and prepare for earthquakes to minimize harm.
The document discusses earthquakes, including their causes, measurement, effects, and preparedness. Earthquakes occur due to the sudden release of built-up stress along fault lines in the earth's crust, causing seismic waves. Their magnitude is measured using scales like the Richter scale or moment magnitude scale. Earthquakes can damage infrastructure and the environment through ground shaking and secondary events like tsunamis or landslides. While earthquakes cannot be prevented, preparation through emergency planning and building design can reduce risks.
Earthquakes, landslides, volcanic eruptions and other disturbances can cause tsunamis by displacing large amounts of water. Tsunamis are a series of long sea waves that can travel across entire oceans within hours. Three-quarters of tsunamis occur in the Pacific Ocean due to high seismic activity along subduction zones that make up the Pacific Ring of Fire. When tsunamis reach land, they can devastate coastal areas by destroying homes and infrastructure and endangering human life. On average, two tsunamis occur globally each year, with about 80% originating in the Pacific Ocean.
1) Earthquakes are caused by the sudden release of energy from movement along geological faults in the earth's crust, generating seismic waves.
2) Larger earthquakes can trigger tsunamis if located offshore by displacing seabed, as well as landslides and volcanic eruptions.
3) Earthquake shaking causes loss of life and property destruction from building collapse and landslides burying infrastructure.
This presentation is for my Geography 110 class. Just an FYI if you are curious, the second to last slide that is captioned "Problems?" is about Red Tides
The document summarizes key aspects of Earth's internal structure, surface features, tectonic plates, earthquakes, volcanoes, and landforms. The Earth has a solid crust on top of a thick mantle and liquid outer and solid inner cores. Over 70% of the surface is ocean, covering underwater volcanoes, mountains and trenches. The remaining 30% includes various landforms like forests and deserts. Tectonic plates float on the mantle and interact, causing earthquakes and forming volcanoes and mountains. Earthquakes generate seismic waves and tsunamis. Volcanoes form at plate boundaries and erupt molten magma from the crust. Important landforms include mountains, valleys, plains and coastal features.
1) Tectonic plates slowly move across the Earth's surface over the course of a year, occasionally crashing into each other. When they crash, it can cause natural disasters like volcanic eruptions and earthquakes.
2) Volcanoes form as magma cools and piles up from cracks in the Earth's crust caused by the movement of tectonic plates and resulting earthquakes.
3) Tectonic plate collisions, though slow, continually form new landforms like mountains and volcanoes as the plates interact within the limited space available.
The Pacific Ring of Fire is a horseshoe shaped area surrounding the Pacific Ocean that experiences significant seismic and volcanic activity due to tectonic plate movement. Major plate boundaries like the subduction of the Pacific plate cause volcanoes and earthquakes that have impacted billions and cost billions. The Ring of Fire is responsible for events like the 1991 Mt. Pinatubo eruption and the 2011 Japan earthquake and tsunami that killed over 10,000 people annually and cost billions.
Earthquakes and faults (Grade 8 Lesson) Riya Duran
This document describes a learning competency on faults. It defines a fault as a break in the Earth's crust where movement has occurred. When plates move apart, it can result in earthquakes and faults. The objectives are to define fault, describe the consequences of diverging plates, and draw a fault. Activities include defining key terms, watching a video, and doing a hands-on modeling activity to simulate how a fault forms when plates pull apart.
1. The document discusses earthquakes and faults, explaining that the Philippines is prone to earthquakes due to its location along the Ring of Fire.
2. It defines a fault as a break in the earth's crust where significant movement has occurred, and explains how faults produce earthquakes through the buildup and sudden release of energy from inside the earth.
3. The document provides information on earthquake waves, intensity scales, and safety tips for both indoors and outdoors during and after an earthquake.
An earthquake is a sudden, rapid shaking of the Earth caused by the breaking and shifting of rock beneath the Earth's surface, which creates seismic waves. There are two main types of seismic waves: P-waves and S-waves. Earthquakes are caused by the buildup and sudden release of stress in the Earth's crust, which generates vibrations that travel through the Earth's interior and surface as seismic waves. Major earthquakes can cause significant damage through shaking, ground ruptures, landslides, fires, tsunamis, and floods.
The document discusses plate tectonics and volcanoes. It explains that plates move in three ways - converging towards each other, diverging away from each other, or sliding past each other. Volcanoes form at plate boundaries, especially at convergent boundaries where one plate subducts beneath another. This causes melting and upwelling of magma, resulting in volcanism. The Ring of Fire in the Pacific is an example of concentrated volcanism along plate boundaries.
1) Earthquakes are caused by the sudden release of energy stored along fault lines in the earth's crust due to the movement of tectonic plates.
2) The Philippines experiences over five earthquakes per day on average, with about 16 felt each year, including a magnitude 7.7 quake in 1990 that badly damaged areas in northern Luzon.
3) Major earthquakes are measured using scales like the Modified Mercalli Intensity Scale or Richter Magnitude Scale, which quantify the shaking intensity and energy released.
An earthquake occurred in Christchurch, New Zealand on Saturday morning, causing buildings to crumble but no deaths. In contrast, a similar earthquake in Haiti the previous year resulted in over 230,000 deaths due to the weaker construction of buildings there. The document provides safety tips for earthquakes, advising people to take shelter under sturdy furniture and protect their heads until the shaking stops.
1. An earthquake occurs when built-up tension along fault lines in the Earth's crust is suddenly released, causing the ground to shake.
2. The effects of an earthquake depend on several factors, including its magnitude on the Richter scale, distance from the epicenter, and the level of development in the affected area.
3. The 1995 Kobe earthquake in Japan caused over 30,000 injuries, left over 300,000 homeless as buildings collapsed, and led to long-term economic and social impacts as the city was rebuilt.
WHAT IS AN EARTHQUAKE?
Where Do Earthquakes Happen?
Why Do Earthquakes Happen?
How Are Earthquakes Studied?
How To Locate The Earthquake's Epicenter?
SCALES FOR EARTHQUAKE MEASUREMENT
What Are Earthquake Hazards?
Earthquakes occur due to forces within the Earth's structure. The planet's crust is broken into tectonic plates that float on the mantle, sometimes getting stuck and building pressure at the seams. When plates suddenly slip past each other, it causes the ground to shake and structures to fall. Most quakes happen along areas in the Pacific Ocean called the Ring of Fire. Beyond initial shaking, earthquakes can lead to dangerous secondary events like tsunamis, fires, and landslides that claim thousands of lives annually.
The document discusses earthquakes and how they occur. It explains that earthquakes are caused by sudden movement along faults in the Earth's crust due to a build up of stress. There are three main types of faults - normal, reverse, and strike-slip - each forming in a different way due to tension or compression in the crust. When friction along a fault is overcome, the fault will slip and move, causing seismic waves that produce shaking during an earthquake. The intensity of shaking and damage decreases further from the earthquake's epicenter.
What is earthquakes? What is the Elastic Rebound Theory?
Seismographs record earthquake events. Where Do Earthquakes Occur and How Often? What are the Destructive Effects of Earthquakes? How are the Size and Strength of an Earthquake Measured? Can Earthquakes be Predicted? Can Earthquakes be Controlled?
Ground shaking during earthquakes can cause significant damage depending on factors like magnitude, distance from epicenter, and duration of shaking. Strong shaking can collapse buildings, especially those constructed poorly or on weak foundations. Areas with thick unconsolidated sediments are susceptible to liquefaction, where shaking causes soils to lose strength and behave like liquid. This can damage structures and cause ground failures like lateral spreading. Mapping of soil types, groundwater levels, and historical liquefaction helps identify hazard zones to inform construction practices.
An earthquake is caused by the movement of tectonic plates deep underground. As the plates squeeze and stretch, stress builds until the rocks break, releasing energy in waves that cause the shaking felt during earthquakes. Common effects of earthquakes include damaged or destroyed buildings and homes, cracks in the ground, and potential tsunamis. While scientists are working to predict earthquakes, they currently cannot determine exactly how or when one will stop once the shaking has begun.
I do not have enough context to answer those specific questions. The document provided discusses different types of earthquake hazards and their effects, but does not mention fault types in the Philippines or bringing cookies to class.
The document discusses earthquakes, including what causes them, the Richter scale for measuring their strength, and safety tips. It notes that earthquakes occur when tectonic plates suddenly slip, releasing energy in the form of shock waves. The Richter scale is used to describe the magnitude of earthquakes on a logarithmic scale. Larger numbers indicate stronger quakes that can cause greater damage to structures. The document advises that during an earthquake, one should drop, cover, and hold on to protect oneself.
The document discusses the K-T extinction event that occurred 65 million years ago at the end of the Cretaceous period. Walter Alvarez first discovered evidence of an asteroid impact in the form of iridium in the geologic layers from that time. The asteroid struck what is now the Chicxulub crater in the Yucatan Peninsula. This catastrophic impact had massive environmental effects, causing an impact winter and the extinction of 75% of land species and 90% of marine species, including non-avian dinosaurs. While an asteroid impact caused global climate change, volcanism may have also contributed to the conditions that drove the mass extinction.
1) The document discusses the connection between continental drift and plate tectonics, explaining that continental drift occurred as the single early continent of Pangea broke apart due to movements of tectonic plates.
2) NASA studies how continental drift may affect the future positioning of continents hundreds of millions of years from now.
3) Evidence for possible life on other planets includes extremophiles on Earth that thrive in extreme conditions, evidence that interstellar dust contains organic compounds and microbes, and indications that the Jupiter moons Europa and Callisto may harbor subsurface oceans.
The document discusses plate tectonics and how it shapes the Earth's surface. It explains that plate tectonics involves several large plates and smaller plates that make up the Earth's outer shell. These plates are constantly and very slowly moving in relation to each other, either pulling apart, crashing together, or sliding past one another. The movement of these plates through processes like rifting, earthquakes, and volcanic activity is what creates and alters the Earth's landforms and features over long periods of time.
The Pacific Ring of Fire is a horseshoe shaped area surrounding the Pacific Ocean that experiences significant seismic and volcanic activity due to tectonic plate movement. Major plate boundaries like the subduction of the Pacific plate cause volcanoes and earthquakes that have impacted billions and cost billions. The Ring of Fire is responsible for events like the 1991 Mt. Pinatubo eruption and the 2011 Japan earthquake and tsunami that killed over 10,000 people annually and cost billions.
Earthquakes and faults (Grade 8 Lesson) Riya Duran
This document describes a learning competency on faults. It defines a fault as a break in the Earth's crust where movement has occurred. When plates move apart, it can result in earthquakes and faults. The objectives are to define fault, describe the consequences of diverging plates, and draw a fault. Activities include defining key terms, watching a video, and doing a hands-on modeling activity to simulate how a fault forms when plates pull apart.
1. The document discusses earthquakes and faults, explaining that the Philippines is prone to earthquakes due to its location along the Ring of Fire.
2. It defines a fault as a break in the earth's crust where significant movement has occurred, and explains how faults produce earthquakes through the buildup and sudden release of energy from inside the earth.
3. The document provides information on earthquake waves, intensity scales, and safety tips for both indoors and outdoors during and after an earthquake.
An earthquake is a sudden, rapid shaking of the Earth caused by the breaking and shifting of rock beneath the Earth's surface, which creates seismic waves. There are two main types of seismic waves: P-waves and S-waves. Earthquakes are caused by the buildup and sudden release of stress in the Earth's crust, which generates vibrations that travel through the Earth's interior and surface as seismic waves. Major earthquakes can cause significant damage through shaking, ground ruptures, landslides, fires, tsunamis, and floods.
The document discusses plate tectonics and volcanoes. It explains that plates move in three ways - converging towards each other, diverging away from each other, or sliding past each other. Volcanoes form at plate boundaries, especially at convergent boundaries where one plate subducts beneath another. This causes melting and upwelling of magma, resulting in volcanism. The Ring of Fire in the Pacific is an example of concentrated volcanism along plate boundaries.
1) Earthquakes are caused by the sudden release of energy stored along fault lines in the earth's crust due to the movement of tectonic plates.
2) The Philippines experiences over five earthquakes per day on average, with about 16 felt each year, including a magnitude 7.7 quake in 1990 that badly damaged areas in northern Luzon.
3) Major earthquakes are measured using scales like the Modified Mercalli Intensity Scale or Richter Magnitude Scale, which quantify the shaking intensity and energy released.
An earthquake occurred in Christchurch, New Zealand on Saturday morning, causing buildings to crumble but no deaths. In contrast, a similar earthquake in Haiti the previous year resulted in over 230,000 deaths due to the weaker construction of buildings there. The document provides safety tips for earthquakes, advising people to take shelter under sturdy furniture and protect their heads until the shaking stops.
1. An earthquake occurs when built-up tension along fault lines in the Earth's crust is suddenly released, causing the ground to shake.
2. The effects of an earthquake depend on several factors, including its magnitude on the Richter scale, distance from the epicenter, and the level of development in the affected area.
3. The 1995 Kobe earthquake in Japan caused over 30,000 injuries, left over 300,000 homeless as buildings collapsed, and led to long-term economic and social impacts as the city was rebuilt.
WHAT IS AN EARTHQUAKE?
Where Do Earthquakes Happen?
Why Do Earthquakes Happen?
How Are Earthquakes Studied?
How To Locate The Earthquake's Epicenter?
SCALES FOR EARTHQUAKE MEASUREMENT
What Are Earthquake Hazards?
Earthquakes occur due to forces within the Earth's structure. The planet's crust is broken into tectonic plates that float on the mantle, sometimes getting stuck and building pressure at the seams. When plates suddenly slip past each other, it causes the ground to shake and structures to fall. Most quakes happen along areas in the Pacific Ocean called the Ring of Fire. Beyond initial shaking, earthquakes can lead to dangerous secondary events like tsunamis, fires, and landslides that claim thousands of lives annually.
The document discusses earthquakes and how they occur. It explains that earthquakes are caused by sudden movement along faults in the Earth's crust due to a build up of stress. There are three main types of faults - normal, reverse, and strike-slip - each forming in a different way due to tension or compression in the crust. When friction along a fault is overcome, the fault will slip and move, causing seismic waves that produce shaking during an earthquake. The intensity of shaking and damage decreases further from the earthquake's epicenter.
What is earthquakes? What is the Elastic Rebound Theory?
Seismographs record earthquake events. Where Do Earthquakes Occur and How Often? What are the Destructive Effects of Earthquakes? How are the Size and Strength of an Earthquake Measured? Can Earthquakes be Predicted? Can Earthquakes be Controlled?
Ground shaking during earthquakes can cause significant damage depending on factors like magnitude, distance from epicenter, and duration of shaking. Strong shaking can collapse buildings, especially those constructed poorly or on weak foundations. Areas with thick unconsolidated sediments are susceptible to liquefaction, where shaking causes soils to lose strength and behave like liquid. This can damage structures and cause ground failures like lateral spreading. Mapping of soil types, groundwater levels, and historical liquefaction helps identify hazard zones to inform construction practices.
An earthquake is caused by the movement of tectonic plates deep underground. As the plates squeeze and stretch, stress builds until the rocks break, releasing energy in waves that cause the shaking felt during earthquakes. Common effects of earthquakes include damaged or destroyed buildings and homes, cracks in the ground, and potential tsunamis. While scientists are working to predict earthquakes, they currently cannot determine exactly how or when one will stop once the shaking has begun.
I do not have enough context to answer those specific questions. The document provided discusses different types of earthquake hazards and their effects, but does not mention fault types in the Philippines or bringing cookies to class.
The document discusses earthquakes, including what causes them, the Richter scale for measuring their strength, and safety tips. It notes that earthquakes occur when tectonic plates suddenly slip, releasing energy in the form of shock waves. The Richter scale is used to describe the magnitude of earthquakes on a logarithmic scale. Larger numbers indicate stronger quakes that can cause greater damage to structures. The document advises that during an earthquake, one should drop, cover, and hold on to protect oneself.
The document discusses the K-T extinction event that occurred 65 million years ago at the end of the Cretaceous period. Walter Alvarez first discovered evidence of an asteroid impact in the form of iridium in the geologic layers from that time. The asteroid struck what is now the Chicxulub crater in the Yucatan Peninsula. This catastrophic impact had massive environmental effects, causing an impact winter and the extinction of 75% of land species and 90% of marine species, including non-avian dinosaurs. While an asteroid impact caused global climate change, volcanism may have also contributed to the conditions that drove the mass extinction.
1) The document discusses the connection between continental drift and plate tectonics, explaining that continental drift occurred as the single early continent of Pangea broke apart due to movements of tectonic plates.
2) NASA studies how continental drift may affect the future positioning of continents hundreds of millions of years from now.
3) Evidence for possible life on other planets includes extremophiles on Earth that thrive in extreme conditions, evidence that interstellar dust contains organic compounds and microbes, and indications that the Jupiter moons Europa and Callisto may harbor subsurface oceans.
The document discusses plate tectonics and how it shapes the Earth's surface. It explains that plate tectonics involves several large plates and smaller plates that make up the Earth's outer shell. These plates are constantly and very slowly moving in relation to each other, either pulling apart, crashing together, or sliding past one another. The movement of these plates through processes like rifting, earthquakes, and volcanic activity is what creates and alters the Earth's landforms and features over long periods of time.
This document presents a theory for the extinction of dinosaurs that involves significant changes to the Earth's structure and rotation. It suggests that around 65 million years ago, 3/4 of the Earth's continental crust broke off and coalesced into the Moon, causing a shift in the Earth's axis that introduced seasons. This event would have drastically altered gravity on Earth and made conditions inhospitable for the large dinosaur species. Evidence is presented that calculations of the mass of the Moon and missing continental crust support this theory. It aims to provide a more complex explanation than other popular theories like an asteroid impact.
This document discusses the possibility of extraterrestrial life. It defines extraterrestrial life as any life existing outside of Earth and notes that while its existence is hypothetical, scientists search for planets that could support life. Key requirements for life include water, temperature, gravity and chemicals. The document explores potential places in our solar system that could support life, like Mars, Europa and Titan. It also discusses extremophiles, microorganisms, and evidence found by probes that water may exist below Mars' surface, though life has not yet been confirmed on other planets.
This document discusses three types of tectonic plate boundaries: divergent boundaries where plates move apart and new crust is formed, convergent boundaries where plates collide and subduct or cause mountain building, and transform boundaries where plates slide past each other along transform faults. It also provides science trivia about the moon and its formation, features, and exploration by astronauts. Finally, it lists nine superstitious beliefs from different cultures around the world about the causes of solar and lunar eclipses.
The document discusses plate tectonics and how it shapes Earth. Plate tectonics involves large plates in Earth's lithosphere that slowly move over time. When plates meet, they form boundaries which can result in volcanoes and earthquakes. Convection currents in the mantle drive the plate movements. Plates diverge at mid-ocean ridges, where new crust is formed, and converge in some places, causing volcanoes or mountains to form.
The document summarizes Earth's geologic history condensed into one calendar year. Key events include:
- By March, oceans formed but no life existed on the barren planet.
- First life emerged in April in the form of single-celled organisms near ocean vents.
- By December, more complex sea creatures evolved and the first plants colonized land despite heavy rains.
- On December 31st, early humans appeared in the last hour of the year along with Neanderthals and cave drawings. Modern civilizations emerged in the final minutes.
This document provides an overview of plate tectonics and its history. It discusses how the theory of plate tectonics emerged in the 1960s and revolutionized earth sciences by explaining phenomena like earthquakes and mountain building. It also summarizes early ideas around continental drift proposed by scientists like Alfred Wegener in the early 20th century, and how plate tectonics unified and built upon these early concepts.
This document provides information about plate tectonics and the development of the theory. It begins with a brief history of the theory and mentions key figures like Alfred Wegener who first proposed continental drift. It then provides details on the structure of the Earth and what constitutes a tectonic plate. The summary focuses on the key aspects and progression of the theory.
This document provides information about plate tectonics and the development of the theory. It begins with a brief history of the theory and mentions key figures like Alfred Wegener who first proposed continental drift. It then provides details on the structure of the Earth and what constitutes a tectonic plate. It explains how plates move and interact at their boundaries, which influences geological processes.
This document summarizes how various global systems affect Earth's climates. It discusses how latitude, with the equator receiving more solar heating than higher latitudes, affects climate. It also explains how land and sea distributions impact climate through differing heat capacities. Ocean currents are described as influencing climate by transporting heat around the globe. Relief, or elevation changes, are noted to impact climate by altering temperature and precipitation patterns.
introduction of plate tectonics leading to finding the epicenter.
Divergent plate boundary is alsoincluded in the ppt. Search the activity sheet on this topic also uploaded here
The document provides information over 12 days about changing Earth and plate tectonics. Day 1 introduces the four layers of the Earth - crust, mantle, outer core and inner core. Day 2 reviews the layers and their characteristics. Day 3 discusses Alfred Wegener's theory of continental drift and how plate tectonics explains the movement of continents. It also introduces the concept of Pangaea. Day 4 identifies the three types of plate boundaries - divergent, convergent and transform. Later days discuss earthquakes, volcanoes, and how volcanic activity forms new land and islands.
The document provides an overview of relief and water on Earth. It discusses the structure of the Earth and how tectonic plate movements have shaped the continents over hundreds of millions of years. It also describes the main types of continental and oceanic relief that have been formed through internal forces like earthquakes and volcanoes, as well as external forces like erosion. Finally, it examines the distribution of water on Earth, including the characteristics and movements of oceans, seas, and continental freshwater sources.
This document provides an overview of world regions and geography. It discusses how geography influences cultures and economies. Regions are defined and classified in various ways, including formally by shared attributes and functionally by economic organization. Forces like globalization are increasing interconnectivity between regions. The document examines topics like population trends, economic development, social issues, the environment, and political structures at regional and global scales. Regional geography combines physical and human perspectives to holistically study territories and the relationships between communities worldwide.
The giant ancient forest you cannot see coyote crossingLisa Schmidt
The document describes the creosote bushes that dominate the Mojave desert as an "ancient forest" that is invisible to many. It notes that individual creosote bushes can be thousands of years old, with some estimated at over 11,000 years old. Though unremarkable in appearance, these creosote bushes represent a vast ancient landscape that is increasingly threatened by development and habitat destruction. The author argues this ancient desert ecosystem deserves more appreciation and protection.
The document discusses the benefits of exercise for mental health. Regular physical activity can help reduce anxiety and depression and improve mood and cognitive functioning. Exercise causes chemical changes in the brain that may help boost feelings of calmness, happiness and focus.
This document provides an overview of the Physical Geography 101 course. It outlines that students will learn about the basic elements of geography including climate, landforms, water, soils, and plants and animals. It lists required textbooks and materials. The course objectives are to help students understand physical geography concepts like maps and the four environmental spheres of atmosphere, hydrosphere, lithosphere and biosphere. The document details assignments like exams, quizzes, maps and a presentation. Academic policies around attendance, cheating and cell phones are also addressed.
This document provides information for a geography lab course. It outlines the instructor and contact details, prerequisites, required textbooks and materials, student learning outcomes, course expectations and structure, grading policies, and the course schedule. The lab will focus on physical geography topics and provide hands-on experience investigating earth systems. Students will complete weekly lab assignments using worksheets and online submissions.
This document provides the syllabus for a Cultural Geography course taught online in Spring 2016. The 3-credit course is instructed by Lisa Schmidt and uses the textbook "Human Geography" by Knox. Assignments include weekly postings, maps quizzes, chapter quizzes, exams, and a semester-long project. The course aims to examine human activities and cultures around the world through geographical concepts and analysis of populations, development, economies, and social differences. Grades are calculated based on completion of these assignments throughout the semester.
This document provides information for an online physical geography course taught by Professor Lisa Schmidt. It outlines the course details, including required textbooks, assignments, grading criteria, and contact information for the professor. Students will study the four environmental spheres of Earth - the atmosphere, lithosphere, hydrosphere, and biosphere - and their interactions. Weekly readings, discussions, and quizzes will cover these topics. The course aims to give students a foundational understanding of physical geography concepts and patterns around the world.
The document discusses the benefits of exercise for mental health. Regular physical activity can help reduce anxiety and depression and improve mood and cognitive functioning. Exercise causes chemical changes in the brain that may help protect against mental illness and improve symptoms.
Will exxon have to pay for years of misleading the public bill moyersLisa Schmidt
The document discusses the benefits of exercise for mental health. Regular physical activity can help reduce anxiety and depression and improve mood and cognitive functioning. Exercise causes chemical changes in the brain that may help protect against mental illness and improve symptoms.
Periodic table's 7th row completed with discovery of four new elements ifl ...Lisa Schmidt
The 7th row of the periodic table has been completed with the discovery of four new elements by scientists from Russia, the U.S., and Japan. The elements occupy positions 113, 115, 117, and 118 and were previously known as Uut, Uup, Uus, and Uuo respectively. The discoveries were ratified by IUPAC, allowing the elements to be formally named. The Japanese team that discovered element 113 will name it, with reports suggesting it may be called "Japanium". Completing the 7th row was an important achievement for chemistry as the periodic table is now filled down to that row.
Tools used in geography include maps, globes, GPS, remote sensing, and GIS. Maps show physical features and are printed on paper, while globes model the spherical earth accurately. GPS uses satellite distances to determine position. Remote sensing studies objects from afar using tools like aerial photography. GIS digitally analyzes and displays geographic data, allowing overlay of different data layers.
2. Serendipity 3
Caesars
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Read more at: http://www.foodnetwork.com/restaurants/nv/las-vegas/serendipity-3-
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3. Plate Tectonics
1. What is it?
It is a layer of the earth crust on which most
people refer to as “terra Fermi”, but it a great deal
more. Everything we know mineral, water, living
thing, even our atmosphere has or is affected by it in
some way for all time every since earth was created.
Your book defines plate tectonics – as a coherent
theory of massive lithospheric rearrangement based
on the movement of continent – sized plates.
4. This is a cutaway of the Earth as we think it is.
You see no one has every really gone to the center
of the Earth. But this is what everyone thinks it is.
5. This is another cutaway getting us to where we need to
be.
See that upper left corner that says “Lithosphere” well that
is the layer we are going to be talking about here. Welcome
to “Plate Tectonics 101” The short version.
6. 1. Earth is made up of several layers. The outermost layer is called Earth's
crust. The thickness of the crust varies. Under the oceans , the crust is only
about 3–5 mi (5–10 km) thick. This is at the bottom of those trenches.
2. Under the continents, however, the crust thickens to about 22 mi (35 km)
and reaches depths of up to 37 mi (60 km) under some mountain ranges. 3.
Beneath the crust is a layer of rock material that is also solid, rigid, and
relatively cool, but is assumed to be made up of denser material.
3. This layer is called the upper part of the upper mantle, and varies in depth
from about 31–62 mi (50–100 km) below Earth's surface. The combination
of the crust and this upper part of the upper mantle, which are both
comprised of relatively cool and rigid rock material, is called the
lithosphere. This section is thought to be brittle.
7. 2. Where is it happening?
A. First this is a World Wide situation. Everyone is
affected whether you think you are or not.
B. It is happening in your backyard and as well your
front yard.
C. You cannot see it unless you look at mountain or go look at San Andres
Fault. These plates move all the time 24/7/365. It is when they don’t we
worry.
D. But it is possibly it will be on the news or you have been woke in the
middle of the night when your house and bed moved, or you saw on
the news and saw that a bridge collapsed on a highway or river
somewhere.
E. Maybe you heard about Haiti?
8. Alfred Wegener was a German meteorologist and geophysicist who
developed the first theory of continental drift and formulated the idea that a
supercontinent known as Pangaea existed on the Earth millions of years ago.
His ideas were largely ignored at the time they were developed but today
they are very well accepted by most of the scientific community.
9. Plate Tectonics Today Still Working
• Remember the top layer
of the cake with the whip
cream and cherry on top
and 1st layer of cake. Well
that whole 1st layer
moved on the Earth
“Lithosphere” and has
been moving every since.
The speed it moves is
about the speed your
finger nail grows each
year.
11. 3. How does it affect life on Earth? Or how is life on
Earth affected by it?
If there was no sun, there would be no life on earth!
If there was no lithosphere the earth would not be
like it is, and we would have
No diversity of life!
We have found that certain animals lived in the same
place at one time and the bones where found thousands
of miles away in another land. That how the theory of
plate tectonics started. When the land and earth changes
something new pops up that we had not seen before.
12. You recognize this?
Yes! So let us go deeper. I chose this picture for the
landscape for your bearing. Don’t be shocked at the
next picture.
13. Yes! This is a dead planet with no water.
But hey it is only a picture. Let us go deeper. You are
looking at the continental plate of Africa and it is
floating! Yes! Even without water.
14. This is the giant mechanism that scientist think moves the
plates or build a new crust. Notice the “Ridge in the Center,”
that would be like the Atlantic Ridge.
15. The Mid-Atlantic Ridge, which splits nearly the entire Atlantic
Ocean north to south, is probably the best-known and most-
studied example of a divergent-plate boundary. (Illustration
adapted from the map This Dynamic Planet.)
16. The speed at which new ocean floor is created varies from one
location on the ocean ridge to another. Between North America
and Europe, the rate is about 2.2 inches (3.6 cm) per year. At the
East Pacific rise, which is pushing a plate into the west coast of
South America, the rate is 12.6 inches (32.2 cm) per year.
17. The Divergent is the middle example is what may have started the whole separation of
the major continental plates. It runs down the middle of the Atlantic and moves
outward on either side. Closer to it is new while farther out is the older stuff.
18. Map showing the Mid-Atlantic Ridge splitting Iceland and separating
the North American and Eurasian Plates. The map also shows
Reykjavik, the capital of Iceland, the Thingvellir area, and the locations
of some of Iceland's active volcanoes (red triangles), including Krafla.
19. Scientists now have a fairly good understanding of how the plates
move and how such movements relate to earthquake activity. Most
movement occurs along narrow zones between plates where the
results of plate-tectonic forces are most evident. Volcanoes like this
zone also, as well as earthquakes.
There are four types of plate boundaries:
1. Divergent boundaries -- where new crust is generated as the plates
pull away from each other.
2. Convergent boundaries -- where crust is destroyed as one plate
dives under another. Some of the plates will soon disappear.
3. Transform boundaries -- where crust is neither produced nor
destroyed as the plates slide horizontally past each other. That's us.
4. Plate boundary zones -- broad belts in which boundaries are not well
defined and the effects of plate interaction are unclear.
20. Transform boundaries neither create nor consume crust. Rather, two plates move
against each other, building up tension, then releasing the tension in a sudden and
often violent jerk. This sudden jerk creates an earthquake.
The San Andreas Fault is undoubtedly the most famous transform boundary in the
world. To the west of the fault is the Pacific plate, which is moving northwest. To the
east is the North American Plate, which is moving southeast.
Los Angeles, located on the Pacific plate, is now 340 miles south of San Francisco,
located on the North American plate. In 16 million years, the plates will have moved so
much that Los Angeles will be north of San Francisco!
21. 4. Is there some problem or issue with your topic?
Even with all the accumulated knowledge of science and I take all that study
some part of what makes up earth we still have little knowledge per say over
the vast mechanical mechanism that make it work. We have theories that are
still being battled over since 1929. A simple example: We are in deep
decisions and arguments on what “Fraking.” What are the long term effects?
It may be profitable, but is it worth it? What else is being affected? If we
knew everything about the lithosphere why do we spend so much money and
time studying it? The Atlantic, and the California coast, and Yellowstone just
to mention a few. We just don’t know all the facts and do not have enough
people and equipment to deal with something “World Size.” Even with
satellites up their daily gathering facts in some cases you have to have feet on
the ground to tell you what really is happening or to go over the data
collected.
Note: We dig holes it every day looking for oil, coal, gas, diamond, you name it.
These may be worthless in the future or gone. Water may be the new “Gold” in the
future trapped below the surface. New environments have been found under the ice
shelves‘ by the university of Nebraska recently. So who knows?
22. 5. What are some solutions?
We just need more people in the field so many different fields out there to get a grip on all
that is happening. Not just only in Geology, Geography. Physics, Chemistry, Electronics, or just
read the list Professor Schmidt gave you pick a field, they are in desperate need of people.
I will give you two examples of why
Example 1. We know that we humans are producing carbon dioxide at an alarming rate and the
reason we know that is because we can measure what we do and know where it came from, but
if you look at the other big contributor “volcanoes” we really don’t know. Why is that? Well there
are 155 active volcanoes worldwide and recently the testing on them has gotten us to 35 to find
out mother nature may be increasing her rate of contribution to the atmosphere on a bigger
scale than we thought the figures in the past years have jump from 200 ppm, to 400 ppm and
then 600 ppm, and the last figures on saw are closer to 900 ppm. So if you wanted to really sell
the world on that we are shooting ourselves in the foot to make profit and then we need more
help and technical information.
Example 2. On April 29th 2015 5,600 square miles of Nepal dropped 3 to 5 feet all at once. Of
course that included a famous mountain we talk about a lot it is or was 29, 312 feet high and
nobody is going to change that, but it dropped 5 feet. Sentinel-1a radar, which passed over
the affected areas and scanned the differences. There are sensors all over that area, but most on
manual and someone has to go collect the information and is it still where it was and can we get
to it? No one knows and it may take years to collect as emergency teams and everyone else is
trying to deal with loss of life and many other things. Also National Geographic (you got to bless
that group) they were up on Mt. Everest when it happened. One statement said when it happen
Mt. Everest Roared!
Nepal Earthquake Triggers Avalanche at Mount Everest Base Camp
An avalanche triggered by a 7.8-magnitude earthquake in Nepal plowed through Mount Everest's
base camp Saturday killing at least 18 people and injuring dozens more.
23. Landsat 8 satellite observations were first obtained over Nepal after the earthquake on April 30. Landsat 8 acquired the first largely cloud-free
image of the Langtang Valley. This imagery helped show the true extent of the disaster that took place in Langtang Valley.
May 2, 2015 • [By: Tony Greicius, NASA JPL] The magnitude 7.8 Gorkha earthquake that struck Nepal on April 25, 2015, caused extensive
damage in Kathmandu Valley and severely affected Nepal’s rural areas. The Langtang Valley in the Rasuwa district was particularly hard hit, as
became apparent from pictures taken by a rescue helicopter mission on April 26. Numerous tourists and Nepali were, or are, still trapped in
the valley as access is completely blocked by avalanches and landslides. The valley’s main village, Langtang , was completelydestroyed by the
earthquake and the large, wet, debris- and ice-rich avalanche and likely pressure wave from dust avalanche that it triggered, resulting in an
unknown number of casualties. Other avalanches also struck elsewhere in the valley.
24. Note:
As a passage on Earth we are moving constantly even when resting!
Earth rotates at a speed of 1,040 mph, and we are not done yet. Earth
circles the Sun each year at a velocity of 66,600 mph. Also since the
Sun and our solar system is moving through space at 45,000 mph.*
Is the Earth under “Stress” Yes! Otherwise we would not have the
“bulge” at the equator from rotation of the Earth.
Remember I said the “lithosphere is Brittle!” What happens to brittle
things when put under stress? They break up.
Also for your information the reason you don’t notice it is that gravity
locks you in place and you have no reference of the movement
because everything else is moving at the same speed.
*This speed is in a frame of rest if the other stars were all standing still.
25. Is the “machine still working” Yes! This a new island that was
born about 620 miles from Japan on November 21, 2013.
26. So can we control it? NO!
Look at what has happen every time man has tried to control
Mother Nature.
Do we really understand it? Yes! and No!, because in science it
theory, proof then agreement and we are still arguing over it
since 1929. We are dealing with some new technical things that
we have no idea what the impact will be. I would like to know we
gave the next generation something to base the work and not
have it still in theory.
Can we track it? Yes!
Can we learn something more than we do now? Yes!
Can we get a warning system from the studies? Maybe?
Have we in some cases complicated the system? Yes! We need
a more unified front to educate the public. The public can force
companies and politicians to change their ways. Education of the
masses.
27. Note:
This is just the tip of what is going on daily around the world and unless it is in your
back yard you don’t pay attention to it. You’re the future and I’m not proud what my
generation has done. Some of us are getting back in the fight trying to change the
thinking, but it will be you that will have to make the difference. I have just giving you
a glimpse of what is happening and this class is showing you the effects that are
happening at an alarming rate. Plate Tectonics is a massive element that even now
new theories are being put forth from NASA scientist that completely turn everything
around. In either case it will still keep happening and time is not our side. We work in
years and the system works in millenniums at a steady pace with immovable objects
meeting ever relenting force. We are destroying the environment and go on doing our
everyday thing saying is it won’t happen to me. Really! Give it time, which I said was
against us.
This part has been about layers and the different layers of jobs and position in this
field is really open. THINK ABOUT IT!
I THANK YOU FOR YOUR TIME ON THIS . SORRY ABOUT THE SOAP BOX!
28. Work Cited
Document from Print Source Published Electronically
"Structure of the Interior of Earth." Earth's Interior. N.p., n.d. Web. 15 July
2015.
http://www.windows2universe.org/earth/Interior_Structure/interior.html
"This Dynamic Earth--Contents [USGS]." This Dynamic Earth--Contents [USGS].
N.p., n.d. Web. 15 July 2015.
http://pubs.usgs.gov/gip/dynamic/dynamic.html
"The Geological Society." The Geological Society. N.p., n.d. Web. 15 July 2015.
http://www.geolsoc.org.uk/Plate-Tectonics/
"Continents in Collision: Pangea Ultima." - NASA Science. N.p., n.d. Web. 15
July 2015.
http://science.nasa.gov/science-news/science-at-nasa/2000/ast06oct_1/
National Association of Geoscience Teachers (NAGT): Plate Tectonic
Movement
http://serc.carleton.edu/NAGTWorkshops/geophysics/visualizations/PTMove
ments.html