Stop that Sediment! Create a plan to help the people that work, live, and play by the Toutle River

Size: px
Start display at page:

Download "Stop that Sediment! Create a plan to help the people that work, live, and play by the Toutle River"

Transcription

1 Stop that Sediment! Create a plan to help the people that work, live, and play by the Toutle River

2 The 1980 eruption began with an enormous landslide.

3

4 As far as we know, this landslide was the largest landslide that was witnessed by people that lived to tell the tale. It removed an entire mountaintop! In just a few moments, Mount St. Helens changed From this: To this: Jim Nieland/USFS

5

6 How much rock was in the landslide? 4 BILLION Boxes this Big OR 1 MILLION Olympic-sized swimming pools Getty Images/ Lana Oatey Pixabay.com

7 The landslide ended up in the Toutle River Valley as big chunks of rock called hummocks.

8 This is what the hummocks look like today.

9 The hummocks are made of sediment. Sediment is a word for a piece of rock that has been moved from where it originally was, usually by water.

10 Sand is a type of sediment. Sediment can also be smaller or bigger (like the size of powdered sugar) (like pebbles, cobbles, and boulders).

11 After the landslide, not all of that sediment remained in the hummocks in the upper Toutle River Valley A few hours after the eruption, the sediment mixed with water and created a dangerous lahar (or volcanic mudflow) that ripped up buildings, trees, and bridges. USGS

12 The mudflows in the 1980 eruption were devastating. The mudflows ripped up bridges, trees, buildings, and other things in their path. & The mudflows buried things that were at the bottom of the valley.

13 Sediment went into the Columbia River and settled to the bottom, making the river shallower. Some ships were trapped until the river was dredged. Dredging is what people do to make rivers deeper. They use equipment to dig out or suck up sediment. Both of these are dredging boats U.S. Army Corps of Engineers Photo Archives Website

14 How much sediment was in the 1980 lahar? This is a million Olympic pools

15 How much sediment was in the 1980 lahar? This is a million Olympic pools This is about 10,000 Olympic pools

16 The 1980 mudflows were large and devastating, but there s still a lot of sediment in the hummocks.

17 You don t need a lahar to move sediment. You just need a river.

18 It happens much more slowly, but the Toutle River carries a surprisingly large amount of sediment. Each year, the Toutle River moves about 1/3 of the sediment that was moved by the 1980 lahar.

19 It might not seem like much when compared to the mountain and the sediment in the landslide, but It s enough to fill up about 3000 of these Olympic swimming pools! It s a LOT of sediment!

20 This huge amount of sediment may cause problems for the people that work, live, and play by the river for many years to come. If nothing is done to slow or stop the sediment, it could bury things, like the mudflow did. WE NEED YOUR HELP!

21 YOUR MISSION: Design a plan to minimize the effect of ongoing sedimentation in the Toutle River Valley for the next 50 years. This can include: Building a structure Using natural resources Using services (like digging or dredging) or or Army Corps of Engineers USGS or some combination of the three or an entirely different, creative idea!

22 Building a structure This is the Sediment Retention Structure (SRS). The SRS is a dam (a wall that goes across the whole valley). Army Corps of Engineers It has a place for water to escape, so pressure doesn t build and it doesn t burst open.?what other shapes could slow or stop sediment??how big should it be??what should it be made of??how many?

23 Using Natural Resources Buried logs can make a log jam The logs catch some of the sediment. do you think would happen to the way sediment moves if you planted trees or shrubs?

24 Using services (like digging or dredging) USGS Remember: dredging is digging up sediment to make a river channels deeper Cat.com?How often should I dig??where should I dredge or dig?

25 INSTRUCTIONS You will receive a list of supplies and services that you can use. This list is kind of like a Minecraft inventory. Each supply is priced per block. The supply list will tell you how many coins a block of each supply costs. You are on a budget! You may only spend 200 coins. Minecraft

26 downstream This is a view of the Toutle River valley from the side. This is called a crosssection. You will draw your design on this sheet. MOUNT ST. HELENS this way

27 Your worksheet will have a grid on it. Each square means 1 block on your supply list. Minecraft When you design your structure, count the number of blocks of each supply you use. Keep track of how many coins you spend on supplies and services. You can only spend 200 coins!

28 EXAMPLE supplies: 60 cement blocks 6 trees 25 small plants 2 large logs 3 big pipes 6 small pipes 19 chainlink fence =195 coins services: Dredge every 10 years =5 coins = 200

3 Erosion and Deposition by Ice

3 Erosion and Deposition by Ice CHAPTER 12 3 Erosion and Deposition by Ice SECTION Agents of Erosion and Deposition BEFORE YOU READ After you read this section, you should be able to answer these questions: What are glaciers? How do

More information

Beyond the Book. FOCUS Book

Beyond the Book. FOCUS Book FOCUS Book Suppose your city wants to build a new housing development on a steep slope outside town. Design a model to test whether the land is safe from the types of landslides you read about in this

More information

Changes over Time: Destructive Processes

Changes over Time: Destructive Processes 1 Name Date Changes over Time: Destructive Processes Earth s surface is always changing. Blowing wind and flowing water causes some changes. Moving rock deep inside Earth causes other changes. These processes

More information

Debris Avalanches. Debris avalanche deposits on a volcano in Chile. All of the area in the foreground is buried by a thick debris avalanche.

Debris Avalanches. Debris avalanche deposits on a volcano in Chile. All of the area in the foreground is buried by a thick debris avalanche. Debris Avalanches Volcanoes are not very stable structures. From time to time, they collapse producing large rock and ash avalanches that travel at high speeds down valleys. Collapse maybe caused by an

More information

Patterns of Recovery Outdoor Activity

Patterns of Recovery Outdoor Activity Mount St Helens National Volcanic Monument Teacher s Corner 2011 Gifford Pinchot National Forest USDA Forest Service Patterns of Recovery Outdoor Activity Time Commitment: Site: Location: 45 minutes to

More information

TEACHER BACKGROUND KNOWLEDGE. Surface Processes: Weathering and Erosion

TEACHER BACKGROUND KNOWLEDGE. Surface Processes: Weathering and Erosion TEACHER BACKGROUND KNOWLEDGE Surface Processes: Weathering and Erosion Core Concepts Precipitation (caused by the water cycle) and wind cause rocks to be broken into smaller pieces in the process called

More information

Earthquake Lab! Seismic Waves 1. What do scientists believe the Earth is made of?

Earthquake Lab! Seismic Waves 1. What do scientists believe the Earth is made of? Name: Earthquake Lab! Seismic Waves 1. What do scientists believe the Earth is made of? Period: 2. How do scientists make measurements of inside the Earth? 3. What are the two types of Earthquake waves?

More information

Ch. 8: Mass Movements, Wind and Glaciers

Ch. 8: Mass Movements, Wind and Glaciers Ch. 8: Mass Movements, Wind and Glaciers Every day the landscape around us undergoes changes. Changes that are powered by gravity alone are called mass movement or mass wasting. Mass movement includes

More information

Read Across America. Listen as I read for facts about Volcanoes. In the Shadow of the Volcano

Read Across America. Listen as I read for facts about Volcanoes. In the Shadow of the Volcano Read Across America Listen as I read for facts about Volcanoes. In the Shadow of the Volcano Constructive & Destructive Processes Earth s surface is always changing. Blowing wind and flowing water causes

More information

Weathering and Erosion

Weathering and Erosion Have you ever looked at the land around you and wondered how it was shaped? The geologic features that help define the world are still being shaped by the natural processes of weathering, erosion, and

More information

GOING WITH THE FLOW (1 Hour)

GOING WITH THE FLOW (1 Hour) GOING WITH THE FLOW (1 Hour) Addresses NGSS Level of Difficulty: 3 Grade Range: 3-5 OVERVIEW In this activity, students use a stream table to model the processes of erosion and streambed formation. The

More information

1 Earth s Oceans. TAKE A LOOK 2. Identify What are the five main oceans?

1 Earth s Oceans. TAKE A LOOK 2. Identify What are the five main oceans? CHAPTER 13 1 Earth s Oceans SECTION Exploring the Oceans BEFORE YOU READ After you read this section, you should be able to answer these questions: What affects the salinity of ocean water? What affects

More information

DO NOW HW due Friday 9/9!

DO NOW HW due Friday 9/9! DO NOW HW due Friday 9/9! 1. What are 6 characteristics used to identify a mineral? 2. What are the four things something must be in order to be considered a mineral? 3. What is luster? 4. If a mineral

More information

Hazards in the Seattle Area. Disaster Questions. Where Were You? Where Were You? Volcanoes St. Helens Adams, Rainier, Glacier, Baker

Hazards in the Seattle Area. Disaster Questions. Where Were You? Where Were You? Volcanoes St. Helens Adams, Rainier, Glacier, Baker Hazards in the Seattle Area Volcanoes St. Helens Adams, Rainier, Glacier, Baker Earthquakes Outer coast Puget Sound (Seattle Fault & others) Tsunami Outer coast Puget Sound (Seattle Fault & others) Disaster

More information

Constructive & Destructive Forces

Constructive & Destructive Forces Constructive & Destructive Forces Intro: Constructive Forces Processes that create landforms. Destructive Forces Processes that destroy landforms. Intro: Constructive Forces Volcanoes Deposition Landslides

More information

Volcanoes. Environmental Geology, Mr. Paul Lowrey Stacey Singleton, Cassandra Combs, Dwight Stephenson, Matt Smithyman

Volcanoes. Environmental Geology, Mr. Paul Lowrey Stacey Singleton, Cassandra Combs, Dwight Stephenson, Matt Smithyman Volcanoes Environmental Geology, Mr. Paul Lowrey Stacey Singleton, Cassandra Combs, Dwight Stephenson, Matt Smithyman EMPACTS Project, Spring 2017 Northwest Arkansas Community College, Bentonville, AR

More information

Non-fiction: Dig This! Want to know what the world was like millions of years ago? Look to the rocks.

Non-fiction: Dig This! Want to know what the world was like millions of years ago? Look to the rocks. Non-fiction: Dig This! Dig This! Fossil Find Want to know what the world was like millions of years ago? Look to the rocks. One hundred and fifty million years ago, one of the very first birds appeared

More information

Cattaraugus Creek: A Story of Flowing Water and the Geology of the Channel It Flows Through Presentation to West Valley Citizen Task Force 4/27/16

Cattaraugus Creek: A Story of Flowing Water and the Geology of the Channel It Flows Through Presentation to West Valley Citizen Task Force 4/27/16 Cattaraugus Creek: A Story of Flowing Water and the Geology of the Channel It Flows Through Presentation to West Valley Citizen Task Force 4/27/16 Raymond C. Vaughan, Ph.D. What happens if you drop a

More information

GEt Dirty SKE2 Students will describe the physical attributes of rocks and soils. Background information

GEt Dirty SKE2 Students will describe the physical attributes of rocks and soils. Background information Get Dirty This activity covers the following Georgia Performance Standards: SKE2 Students will describe the physical attributes of rocks and soils. a. Use senses to observe and group rocks by physical

More information

L.O: SLOWING STREAMS DEPOSIT (SORT) SEDIMENT HORIZONTALLY BY SIZE.

L.O: SLOWING STREAMS DEPOSIT (SORT) SEDIMENT HORIZONTALLY BY SIZE. L.O: SLOWING STREAMS DEPOSIT (SORT) SEDIMENT HORIZONTALLY BY SIZE. 1. Base your answer to the following question on the profile shown below, which shows the pattern of horizontal sorting produced at a

More information

Weathering, Erosion and Deposition

Weathering, Erosion and Deposition Weathering, Erosion and Deposition Shaping the Earth s Surface Weathering the process of breaking down rocks into smaller fragments Erosion the transport of rock fragments from one location to another

More information

Geomorphology Geology 450/750 Spring Fluvial Processes Project Analysis of Redwood Creek Field Data Due Wednesday, May 26

Geomorphology Geology 450/750 Spring Fluvial Processes Project Analysis of Redwood Creek Field Data Due Wednesday, May 26 Geomorphology Geology 450/750 Spring 2004 Fluvial Processes Project Analysis of Redwood Creek Field Data Due Wednesday, May 26 This exercise is intended to give you experience using field data you collected

More information

Mount St. Helens. Copyright 2010 LessonSnips

Mount St. Helens. Copyright 2010 LessonSnips Mount St. Helens Washington State is home to the Cascade Mountains, a range of mountains that extends from the Canadian province of British Columbia to northern California. Many of these mountains are

More information

Mass Wasting: The Work of Gravity

Mass Wasting: The Work of Gravity Chapter 15 Lecture Earth: An Introduction to Physical Geology Twelfth Edition Mass Wasting: The Work of Gravity Tarbuck and Lutgens Chapter 15 Mass Wasting The Importance of Mass Wasting Slopes are the

More information

Earth Science Review

Earth Science Review Earth Science Review Earth Science Categories Resources Earth Clues W-E-D 1 W-E-D 2 Misc. Grab Bag $100 $100 $100 $100 $100 $100 $200 $200 $200 $200 $200 $200 $300 $300 $300 $300 $300 $300 $400 $400 $400

More information

Changes to Land 5.7B. landforms: features on the surface of Earth such as mountains, hills, dunes, oceans and rivers

Changes to Land 5.7B. landforms: features on the surface of Earth such as mountains, hills, dunes, oceans and rivers All the landforms on Earth have changed over time and continue to change. Many of the changes were caused by wind, moving water, and moving ice. Mountains have grown and shrunk. Rivers have cut away land

More information

How does erosion happen?

How does erosion happen? How does erosion happen? By National Geographic, adapted by Newsela staff on 10.03.17 Word Count 682 Level 830L These rock formations, in Bryce Canyon National Park, Utah, are called hoodoos. Although

More information

Think about the landforms where you live. How do you think they have changed over time? How do you think they will change in the future?

Think about the landforms where you live. How do you think they have changed over time? How do you think they will change in the future? reflect All the landforms on Earth have changed over time and continue to change. Many of the changes were caused by wind, moving water, and moving ice. Mountains have grown and shrunk. Rivers have cut

More information

DeltaScience. Content Readers. Summary. Science Background. Objectives. Reading Comprehension Skills. Supporting English Learners

DeltaScience. Content Readers. Summary. Science Background. Objectives. Reading Comprehension Skills. Supporting English Learners DeltaScience Content Readers TM Objectives List four main types of landforms. Red Edition Grade 3 4 reading level Purple Edition Grade 4 5 reading level Explore ways that rocks are broken down into smaller

More information

Module/Unit: Landforms Grade Level: Fifth

Module/Unit: Landforms Grade Level: Fifth Module/Unit: Landforms Grade Level: Fifth PA Academic Standards for Science and Technology and Environment and Ecology: 3.1.7.B Describe the use of models as an application or scientific or technological

More information

What are two kinds of volcanic eruptions? How does the composition of magma affect eruptions? What are two ways that magma can erupt from a volcano?

What are two kinds of volcanic eruptions? How does the composition of magma affect eruptions? What are two ways that magma can erupt from a volcano? CHAPTER 9 1 Volcanic Eruptions SECTION Volcanoes BEFORE YOU READ After you read this section, you should be able to answer these questions: What are two kinds of volcanic eruptions? How does the composition

More information

Unit 2 Lesson 1 Geologic Change over Time. Copyright Houghton Mifflin Harcourt Publishing Company

Unit 2 Lesson 1 Geologic Change over Time. Copyright Houghton Mifflin Harcourt Publishing Company Been There, Done That What is the principle of uniformitarianism? The principle of uniformitarianism states that geologic processes that happened in the past can be explained by current geologic processes.

More information

4 th Grade Science Unit C: Earth Sciences Chapter 6: Minerals and Rocks Lesson 1: What are minerals?

4 th Grade Science Unit C: Earth Sciences Chapter 6: Minerals and Rocks Lesson 1: What are minerals? 4 th Grade Science Unit C: Earth Sciences Chapter 6: Minerals and Rocks Lesson 1: What are minerals? mineral A mineral is a natural, nonliving, solid crystal that makes up rocks. All over the world, each

More information

Mount St. Helens changed the way we look at things!

Mount St. Helens changed the way we look at things! Mount St. Helens, a turning point in studies of, and perceptions about explosive volcanoes Mount St. Helens changed the way we look at things! Plinian column during the cataclysmic eruption of May 18,

More information

The Norwood Science Center. Geology (Minerals) Grade 4

The Norwood Science Center. Geology (Minerals) Grade 4 The Norwood Science Center Geology (Minerals) Grade 4 Background Information: Where do rocks come from? At first you might think the answer to this question is simple. Igneous rock comes from either magma

More information

Learning Objectives: I can identify and interpret river flows and directions.

Learning Objectives: I can identify and interpret river flows and directions. Learning Objectives: I can identify and interpret river flows and directions. Bellringer Review: Check for Understanding Questions: 1 2 What Are The Key Parts Of A River s Anatomy? In your data notebooks

More information

Debris flow: categories, characteristics, hazard assessment, mitigation measures. Hariklia D. SKILODIMOU, George D. BATHRELLOS

Debris flow: categories, characteristics, hazard assessment, mitigation measures. Hariklia D. SKILODIMOU, George D. BATHRELLOS Debris flow: categories, characteristics, hazard assessment, mitigation measures Hariklia D. SKILODIMOU, George D. BATHRELLOS Natural hazards: physical phenomena, active in geological time capable of producing

More information

Natural Disasters. Why Are There Earthquakes? 197 words. The Power of the Earth 221 words. Big Waves! 188 words

Natural Disasters. Why Are There Earthquakes? 197 words. The Power of the Earth 221 words. Big Waves! 188 words ARTICLE-A-DAY Natural Disasters 6 Articles Check articles you have read: Why Are There Earthquakes? 197 words The Power of the Earth 221 words Big Waves! 188 words The Volcano That Keeps Erupting 228 words

More information

Student Packet session # 11 Name: Date:

Student Packet session # 11 Name: Date: Student Packet session # 11 Name: Date: Student Exploration: Building Pangaea Big Idea 6: Earth Structures Benchmark: SC.7.E.6.4 Explain and give examples of how physical evidence supports scientific theories

More information

Tales of the Past. Source: Sci-ber Text with the Utah State Office of Education

Tales of the Past. Source: Sci-ber Text with the Utah State Office of Education Tales of the Past Source: Sci-ber Text with the Utah State Office of Education http://www.uen.org/core/science/sciber/trb4/downloads/literacy4.pdf Do you like mystery and intrigue? Do you like to do detective

More information

GEOLOGY 285: INTRO. PETROLOGY

GEOLOGY 285: INTRO. PETROLOGY Dr. Helen Lang Dept. of Geology & Geography West Virginia University FALL 2005 GEOLOGY 285: INTRO. PETROLOGY Mount St. Helens 1980 Eruption Small earthquakes Small steam and ash eruptions in March and

More information

Describing Cause and Effect

Describing Cause and Effect Introduction RI.3.3 Describe the relationship between a series of historical events, scientific ideas or concepts, or steps in technical procedures in a text, using language that pertains to... cause/effect.

More information

Earth processes are dynamic actions that occur both on

Earth processes are dynamic actions that occur both on 29 Weathering, Erosion, and Deposition R EA D I N G Earth processes are dynamic actions that occur both on the earth s surface and inside the earth. Any process that breaks down earth material, such as

More information

Weathering, Erosion, and Deposition

Weathering, Erosion, and Deposition Weathering, Erosion, and Deposition E Q : H O W I S T H E E A R T H A F F E C T E D B Y C O N S T R U C T I V E A N D D E S T R U C T I V E F O R C E S? http://player.discoveryeducation.com/index.cfm?guidassetid=6b1e329e-5a77-4b36-bfa9-1d307f75441c&blnfromsearch=1&productcode=us

More information

Question #1: What are some ways that you think the climate may have changed in the area where you live over the past million years?

Question #1: What are some ways that you think the climate may have changed in the area where you live over the past million years? Reading 5.2 Environmental Change Think about the area where you live. You may see changes in the landscape in that area over a year. Some of those changes are weather related. Others are due to how the

More information

The Upper Course of a River

The Upper Course of a River The Upper Course of a River I. Introduction A river is split along the long profile into three different sections; the upper, middle and lower course. As GCSE students you are expected to know the characteristics

More information

NOTES 1. Fossils. The BIG Idea Rocks, fossils, and other types of natural evidence tell Earth s story.

NOTES 1. Fossils. The BIG Idea Rocks, fossils, and other types of natural evidence tell Earth s story. Name Period Date UNIT 6 NOTES 1 Fossils Objectives Identify and describe the types of fossils. Define fossils Explain fossil formation Explain how different kinds of fossils show traces of life from Earth

More information

River Response. Sediment Water Wood. Confinement. Bank material. Channel morphology. Valley slope. Riparian vegetation.

River Response. Sediment Water Wood. Confinement. Bank material. Channel morphology. Valley slope. Riparian vegetation. River Response River Response Sediment Water Wood Confinement Valley slope Channel morphology Bank material Flow obstructions Riparian vegetation climate catchment vegetation hydrological regime channel

More information

BUILDING STRUCTURES ON OR NEAR STEEP SLOPES

BUILDING STRUCTURES ON OR NEAR STEEP SLOPES BUILDING STRUCTURES ON OR NEAR STEEP SLOPES Benefits of Building Structures on or Near Steep Slopes Why would you ever do this? In some instances, it is the steep slope that people want to be near. Like

More information

Your web browser (Safari 7) is out of date. For more security, comfort and the best experience on this site: Update your browser Ignore

Your web browser (Safari 7) is out of date. For more security, comfort and the best experience on this site: Update your browser Ignore Your web browser (Safari 7) is out of date. For more security, comfort and the best experience on this site: Update your browser Ignore ALLU VIAL FAN colluvial fan, debris cone For the complete encyclopedic

More information

GEOMORPHOLOGY WHAT AM I EXECTED TO LEARN?

GEOMORPHOLOGY WHAT AM I EXECTED TO LEARN? GEOMORPHOLOGY WHAT AM I EXECTED TO LEARN? Define rock. List and recognize clear examples of the three primary rocks types. Explain the difference between the three different ways sedimentary rocks are

More information

Science in the News - Plate Tectonics 1. Story

Science in the News - Plate Tectonics 1. Story Science in the News - Plate Tectonics 1. Story Scientists who study the Earth tell us the continents and ocean floors are always moving. This movement sometimes can be violent, causing death and destruction.

More information

Ronald Wilhelm & Jennifer Wilhelm, University of Kentucky Ages on Mars. Martian Surface Age Exploration

Ronald Wilhelm & Jennifer Wilhelm, University of Kentucky Ages on Mars. Martian Surface Age Exploration Ronald Wilhelm & Jennifer Wilhelm, University of Kentucky 2008 Ages on Mars Martian Surface Age Exploration You have now learned some very important things about various planets and moons in our Solar

More information

Earth s History. The principle of states that geologic processes that happened in the past can be explained by current geologic processes.

Earth s History. The principle of states that geologic processes that happened in the past can be explained by current geologic processes. Earth s History Date: Been There, Done That What is the principle of uniformitarianism? The principle of states that geologic processes that happened in the past can be explained by current geologic processes.

More information

Lesson 4 Rocks Rock! Lesson Overview: Students will become familiar with rocks, minerals, and be introduced to the rock cycle.

Lesson 4 Rocks Rock! Lesson Overview: Students will become familiar with rocks, minerals, and be introduced to the rock cycle. Lesson 4 Rocks Rock! Lesson Overview: Students will become familiar with rocks, minerals, and be introduced to the rock cycle. Objectives: Students will be able to: 1. Explain the difference between rocks

More information

Earth s Resources. Earth s Surface

Earth s Resources. Earth s Surface Earth s Resources Earth s Surface Earth s surface is made up of a layer of rock called the crust. The crust covers all of Earth. It is several miles thick. Most of the crust is under water. The upper part

More information

From VOA Learning English, this is SCIENCE IN THE NEWS, in Special English. I m Kelly Jean Kelly.

From VOA Learning English, this is SCIENCE IN THE NEWS, in Special English. I m Kelly Jean Kelly. From VOA Learning English, this is SCIENCE IN THE NEWS, in Special English. I m Kelly Jean Kelly. And I m Christopher Cruise. Scientists who study the Earth tell us the continents and ocean floors are

More information

Earth Boot Camp. 3.7B: Investigate rapid changes in Earth s surface such as volcanic eruptions, earthquakes and landslides.

Earth Boot Camp. 3.7B: Investigate rapid changes in Earth s surface such as volcanic eruptions, earthquakes and landslides. Earth Boot Camp 3.7B: Investigate rapid changes in Earth s surface such as volcanic eruptions, earthquakes and landslides. Release Questions 2006 #21 (65%) 1. In which of these ways can volcanoes help

More information

SEDIMENTARY ROCKS. When mountains are first formed, they are tall and jagged like the Rocky Mountains on the west coast of North America.

SEDIMENTARY ROCKS. When mountains are first formed, they are tall and jagged like the Rocky Mountains on the west coast of North America. SEDIMENTARY ROCKS When mountains are first formed, they are tall and jagged like the Rocky Mountains on the west coast of North America. Over time (millions of years) mountains become old mountains like

More information

Waterbury Dam Disturbance Mike Fitzgerald Devin Rowland

Waterbury Dam Disturbance Mike Fitzgerald Devin Rowland Waterbury Dam Disturbance Mike Fitzgerald Devin Rowland Abstract The Waterbury Dam was completed in October 1938 as a method of flood control in the Winooski Valley. The construction began in April1935

More information

Orting Community College Proposal

Orting Community College Proposal Orting Community College Proposal Cedric, Celina, Francine, Sarah, Samuel GEO CORP Located in Washington, 42 miles south of Seattle. Situated between two rivers on fertile plains. Built on lahar deposits.

More information

6.E E Rock Cycle/Weathering/Soil

6.E E Rock Cycle/Weathering/Soil Name: Date: 1. A lake is surrounded by hills covered with trees and shrubs. Which statement correctly describes how a change to the plants in this area will affect this environment? A. Adding plants to

More information

4 th Grade PSI. Slide 1 / 107 Slide 2 / 107. Slide 3 / 107. Slide 4 / 107. Slide 5 / 107. Slide 6 / 107. The History of Planet Earth

4 th Grade PSI. Slide 1 / 107 Slide 2 / 107. Slide 3 / 107. Slide 4 / 107. Slide 5 / 107. Slide 6 / 107. The History of Planet Earth Slide 1 / 107 Slide 2 / 107 4 th Grade PSI The History of Planet Earth 2015-11-10 www.njctl.org Slide 3 / 107 Slide 4 / 107 The History of Planet Earth The Structure of Earth Rock Layers Fossils and Relative

More information

Edible Changing Rock (Starbursts)

Edible Changing Rock (Starbursts) Name: Date: Hour: Lab Conduct Grade: 10 9 8 7 6 5 4 3 2 1 0 Edible Changing Rock (Starbursts) Most rocks are made of minerals. All rock begin as igneous rock which is formed when magma or lava cools and

More information

Earthquakes. Copyright 2006 InstructorWeb

Earthquakes. Copyright 2006 InstructorWeb Earthquakes Earthquakes cause the earth to shake! Earthquakes are caused by a fault line under the earth's crust. You do not have to be right under a fault line to feel an earthquake. You could be miles

More information

DETAILED DESCRIPTION OF STREAM CONDITIONS AND HABITAT TYPES IN REACH 4, REACH 5 AND REACH 6.

DETAILED DESCRIPTION OF STREAM CONDITIONS AND HABITAT TYPES IN REACH 4, REACH 5 AND REACH 6. DETAILED DESCRIPTION OF STREAM CONDITIONS AND HABITAT TYPES IN REACH 4, REACH 5 AND REACH 6. The Eklutna River was divided into study reaches (figure 1) prior to this site visit. Prominent geologic or

More information

You don t have to look too deeply to see how chemistry affects your life.

You don t have to look too deeply to see how chemistry affects your life. Chapter 1: Page 0 Chapter 1: Page 1 You don t have to look too deeply to see how chemistry affects your life. Every breath you take, every meal you eat, everything has something to do with the interaction

More information

Tips for Success on a Test

Tips for Success on a Test Number of Incorrect: Final Grade: Parent Signature: Top Tips for Success on a Test 1. Read the following statements at least two times. 2. Circle the key words in each question/ or statement. (*Remember

More information

sort examples of weathering into categories of biological, chemical, and physical;

sort examples of weathering into categories of biological, chemical, and physical; Key Question How are rocks and minerals weathered? Learning Goals sort examples of weathering into categories of biological, chemical, and physical; observe and describe physical and chemical changes in

More information

You Might Also Like. Thanks. Connect

You Might Also Like. Thanks. Connect Thanks Thank you for downloading my product. I truly appreciate your support and look forward to hearing your feedback. You can connect with me and find many free activities and strategies over at my blog

More information

Japan Disaster: 9.0 Earthquake

Japan Disaster: 9.0 Earthquake Well thank you all for coming. So I'm here to talk about the earthquake itself, and then we have other speakers who will talk about the tsunami and nuclear power, and radioactive fallout. So what happened

More information

1 Shoreline Erosion and Deposition

1 Shoreline Erosion and Deposition CHAPTER 12 1 Shoreline Erosion and Deposition SECTION Agents of Erosion and Deposition BEFORE YOU READ After you read this section, you should be able to answer these questions: What is a shoreline? How

More information

River Sediments. Sediment Types Are Not Randomly Distributed in a River s Sediment

River Sediments. Sediment Types Are Not Randomly Distributed in a River s Sediment River Sediments Sediment Types Are Not Randomly Distributed in a River s Sediment I ll just sit down on this bank of sand and watch the river flow. (Bob Dylan Watching the River Flow, 1971) A river has

More information

1. Erosion by Running Water Most powerful cause of erosion

1. Erosion by Running Water Most powerful cause of erosion I. Destructive Forces Notes: Destructive force: a process in which land is destroyed or changed such as weathering and erosion. All landforms are a result of a combination of constructive and destructive

More information

Notes and Summary pages:

Notes and Summary pages: Topographic Mapping 8.9C Interpret topographical maps and satellite views to identify land and erosional features and predict how these shapes may be reshaped by weathering ATL Skills: Communication taking

More information

Mechanical Weathering

Mechanical Weathering Mechanical Weathering Objectives Students will be able to: Explain how weathering breaks down rock. Explain how a rock s surface area affects the rate of weathering. The Great Sphinx Of all the amazing

More information

Figure 1 The map shows the top view of a meandering stream as it enters a lake. At which points along the stream are erosion and deposition dominant?

Figure 1 The map shows the top view of a meandering stream as it enters a lake. At which points along the stream are erosion and deposition dominant? 1. In which type of climate does chemical weathering usually occur most rapidly? 1. hot and dry 3. cold and dry 2. hot and wet 4. cold and wet 2. Figure 1 The map shows the top view of a meandering stream

More information

C E C U R R I C U L U M I E N S C B L E I T A. i N T E G R A T I N G A R T S i n O N A T I D U C B L I P U. Student Learning Objectives:

C E C U R R I C U L U M I E N S C B L E I T A. i N T E G R A T I N G A R T S i n O N A T I D U C B L I P U. Student Learning Objectives: We athering E Q U I T A B L E S C I E N C E C U R R I C U L U M Lesson 1 i N T E G R A T I N G A R T S i n P U B L I C E D U C A T I O N NGSS Science Standard: 4-ESS1-1 Identify evidence from patterns

More information

1. What is the definition of uniformitarianism? 2. What is the definition of organic? 4. What is the definition of inorganic?

1. What is the definition of uniformitarianism? 2. What is the definition of organic? 4. What is the definition of inorganic? Earth Science Unit 3- History of the Earth Knowledge Packet Learning Target 3B: Have you ever thought about the history of the Earth? No, well you should have because it s pretty cool. Things like mountain

More information

LANDFORMS. Extra Credit. Name Date

LANDFORMS. Extra Credit. Name Date LANDFORMS Extra Credit Name Date 1. Label the drawing above using the words below that match the landforms. canyon meander plateau delta mountain valley 2. The bending of rock at plate boundaries is A.

More information

Geography. Key facts. Volcanoes and volcanic eruptions

Geography. Key facts. Volcanoes and volcanic eruptions Geography Volcanoes and volcanic eruptions Volcanoes form when magma reaches the Earth's surface, causing eruptions of lava and ash. They occur at destructive (compressional) and constructive (tensional)

More information

River Processes. Learning Objective: Discover how a river erodes, transports and deposits material

River Processes. Learning Objective: Discover how a river erodes, transports and deposits material River Processes Learning Objective: Discover how a river erodes, transports and deposits material Learning Outcomes: Compare vertical and lateral erosion Describe how a river erodes, transports and deposits

More information

11.4 The Rock Cycle. Rocks and Soils. Objective. Materials. Teacher Tip. Directed Instruction. Content. Introduction

11.4 The Rock Cycle. Rocks and Soils. Objective. Materials. Teacher Tip. Directed Instruction. Content. Introduction 11.4 The Rock Cycle Rocks and Soils Objective Students will explain orally how rocks change form through the rock cycle. Materials Blackline Master 11.4A Discover: The Rock Cycle Blackline Master 11.4B

More information

The Importance of Mass Wasting

The Importance of Mass Wasting Mass Wasting: The Work of Gravity Earth Chapter 15 Chapter 15 Mass Wasting The Importance of Mass Wasting Slopes are the most common elements in our physical landscape Slopes may appear to be stable, but

More information

Science Is A Verb! Part 1 LET S DO IT! ISBN

Science Is A Verb! Part 1 LET S DO IT! ISBN LET S DO IT! Science Is A Verb! Part 1 ISBN 978-1-847003-56-0 Contents INTRODUCTION Lab Title How bright can you make the light bulbs? Students know how to design and build simple series and parallel circuits

More information

Erosion. changing landforms. Purpose. Process Skills. Background. Time 1 1 ½ hours Grouping Pairs, small groups, or class.

Erosion. changing landforms. Purpose. Process Skills. Background. Time 1 1 ½ hours Grouping Pairs, small groups, or class. Purpose To demonstrate how several factors affect the rate of erosion. Process Skills Observe, Measure, Collect data, Interpret data, Form a hypothesis, Make a model, Identify and control variables, Draw

More information

REVIEW. There are 2 types of WEATHERING: 1. CHEMICAL 2. PHYSICAL. What is WEATHERING? The breakdown of rocks at or near Earth s surface

REVIEW. There are 2 types of WEATHERING: 1. CHEMICAL 2. PHYSICAL. What is WEATHERING? The breakdown of rocks at or near Earth s surface REVIEW What is WEATHERING? Def: The breakdown of rocks at or near Earth s surface There are 2 types of WEATHERING: 1. CHEMICAL 2. PHYSICAL CHEMICAL WEATHERING EXAMPLES: 1. OXIDATION (rust) CHEMICAL WEATHERING

More information

The Moving Story of Plate Tectonics

The Moving Story of Plate Tectonics 08 January 2012 MP3 at voaspecialenglish.com The Moving Story of Plate Tectonics AP Smoke and ash from Italy's Mount Etna volcano last week FAITH LAPIDUS: This is SCIENCE IN THE NEWS in VOA Special English.

More information

Slow and Steady By ReadWorks

Slow and Steady By ReadWorks By ReadWorks How did all the amazing things on our planet form? How did magnificent mountain ranges rise up in one place and beautiful beaches form elsewhere? Why do some places experience earthquakes

More information

What is weathering and how does it change Earth s surface? Answer the question using

What is weathering and how does it change Earth s surface? Answer the question using 7 th Grade Lesson What is weathering and how does it change Earth s surface? Answer the question using the sentence frame. You have 4 minutes. Weathering is. This changes the Earth s surface because. 1

More information

Exploring and Drilling for Oil and Gas. Prepared by Tom Sheeran

Exploring and Drilling for Oil and Gas. Prepared by Tom Sheeran Exploring and Drilling for Oil and Gas What are Oil and Gas? Oil and Gas are substances found within the earth s crust. They are thought to come from decomposed plant and animal matter. Scientists believe

More information

abrasion the rubbing, grinding, and bumping of rocks that cause physical weathering (SRB, IG)

abrasion the rubbing, grinding, and bumping of rocks that cause physical weathering (SRB, IG) FOSS Soils, Rocks, and Landforms Module Glossary NGSS Edition 2019 abrasion the rubbing, grinding, and bumping of rocks that cause physical weathering (SRB, IG) acid a substance that geologists use to

More information

Analyzing our Topic IF SO, MAKE THE CHANGES AND BE READY TO REPORT OUT!

Analyzing our Topic IF SO, MAKE THE CHANGES AND BE READY TO REPORT OUT! Analyzing our Topic Look at the opening slide. Does anything there (words, pictures) make you want to change your thoughts from the smarties and chalk activities? IF SO, MAKE THE CHANGES AND BE READY TO

More information

Lesson Learning Goal

Lesson Learning Goal Rock Dating Lesson Learning Goal 4/12 n I can identify current methods for measuring the age of Earth and its parts, including the law of superposition and radioactive dating. Think About It... How old

More information

Why was this eruption important?

Why was this eruption important? Mount St. Helens Mount St. Helens has a long geological history (>3,000 yrs) of explosive eruptions. The 1980 Events: Initial relatively mild steam and ash (Vulcanian) eruptions. Sustained plinian eruption

More information

e with water and gases.

e with water and gases. Top deck 2 Assessment test Listening Unit 1 (Level 1) Listening test Part 1 1 3.09 Listen to the radio interview and match the sentence halves. Write a e on the line. There is one answer you do not need.

More information

Core Curriculum/Oklahoma AIMS Education Foundation

Core Curriculum/Oklahoma AIMS Education Foundation Topic Rocks Key Question How can models, drawings, and reading passages help you understand some ways that rocks form in layers? Learning Goals Students will: model how sediment layers can form rocks,

More information

Gradualism versus Catastrophism Curriculum written by XXXXX

Gradualism versus Catastrophism Curriculum written by XXXXX Gradualism versus Catastrophism Curriculum written by XXXXX A curriculum written with the goal of educating 8 th grade science students on the difference between gradual and cataclysmic geological events

More information

Activity 4: volcanic Hazards: Airborne Debris!

Activity 4: volcanic Hazards: Airborne Debris! Activity 4: volcanic Hazards: Airborne Debris! Create an entry in your table of contents with this name Write the name of the activity in BIG LETTERS on the next open page of your notebook. Find your new

More information

FOSSILS IN YOUR BACKYARD

FOSSILS IN YOUR BACKYARD MOR BACKYARD 12 Activity Overview BIG IDEA OBJECTIVE BACKGROUND Millions of years ago, dinosaurs roamed all over our planet Why is it then that we only find dinosaurs in certain geographical locations?

More information