Lecture 9: Volcanic Hazards
|
|
- Erika Boone
- 7 years ago
- Views:
Transcription
1 Lecture 9: Volcanic Hazards Key Questions 1. What are the dominant primary volcanic hazards? 2. What is the difference between a pyroclastic flow and an ash fall? 3. If Mt. Baker discharged an ash plume, where would it likely drift to and fallout? 4. What volcanic gases are most hazardous to humans and animals? 5. Why is CO 2 dangerous? 6. What is most at risk to lava flows? 7. What are some ways to lower the risk? 8. What is VEI? 9. What is VPI (see In Harms Way Geotimes link)?
2 Volcanic Hazards Mt Pinatubo in the Philippines, June 1991
3 Tectonic Setting determines Magma Composition determines Eruptive Style determines Hazard Type
4 Stratovolcano andesite basalt steep sided layered (pyroclastic material) mainly andesite explosive convergent zones
5 h high lithostatic pressure
6 eruption expansion cause ground deformation heat h expansion causes earthquakes lower lithostatic pressure drop in pressure causes gases to develop gas pressure builds up and explodes!
7 Volcanic Hazards Air-Fall Tephra (ash fall) Lava Flows Pyroclastic Flows (ash flow) Volcanic Gases Landslides Lahars Tsunamis
8 Ash Fall Gardner et al., Potential Volcanic Hazards from Future Activity of Mount Baker, Washington, Open-File Report
9 Plinian Style Hawaiian Style Kilauea Mount St.Helens
10 Volcano Explosivity Index (VEI)
11 Volcano Explosivity Index (VEI) VEI PLUME HEIGHT VOLUME CLASSIFICATION (See Eruption Types) EXAMPLE 0 <100 m 1000s m3 Hawaiian Kilauea m 10,000s m3 Hawaiian/Strombolian Stromboli km 1,000,000s m3 Strombolian/Vulcanian Galeras (1992) km 10,000,000 m3 Vulcanian Ruiz (1985) km 100,000,000s m3 Vulcanian/Plinian Galunggung (1982) 5 >25 km 1 km3 Plinian St. Helens (1980) 6 >25 km 10s km3 Plinian/Ultra-Plinian Krakatau (1883) 7 >25 km 100s km3 Ultra-Plinian Tambora (1815) 8 >25 km 1000s km3 Ultra-Plinian Toba (74 ka)
12 SIZE (cubic km) EXAMPLE FREQUENCY Kilauea, Unzen several months Etna 5 years St. Helens (1980) 10 years 1-10 Pinatubo 100 years Krakatau (1883), Katmai (1912) 1000 years Tambora (1815) 10,000 years >1000 Yellowstone, Toba 100,000 years
13 Ash Hazards Dangerous to aircraft Cause structural damage (heavy!) Can destroy crops Volcanic ash consists of tiny jagged pieces of rock and glass that is hard, abrasive. Can contaminate water and soil May pollute the atmosphere
14 Mt. St. Helens: Ash Discharge
15 Graph showing mean diamater of ash particles with increasing distance from Mount St. Helens volcano. Mt. St. Helens: Ash Discharge
16 Mt. St. Helens: After May 18, 1980
17
18 Copyrighted photo courtesy of Douglas Miller Ephrata, Washington, on the morning of May 18, km (145 mi) east of Mount St. Helens.
19 Gardner et al., Potential Volcanic Hazards from Future Activity of Mount Baker, Washington, Open-File Report
20 Gardner et al., Potential Volcanic Hazards from Future Activity of Mount Baker, Washington, Open-File Report
21
22 Ash Plume Ash Fall Mt. Pinatubo, Philippines, June 1991 Clark Air Force Base
23 A densely settled area of about 2,000 square kilometers was blanketed by 10 to 25 centimeters of rain-soaked tephra; 189 people were killed by collapsing buildings, and damage to utilities and agricultural lands was extensive. Paladio-Melosantos et al., Tephra Falls of the 1991 Eruptions of Mount Pinatubo
24 Erosional dissection of an ash deposit at Pinatubo volcano
25 Ash particles may absorb these aerosol acid droplets onto their surfaces and contaminate water and soils.
26 Scientists measured a drop in the average global temperature of about 1 o F (0.6 o C) after 15 months.
27 Ash is dangerous for aircraft glass shards can damage and stall engines
28 Volcanic ash particles abrade windows, clog fuel systems, and accumulate in and clog jet engines with molten glass.
29
30 Eyjafjallajökull = island mountain glacier Eyjafjallajökull volcano
31
32
33
34
35 The International Air Transport Association (IATA) said that at its height, the "crisis" hit almost a third of global flights. It estimated that 1.2 million passengers a day were affected, and global airlines have lost about $1.7billion in revenue.
36 Ash is dangerous for aircraft Remote Sensing Image
37 Remote Sensing Data from the Eyjafjallajökull volcano
38 Lava Flows Cause property damage, but rarely kill people. Travel meters per hour to meters per day depending upon the viscosity and topography. Pahoehoe Basaltic Lava: Kalanpana, Hawaii
39 Aa Basaltic Lava: Iceland
40 Hydrocooling: Iceland
41 Aa Basaltic Lava: Iceland
42 Iceland
43 Mount Etna in Sicily
44 Kilauea, Hawaii
45 Mount Etna in Sicily
46 Pyroclastic Flows or Ash Flows Mayon volcano in the Philippines on September 12, 1984 Pyroclastic flows are mixtures of hot gas and rock that travel gravitationally down the flanks of a volcano at high velocities (up to 100 km/hr)
47 Mayon volcano in the Philippines on September 23, 1984
48 Pyroclastic Flow Mt. Unzen, Japan, June 1991
49 Unzen volcano in southern Japan June 23, 1993
50 Augustine volcano in Alaska on March 30, 1986
51 Soufrière Hills volcano on Montserrat June 25, 1997
52 Mt. Pelee: 29,000 people killed by a pyroclastic flow in Port-au-Prince, Haiti Photograph of the remains of St. Pierre, Martinique (by Heilprin, 1902).
53 Volcanic Gases
54 Volcanic Gases Doug Nathe collecting gases from a fumarole on the floor of Sherman Crater, Aug. 22, Gas samples have been sent off to USGS, Menlo Park, for analysis. Photo by D. Tucker
55 Volcanic Gases Sherman Crater Mt Baker
56 Examples of volcanic gas compositions, in volume percent concentrations (from Symonds et. al., 1994) Volcano Tectonic Style Temperature Kilauea Summit Hot Spot 1170 C Erta` Ale Divergent Plate 1130 C Momotombo Convergent Plate 820 C H C S H CO H 2 S HCl HF Most Dangerous
57 Carbon Dioxide (CO 2 ) Discharge Lake Nyos, Cameroon West Africa, 1986
58
59 Carbon Dioxide (CO2) Discharge Lake Nyos, Cameroon West Africa, 1986 Killed 1700 people and 3000 cattle
60 Ash particles may absorb these aerosol acid droplets onto their surfaces and contaminate water and soils.
61 Volcanic Landslides Iriga volcano in the Philippines was produced by a massive landslide during the Holocene.
62 Alaska's Augustine volcano
63 Mt. St. Helens: Just Prior to Eruption This is Harry Glicken who was killed during the eruption of Mt. Utzen, Japan, June However, the geologist occupying this observation site was killed during the May 1980 eruption of Mt St. Helens.
64 Mt. St. Helens: Volcanic Landslide
65 Mt. St. Helens: Volcanic Landslide
66 Mt. St. Helens: Volcanic Landslide
67 Mount Shasta The hummocky landslide deposit was emplaced between 380,000 and 300,000 years ago. Photograph by S.R. Brantley on July 3, 1994
68 VPI Index
69
Viscosity and Volcano Types
20 LESSON Viscosity and Volcano Types This photo, taken in 1943 in Paricutin, Mexico, shows an eruption of the Paricutin volcano at night. Glowing hot, broken rocks outline the shape of the volcano, called
More informationCATACLYSMIC ERUPTIONS
CATACLYSMIC ERUPTIONS The really big ones! This figure compares the size of some recent, well-known eruptions. Note how small the eruptions of Mount St. Helens and even Vesuvius are compared to Katmai,
More informationVolcanic Hazards & Prediction of Volcanic Eruptions
Page 1 of 11 EENS 3050 Tulane University Natural Disasters Prof. Stephen A. Nelson Volcanic Hazards & Prediction of Volcanic Eruptions This page last updated on 03-Jul-2012 Volcanic Hazards This lecture
More informationRapid Changes in Earth s Surface
TEKS investigate rapid changes in Earth s surface such as volcanic eruptions, earthquakes, and landslides Rapid Changes in Earth s Surface Constant Changes Earth s surface is constantly changing. Wind,
More informationFOURTH GRADE VOLCANOES 1 WEEK LESSON PLANS AND ACTIVITIES
FOURTH GRADE VOLCANOES 1 WEEK LESSON PLANS AND ACTIVITIES PLATE TECTONIC CYCLE OVERVIEW OF FOURTH GRADE VOLCANOES WEEK 1. PRE: Comparing different structures of volcanoes. LAB: Modeling three types of
More informationChapter 5: Magma And Volcanoes
Chapter 5: Magma And Volcanoes Introduction: Earth s Internal Thermal Engine Magma is molten rock beneath Earth s surface. Because liquid magma is less dense than surrounding solid rock, and obviously
More informationINTRODUCTION. This project is about volcanoes and how they form and how they function. It will also show you the different aspects of a volcano.
BY RYAN O MAHONY INTRODUCTION This project is about volcanoes and how they form and how they function. It will also show you the different aspects of a volcano. MAP OF VOLCANOES AROUND THE WORLD DIAGRAM
More informationFIRST GRADE VOLCANOES 1 WEEK LESSON PLANS AND ACTIVITIES
FIRST GRADE VOLCANOES 1 WEEK LESSON PLANS AND ACTIVITIES PLATE TECTONIC CYCLE OVERVIEW OF FIRST GRADE VOLCANOES WEEK 1. PRE: Learning the shapes of volcanoes. LAB: Experimenting with "lava." POST: Comparing
More informationAnalysis and Classification of Volcanic Eruptions
Analysis and Classification of Volcanic Eruptions Prof. S. C. Wirasinghe, PEng (APEGA) Ms. H. Jithamala Caldera I 3 R 2 May 2014 Purdue University Department of Civil Engineering, Schulich School of Engineering
More informationNATURAL AND HUMAN INDUCED HAZARDS Vol. I - Environmental Impacts of Volcanic Eruptions - V.Yu. Kirianov ENVIRONMENTAL IMPACTS OF VOLCANIC ERUPTIONS
ENVIRONMENTAL IMPACTS OF VOLCANIC ERUPTIONS V.Yu. Kirianov Institute of Volcanic Geology and Geochemistry RAS, Petropavlovsk-Kamchatsky, Russia Keywords: volcanic eruptions, climate, glaciation, volcanic
More informationMAJOR LANDFORMS IN VOLCANIC REGIONS
MAJOR LANDFORMS IN VOLCANIC REGIONS Volcanism is not randomly distributed over the world. It is concentrated near plate boundaries where plate subduction or seafloor spreading takes place. Other occurrences
More informationInside Earth Chapter 3
Name Hour Due Date Inside Earth Chapter Page 1 Volcanoes and Plate Tectonics Page 2 Volcanic Activity Page - Mapping Earthquakes and Volcanoes Page 4 Mapping Earthquakes and Volcanoes table Page 5 - Mapping
More informationVolcanoes. Talking About Disaster: Guide for Standard Messages. Volcanoes-1. March 2007
Volcanoes Learn about your community s risk from hazards created by volcanic eruptions. While you may be located far from a volcano, the ash from an explosive eruption could affect your area. Contact your
More informationRegents Questions: Plate Tectonics
Earth Science Regents Questions: Plate Tectonics Name: Date: Period: August 2013 Due Date: 17 Compared to the oceanic crust, the continental crust is (1) less dense and more basaltic (3) more dense and
More informationII. Earth Science (Geology) Section (9/18/2013)
EAPS 100 Planet Earth Lecture Topics Brief Outlines II. Earth Science (Geology) Section (9/18/2013) 1. Interior of the Earth Learning objectives: Understand the structure of the Earth s interior crust,
More informationVolcanism and Volcanoes
Volcanism and Volcanoes Volcanism is one of the most impressive displays of Earth s dynamic internal processes. From a human perspective, volcanism can be a destructive force causing property damage, injuries,
More informationVOLCANIC ERUPTION. Definition of Hazard
VOLCANIC ERUPTION Definition of Hazard A volcano is a vent in the earth's crust through which molten rock (magma), rock fragments, gases, and ashes are ejected from the earth's interior. A volcano is created
More informationWhen Things Go Wrong
When Things Go Wrong When Things Go Wrong Our planet has many wondrous things. We plant a tiny sapling and it becomes a mighty tree. Water runs in rivers. Rainbows appear in the sky. But it is not always
More informationBetween June and November, 1989, I had an opportunity to work at Nagasaki
MOUNT UNZEN: AN ACTIVE VOLCANO OF SOUTHWESTERN JAPAN WHICH WAS VISITED BY GURUDEV RABINDRA NATH TAGORE IN MAY 1924 Arun Kumar Mount Unzen (32.75degrees N, 130.30 degrees E) is an active group of stratovolcanoes
More informationTectonic plates have different boundaries.
KEY CONCEPT Plates move apart. BEFORE, you learned The continents join and break apart The sea floor provides evidence that tectonic plates move The theory of plate tectonics helps explain how the plates
More informationGeol 101: Physical Geology PAST EXAM QUESTIONS LECTURE 4: PLATE TECTONICS II
Geol 101: Physical Geology PAST EXAM QUESTIONS LECTURE 4: PLATE TECTONICS II 4. Which of the following statements about paleomagnetism at spreading ridges is FALSE? A. there is a clear pattern of paleomagnetic
More informationModeling Volcanic Eruptions
Modeling Volcanic Eruptions New Mexico Adventures in Supercomputing Challenge Final Report April 6, 2005 Team 052 Rio Rancho Mid-High School Team Members John Bell Nick Vigil Teacher Sponsor Debra Loftin
More informationVOLCANOES AND OTHER IGNEOUS FEATURES
VOLCANOES AND OTHER IGNEOUS FEATURES INSTRUSVE IGNEOUS FEATURES Plutonic-Intrusive igneous rocks can cool and solidify into large rock bodies: plutons Plutons form in all sizes several square meters to
More informationDISTRIBUTION OF ACTIVE VOLCANOES
DISTRIBUTION OF ACTIVE VOLCANOES The earth is a dynamic planet. Its rigid outer surface layer is broken into several tectonic plates which are in constant motion relative to one another. As demonstrated
More informationLearn more at www.pbs.org/nature
Lesson Title: Vibrant Volcanoes Grade level: 2 4 Topic/Subject Matter: Earth Science Time Allotment:1-2 class periods Overview This lesson will introduce elementary students to the fiery and explosive
More informationCHAPTER 6 THE TERRESTRIAL PLANETS
CHAPTER 6 THE TERRESTRIAL PLANETS MULTIPLE CHOICE 1. Which of the following is NOT one of the four stages in the development of a terrestrial planet? 2. That Earth, evidence that Earth differentiated.
More informationPlate Tectonics. Earth, 9 th edition Chapter 2
1 Plate Tectonics Earth, 9 th edition Chapter 2 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 Plate Tectonics: summary in haiku form Alfred Wegener gave us Continental Drift. Fifty years later... Continental Drift
More informationPlate Tectonics Chapter 2
Plate Tectonics Chapter 2 Does not include complete lecture notes. Continental drift: An idea before its time Alfred Wegener First proposed his continental drift hypothesis in 1915 Published The Origin
More informationGCSE GEOGARPHY OCR B REVISION GUIDE Natural Hazards
GCSE GEOGARPHY OCR B REVISION GUIDE Natural Hazards Tectonic Hazards A natural hazard is an extreme natural event or process that causes loss of life and/or extreme damage to property and creates severe
More informationWEATHERING, EROSION, AND DEPOSITION PRACTICE TEST. Which graph best shows the relative stream velocities across the stream from A to B?
NAME DATE WEATHERING, EROSION, AND DEPOSITION PRACTICE TEST 1. The diagram below shows a meandering stream. Measurements of stream velocity were taken along straight line AB. Which graph best shows the
More informationKilauea: Hawaii. Kilauea Facts. Kilauea. Kilauea as hazard. Tsunamis
Kilauea: Hawaii Kilauea is the worldʼs most active volcano. It is an exciting volcano to study because it is part of a massive chain of powerful volcanoes that makes up the Hawaiian chain. Kilauea Facts
More informationInteractive Plate Tectonics
Interactive Plate Tectonics Directions: Go to the following website and complete the questions below. http://www.learner.org/interactives/dynamicearth/index.html How do scientists learn about the interior
More informationSome Processes that Change the Earth s Surface
PART ONE Some Processes that Change the Earth s Surface Science standards To prepare students to understand the Essential Academic Learning Requirements (EALRs) introduced at middle school, this series
More information4. Plate Tectonics II (p. 46-67)
4. Plate Tectonics II (p. 46-67) Seafloor Spreading In the early 1960s, samples of basaltic ocean crust were dredged up from various locations across the ocean basins. The samples were then analyzed to
More informationVolcano Under the City
Volcano Under the City Program Overview NOVA investigates the dangers of Nyiragongo volcano, located in a densely populated valley in the heart of Africa. The program: recounts Nyiragongo s 2002 eruption,
More informationLaboratory 6: Topographic Maps
Name: Laboratory 6: Topographic Maps Part 1: Construct a topographic map of the Egyptian Pyramid of Khafre A topographic map is a two-dimensional representation of a three-dimensional space. Topographic
More information1. The diagram below shows a cross section of sedimentary rock layers.
1. The diagram below shows a cross section of sedimentary rock layers. Which statement about the deposition of the sediments best explains why these layers have the curved shape shown? 1) Sediments were
More informationVolcanoes Erupt Grade 6
TEACHING LEARNING COLLABORATIVE (TLC) EARTH SCIENCE Volcanoes Erupt Grade 6 Created by: Debra McKey (Mountain Vista Middle School); Valerie Duncan (Upper Lake Middle School); and Lynn Chick (Coyote Valley
More informationExploring Our World with GIS Lesson Plans Engage
Exploring Our World with GIS Lesson Plans Engage Title: Exploring Our Nation 20 minutes *Have students complete group work prior to going to the computer lab. 2.List of themes 3. Computer lab 4. Student
More informationGeorgia Performance Standards Framework for Science Grade 6. Unit Organizer: Geology: Inside the Earth (Approximate Time: 7 Weeks)
The following instructional plan is part of a GaDOE collection of Unit Frameworks, Performance Tasks, examples of Student Work, and Teacher Commentary. Many more GaDOE approved instructional plans are
More informationHot Spots & Plate Tectonics
Hot Spots & Plate Tectonics Activity I: Hawaiian Islands Procedures: Use the map and the following information to determine the rate of motion of the Pacific Plate over the Hawaiian hot spot. The volcano
More informationPLATE TECTONICS EXERCISE (Modified from North Seattle Community College online exercise)
PLATE TECTONICS EXERCISE (Modified from North Seattle Community College online exercise) Introduction: As discussed in our textbook, the speed at which tectonic plates move has been calculated in several
More informationThe Dynamic Crust 2) EVIDENCE FOR CRUSTAL MOVEMENT
The Dynamic Crust 1) Virtually everything you need to know about the interior of the earth can be found on page 10 of your reference tables. Take the time to become familiar with page 10 and everything
More informationTransform Boundaries
Lecture 7 Plates and Mantle Plumes Transform Boundaries Transform boundaries occur where one segment of rigid lithosphere slides horizontally past another in response to stresses in the lithosphere. The
More informationVolcano Hazards. In this unit, you will
Unit 4 Volcano Hazards In this unit, you will Examine records of historical volcanoes. Use the Volcanic Explosivity Index (VEI) to categorize volcanoes. Investigate the effects of major eruptions on climate.
More informationUnit 6 Earthquakes and Volcanoes
Unit 6 Earthquakes and Volcanoes Earthquakes and Volcanoes: Essential Questions What evidence can students observe that the Earth is changing? How do scientists know what s inside the Earth? What processes
More informationSECOND GRADE VOLCANOES 1 WEEK LESSON PLANS AND ACTIVITIES
SECOND GRADE VOLCANOES 1 WEEK LESSON PLANS AND ACTIVITIES PLATE TECTONIC CYCLE OVERVIEW OF SECOND GRADE VOLCANOES WEEK 1. PRE: Investigating the parts of a volcano. LAB: Comparing the parts of a volcano
More informationLava Flows. Most lava flows are basaltic in composition. Basalt 90% Andesite 8% Dacite/Rhyolite 2%
Lava Flows Most lava flows are basaltic in composition Basalt 90% Andesite 8% Dacite/Rhyolite 2% This is because most silicic and intermediate magmas erupt explosively (higher gas content and viscocity)
More informationTECTONICS ASSESSMENT
Tectonics Assessment / 1 TECTONICS ASSESSMENT 1. Movement along plate boundaries produces A. tides. B. fronts. C. hurricanes. D. earthquakes. 2. Which of the following is TRUE about the movement of continents?
More informationFOURTH GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES
FOURTH GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES PLATE TECTONIC CYCLE OVERVIEW OF FOURTH GRADE VOLCANOES WEEK 1. PRE: Comparing different structures of volcanoes. LAB: Modeling three types
More informationLesson 13: Plate Tectonics I
Standards Addressed Lesson 13: Plate Tectonics I Overview Lesson 13 introduces students to geological oceanography by presenting the basic structure of the Earth and the properties of Earth s primary layers.
More informationNatural Disasters & Assessing Hazards and Risk. Natural Hazards and Natural Disasters
Page 1 of 9 EENS 3050 Tulane University Natural Disasters Prof. Stephen A. Nelson Natural Disasters & Assessing Hazards and Risk This page last updated on 19-Aug-2014 Natural Hazards and Natural Disasters
More informationCalifornia Standards Grades 9 12 Boardworks 2009 Science Contents Standards Mapping
California Standards Grades 912 Boardworks 2009 Science Contents Standards Mapping Earth Sciences Earth s Place in the Universe 1. Astronomy and planetary exploration reveal the solar system s structure,
More information1 Exploring Earth s Interior
1 Exploring Earth s Interior Crust Mantle Outer Core Crust-to-Mantle Inner Core Cross Section From Surface to Center SCIENCE EXPLORER Focus on Earth Science Prentice-Hall, Inc. 2 Evidence for Continental
More informationSECOND GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES
SECOND GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES PLATE TECTONIC CYCLE OVERVIEW OF SECOND GRADE VOLCANOES WEEK 1. PRE: Investigating the parts of a volcano. LAB: Comparing the parts of a
More informationCONFIRMATION AND CALIBRATION OF COMPUTER MODELING OF TSUNAMIS PRODUCED BY AUGUSTINE VOLCANO, ALASKA
CONFIRMATION AND CALIBRATION OF COMPUTER MODELING OF TSUNAMIS PRODUCED BY AUGUSTINE VOLCANO, ALASKA James E. Beget Geophysical Institute and Alaska Volcano Observatory University of Alaska, Fairbanks,
More informationEarth Materials: Intro to rocks & Igneous rocks. The three major categories of rocks Fig 3.1 Understanding Earth
Earth Materials: 1 The three major categories of rocks Fig 3.1 Understanding Earth 2 Intro to rocks & Igneous rocks Three main categories of rocks: Igneous Sedimentary Metamorphic The most common minerals
More informationWeathering, Erosion, and Soils. Weathering and Erosion. Weathering and Erosion
Weathering, Erosion, and Soils 1 The Grand Canyon, a landscape shaped by weathering and erosion 2 Weathering vs. erosion Types of weathering Physical Chemical Rates of weathering and erosion Climate Rock
More information1. Michigan Geological History Presentation (Michigan Natural Resources)
1. Michigan Geological History Presentation (Michigan Natural Resources) The Michigan Geological History Presentation provides an overview of the approximately 3 billion years of Earth Processes that the
More informationGlacier-clad volcanoes
Glaciers in an Environmental Context Natural hazards in glacierized regions: Glacier-clad volcanoes Contribution by Demian Schneider Eyjafjallajökull, Iceland, April 2010 Overview 1. Distribution of
More informationChapter 8: Plate Tectonics -- Multi-format Test
Name: Class: Date: ID: A Chapter 8: Plate Tectonics -- Multi-format Test Modified True/False Indicate whether the statement is true or false. If false, change the identified word or phrase to make the
More informationKINDERGARTEN PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES
KINDERGARTEN PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES PLATE TECTONIC CYCLE OVERVIEW OF KINDERGARTEN VOLCANOES WEEK 1. PRE: Learning that all mountains are not volcanoes. LAB: Investigating rocks
More informationAlfred Wegener s Theory of Continental Drift Became Modern Plate Tectonics. Wegener in Greenland about 1912. He froze to death there in 1930.
Alfred Wegener s Theory of Continental Drift Became Modern Plate Tectonics Wegener in Greenland about 1912. He froze to death there in 1930. Science is self correcting. The Scientific Method The history
More informationIntroduction and Origin of the Earth
Page 1 of 5 EENS 1110 Tulane University Physical Geology Prof. Stephen A. Nelson Introduction and Origin of the Earth This page last updated on 30-Jul-2015 Geology, What is it? Geology is the study of
More informationContinental Drift. Alfred Wegener (1880-1930) Proposed that all of the continents were once part of a large supercontinent - Pangaea Based on:
Plate Tectonics and Continental Drift Continental Drift Alfred Wegener (1880-1930) Proposed that all of the continents were once part of a large supercontinent - Pangaea Based on: Similarities in shorelines
More informationEarth Egg Model Teacher Notes
Ancient Greeks tried to explain earthquakes and volcanic activity by saying that a massive bull lay underground and the land shook when it became angry. Modern theories rely on an understanding of what
More informationSIXTH GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES
SIXTH GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES PLATE TECTONIC CYCLE OVERVIEW OF SIXTH GRADE VOLCANOES WEEK 1. PRE: Comparing the structure of different types of volcanoes. LAB: Plotting
More informationFIRST GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES
FIRST GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES PLATE TECTONIC CYCLE OVERVIEW OF FIRST GRADE VOLCANOES WEEK 1. PRE: Learning the shapes of volcanoes. LAB: Experimenting with "lava." POST:
More informationIMPLICATIONS OF TEPHRA (VOLCANIC ASH) FALL- OUT ON THE OPERATIONAL SAFETY OF THE SENDAI NUCLEAR POWER PLANT
GREENPEACE COMMISSIONED REPORT February 26th 2015 IMPLICATIONS OF TEPHRA (VOLCANIC ASH) FALL- OUT ON THE OPERATIONAL SAFETY OF THE SENDAI NUCLEAR POWER PLANT Greenpeace Written by: John H Large Large &
More informationDYNAMIC CRUST: Unit 4 Exam Plate Tectonics and Earthquakes
DYNAMIC CRUST: Unit 4 Exam Plate Tectonics and Earthquakes NAME: BLOCK: DATE: 1. Base your answer to the following question on The block diagram below shows the boundary between two tectonic plates. Which
More informationPlate Tectonics. Introduction. Boundaries between crustal plates
Plate Tectonics KEY WORDS: continental drift, seafloor spreading, plate tectonics, mid ocean ridge (MOR) system, spreading center, rise, divergent plate boundary, subduction zone, convergent plate boundary,
More informationIgneous Geochemistry. What is magma? What is polymerization? Average compositions (% by weight) and liquidus temperatures of different magmas
1 Igneous Geochemistry What is magma phases, compositions, properties Major igneous processes Making magma how and where Major-element variations Classification using a whole-rock analysis Fractional crystallization
More informationTectonic plates push together at convergent boundaries.
KEY CONCEPT Plates converge or scrape past each other. BEFORE, you learned Plates move apart at divergent boundaries In the oceans, divergent boundaries mark where the sea floor spreads apart On land,
More informationFourth Grade Geology: The Earth and Its Changes Assessment
Fourth Grade Geology: The Earth and Its Changes Assessment 1a. What is the center layer of the Earth called? a. crust b. core c. mantle d. middle 1b. Label each layer of the Earth. 1c. What are the Earth
More informationThe Earth, Sun, and Moon
reflect The Sun and Moon are Earth s constant companions. We bask in the Sun s heat and light. It provides Earth s energy, and life could not exist without it. We rely on the Moon to light dark nights.
More informationFACTS ABOUT CLIMATE CHANGE
FACTS ABOUT CLIMATE CHANGE 1. What is climate change? Climate change is a long-term shift in the climate of a specific location, region or planet. The shift is measured by changes in features associated
More informationHow Did These Ocean Features and Continental Margins Form?
298 10.14 INVESTIGATION How Did These Ocean Features and Continental Margins Form? The terrain below contains various features on the seafloor, as well as parts of three continents. Some general observations
More informationUnit Plan: Plate Tectonics Shannon B. Carpenter TE 804 1/25/02
Unit Plan: Plate Tectonics Shannon B. Carpenter TE 804 1/25/02 This unit plan is intended to cover about seven weeks and would be appropriate for a middle school general science class or an introductory
More informationGeol 101: Physical Geology Summer 2007 EXAM 1
Geol 101: Physical Geology Summer 2007 EXAM 1 Write your name out in full on the scantron form and fill in the corresponding ovals to spell out your name. Also fill in your student ID number in the space
More informationEarth Science Landforms, Weathering, and Erosion Reading Comprehension. Landforms, Weathering, and Erosion
Reading Comprehension Name 1 How many people have been to the Rocky Mountains or the Grand Canyon? When people go to visit these natural wonders, they may not realize that it took millions of years for
More informationViscosity experiments: physical controls and implications for volcanic hazards. Ben Edwards Dept of Geology, Dickinson College
Viscosity experiments: physical controls and implications for volcanic hazards Student Name: Ben Edwards Dept of Geology, Dickinson College OBJECTIVES OF LAB Learn about the rheological property called
More informationSoda Bottle Volcano An Eruption Begins
Soda Bottle Volcano An Eruption Begins Overview: Examine how gases provide the energy to create explosive volcanic eruptions by making comparisons to gases in a soda bottle and by conducting a carefully
More informationPlate Tectonics. Hi, I am Zed and I am going to take you on a trip learning about Plate Tectonics. And I am Buddy Zed s mascot
Plate Tectonics Hi, I am Zed and I am going to take you on a trip learning about Plate Tectonics And I am Buddy Zed s mascot Continental Drift Alfred Wegener proposed that continents were not always where
More informationChapter Overview. Bathymetry. Measuring Bathymetry. Echo Sounding Record. Measuring Bathymetry. CHAPTER 3 Marine Provinces
Chapter Overview CHAPTER 3 Marine Provinces The study of bathymetry charts ocean depths and ocean floor topography. Echo sounding and satellites are efficient bathymetric tools. Most ocean floor features
More informationThe hazards - and benefits - of volcanic eruptions on oceanic islands. Kathy Cashman University of Oregon
The hazards - and benefits - of volcanic eruptions on oceanic islands Kathy Cashman University of Oregon Ash Lava Volcanic eruptions I. Eruption styles/hazards - Explosive eruptions Magmatic Phreatomagmatic
More information6.E.2.2 Plate Tectonics, Earthquakes and Volcanoes
Name: Date: 1. The road shown below was suddenly broken by a natural event. 3. The convergence of two continental plates would produce Which natural event most likely caused the crack in the road? island
More informationPlate Tectonics Web-Quest
Plate Tectonics Web-Quest Part I: Earth s Structure. Use the following link to find these answers: http://www.learner.org/interactives/dynamicearth/structure.html 1. Label the layers of Earth in the diagram
More informationPlate Tectonics Visual Glossary and Atlas How to use this app in your classroom
Plate Tectonics Visual Glossary and Atlas How to use this app in your classroom In addition to providing a comprehensive list of terms, definitions, illustrations, and animations related to plate tectonics,
More information1. You are about to begin a unit on geology. Can anyone tell me what geology is? The study of the physical earth I.
PLATE TECTONICS ACTIVITY The purpose of this lab is to introduce the concept of plate tectonics and the formation of mountains. Students will discuss the properties of the earth s crust and plate tectonics.
More informationRide the Rock Cycle. Suggested Goals: Students will gain an understanding of how a rock can move through the different stages of the rock cycle.
Illinois State Museum Geology Online http://geologyonline.museum.state.il.us Ride the Rock Cycle Grade Level: 5 6 Purpose: To teach students that the rock cycle, like the water cycle, has various stages
More informationVolcanoes Around the Globe
Volcanoes Around the Globe Volcanoes fed by relatively silica-rich (SiO 2 -rich) magmas tend to explode while those fed by silica-poor magmas usually erupt gently. Where are the explosive volcanoes and
More informationA remote sensing instrument collects information about an object or phenomenon within the
Satellite Remote Sensing GE 4150- Natural Hazards Some slides taken from Ann Maclean: Introduction to Digital Image Processing Remote Sensing the art, science, and technology of obtaining reliable information
More informationVolcanism in Iceland Fig. 59
Volcanism in Iceland Iceland has a high concentration of active volcanoes due to its unique geological origin. There are about 130 mountains of volcanic origin, 18 of which have erupted since the colonization
More informationGLG 112: Geologic Disasters Syllabus 2012
Instructor Name School of Earth Sciences and Environmental Sustainability, Geology Program Office: Bldg X, Room X; Phone: 523- XXXX; Email: instructor e-mail Class Time (Blg 12, Rm 103) Instructor Office
More informationPlate Tectonics Lab Assignment
Plate Tectonics Lab Assignment After reading the introduction to the Plate Tectonics exercises in the lab manual, complete the questions on a hard copy of this Lab Assignment. When finished, transfer your
More informationContributors to report
1. The Global Volcano Model (GVM; http://globalvolcanomodel.org/) was launched in 2011 and has grown to include 31 partner institutes collaborating from across the globe representing scientists from disciplines
More informationSpecimen Paper. Chemistry 1F. Time allowed! 60 minutes
Centre Number Surname Candidate Number Specimen Paper For Examiner s Use Other Names Candidate Signature Examiner s Initials General Certificate of Secondary Education Foundation Tier Question 1 Mark Science
More informationSocial and Environmental Impacts of Landslides
Social and Environmental Impacts of Landslides Latsis Symposium 2007 Research Frontiers in Environment and Sustainability ETH-Zurich September 18, 2007 Dr. A. Keith Turner Emeritus Professor Geological
More informationGENERAL SCIENCE LABORATORY 1110L Lab Experiment 9B: Tracking the Hawaiian Islands: How Fast Does the Pacific Plate Move?
GENERAL SCIENCE LABORATORY 1110L Lab Experiment 9B: Tracking the Hawaiian Islands: How Fast Does the Pacific Plate Move? Background You know that the Earth s crustal plates are always moving, but how fast?
More informationCharacteristics of the. thermosphere
Characteristics of the Atmosphere. If you were lost in the desert, you could survive for a few days without food and water. But you wouldn't last more than five minutes without the ' Objectives Describe
More information