Glaciers on the Move ScienceLIVE Lesson Plan Grades K-8 Summary In an inquiry base activity, students learn about how glaciers move by observing how a.

Slides:



Advertisements
Similar presentations
Investigation 1 Part 3: Water on a Slope
Advertisements

Jeopardy GlaciersLandforms More Landforms RANDOM Q $100 Q $200 Q $300 Q $400 Q $500 Q $100 Q $200 Q $300 Q $400 Q $500 Final Jeopardy.
1. 4. Understand how. moving ice acts as an. agent of erosion and
Erosion and Deposition
Changing Earth’s Surface
Glacial Erosion This type of erosion is called abrasion. Ice
Glaciation of Canada.
The movement of sediments by wind, water, ice, or gravity.
8th Grade Science Unit 8: Changes Over Time
Lisa Gardiner Sandra Henderson Becca Hatheway
Erosion and Deposition by Wind,
Unit 1 Lesson 4 Erosion and Deposition by Wind, Ice, and Gravity
Glacial Geomorphology Lab 10. Concepts Glacier Formation Accumulation and Ablation, Sublimation Movement Glacial Mass Balance Categories of Glaciers Where.
Erosion and Deposition by Glaciers Created By: Belinda Schmahl.
Glacier Movement: How Glaciers Move  The weight of overlying layers of ice and snow push down on the lower layers of the glacier.  This causes melting.
7.1 Glaciers.
Glacier Erosion  A glacier is a large, moving mass of ice that are found in either high elevations or near the poles.  A very large portion of Canada’s.
 As glaciers travel over land, glacial ice can erode the underlying bedrock.  This erosion can happen by:  Plucking  Abrasion.
Chapter 15-1 Glaciers Pages
The Changing Earth. The Changing Earth Chapter Fourteen: Weathering and Erosion 14.3 Rivers Shape the Land.
Erosion and Deposition n Erosion wears away surface materials and moves them from one location to another. n Agents of erosion are: gravity, glaciers,
Activity: Imagine that you are a tin can-shiny, new, and clean. But something happens, and you don’t make it to a recycling bin. Instead, you are left.
Chapter 9 - Section 3, 4, 5, and 6. How Water Erodes  Most sediment washes or falls into a river as a result of mass movement and runoff. Other sediment.
Section 15.2 Glacial Movements and Erosion
Erosion by Glaciers. A glacier is Any large mass of ice that moves slowly over land Think of it as a moving river of ice and snow.
Chapter 7.1 Glaciers.
8.3 Glaciers Types of glaciers Alpine Small glaciers that form valleys
Earth Science Review.
‘S‘S. VOCABULARY GLACIER - LARGE MOVING MASS OF ICE THAT FORMS NEAR EARTH’S POLES AND IN MOUNTAINOUS REGIONS AT HIGH ELEVATIONS. GLACIER - LARGE MOVING.
UNIT SEVEN: Earth’s Water  Chapter 21 Water and Solutions  Chapter 22 Water Systems  Chapter 23 How Water Shapes the Land.
Earth Science: 7.1A Glaciers. Glaciers  As recently as 15,000 years ago, up to 30 percent of earth’s land was covered by an glacial ice.  Earth was.
Chapter 3 Section 4 Glaciers. Moving mass of ice and snow Form when more snow falls than melts Agent of erosion.
Glaciers Erosive forces Glacier persistent body of dense ice that is constantly moving under its own weight. It forms where the accumulation of snow.
Glaciers Moving Ice Formation of Glaciers A glacier is defined as a mass of moving ice. A glacier is defined as a mass of moving ice. There are several.
What is erosion? -Erosion is the removal of rock particles and soil from an area -Erosion requires energy (usually supplied by gravity)
Ch 15: p  Enormous masses of moving ice created by the accumulation and compaction of snow.  Powerful agents of erosion ~ have carved some.
World Geography Unit 1: Land and Water Forms Glaciers as Agents of Erosion.
Glaciers. How Glaciers Form Form when snowfall exceeds melting. The heat and pressure from the mass cause a slight melting which lubricates the bottom.
Glaciers October 21st, Pre - Activity Knowledge Check on the note sheet provided, answer the true or false questions.
Glaciers UNIT 5 STANDARDS: STATE OBJECTIVES: NCES 2.1.1, 2.1.3, LESSON 6.
Table of Contents Title: 8.3 Glaciers Page: 80 Date: 3/4/2013.
An introduction to where, how, and why glaciers form
Mass movement & Glacial erosion
Erosion and Deposition by Glaciers Chapter 4: Topic 8.
Guided Notes For Glaciers Section 8.3. Glaciers shape the landscape by eroding, transporting, and depositing huge volumes of rock and sediment.
Glacial Landscapes Glacier = large moving mass of ice. Glacier = large moving mass of ice. Glaciers erode, transport and deposit massive amount of sediment.
By: Yohana Cantua & Fernando Ontiveros Materials one book cover or large piece of smooth paper one book with a hard, glossy cover one book with a rough.
Section 1 Changing Earth’s Surface Erosion movement of weathered rock and soil from one place to another.
(c) McGraw Hill Ryerson Water’s Effect on Shaping Earth’s Surface Water is always moving due to the water cycle  Quick changes can happen due.
Third Grade Part Two Review.
World Geography 3200/3202 October 2010
Erosion and Deposition Chapter 3 Section 1. Standard  S 6.2 Topography is reshaped by the weathering of roc and soil and by the transportation and deposition.
Glaciers We wouldn’t be here without them.. A Glacier is an accumulation of snow that is large enough to survive the summer melt. What are glaciers?
Lesson 3 Relationships. Stretching a spring What is the input variable here and what is the outcome variable?
Chapter 8 Erosional Forces Section 8-2 Glaciers Note Guide.
Glacier: Any large mass of ice that moves slowly over land.
Aim: How do glaciers move? Topic: Glaciers DN: 1.How does wind move sand? 2.Why are rocks eroded by wind more eroded at the base of the rock than.
Unit 1 Lesson 4 Erosion and Deposition by Wind, Ice, and Gravity Copyright © Houghton Mifflin Harcourt Publishing Company.
Glaciers once covered most of the Earth –in total there have been up to 22 times when glaciers covered large areas of the Earth… including Alberta the.
Agenda Check In Review notes Glaciers WATER Who’d’a Thunk: Karaoke means “empty orchestra” in Japanese.
Ice, Ice, Baby! Glaciers and Glacial Features Photo Source:
How Do Glaciers Shape the Land?
Unit 1 Lesson 4 Erosion and Deposition by Wind, Ice, and Gravity
Glacier Dynamics in a Changing Climate
Weathering, Erosion, and Soil
Unit 1 Lesson 4 Erosion and Deposition by Wind, Ice, and Gravity
Erosion and Deposition
8th Grade: The Dynamic Earth (Module E)
Unit 2 Lesson 3 Erosion and Deposition by Wind, Ice, and Gravity
Unit 1 Lesson 4 Erosion and Deposition by Wind, Ice, and Gravity
Presentation transcript:

Glaciers on the Move ScienceLIVE Lesson Plan Grades K-8 Summary In an inquiry base activity, students learn about how glaciers move by observing how a "flubber" glacier slides down a tiny mountain valley. While honing their observation skills, they will learn how slope and basal conditions (roughness of the ground surface) affect glacier movement. Learning Goals  A glacier is a large mass of ice that moves.  Glaciers form from snowfall that accumulates high in the mountains.  The movement of glaciers has shaped much of the world around us through erosion and deposition, creating U-shaped valleys, hanging valleys, arêtes, horns, and leaving behind glacial erratics.  Basal conditions and slope affect glacier movement. Materials  Flubber: Directions for one “glacier”: Mix together 90 mL glue and 120 mL water Add 80 mL Borax solution [solution is 3% Borax, 97% water] and mix well  4 sections of PVC Pipe (cut in half lengthwise), one covered in sandpaper, one covered in small pebbles (fish tank gravel works great for this)  4 stands for PVC Pipe, 3 tall, 1 short  4 plastic trays to catch flubber at the bottom  4 rulers  Sticky notes to mark glacier travel  Timer Experiment Set-Up Begin by having students come up with a prediction by answering the question, which glacier will travel the fastest and why? Next, divide students into four groups, one at each glacier chute. Use silly putty to connect the glacier chute to the stand and to the plastic trays, so the chute doesn’t slip. Designate a student in each group to be the “flubber handler”, and tell all of the students that the “flubber handler” is the only one allowed to touch the flubber until the end of the activity when its time to clean up. Also designate a student to hold the chute still throughout the activity. Do not begin until each “flubber handler” has the flubber in a ball, held at the top of the chute. Instruct the students to not touch the flubber after letting go until the activity is over. Begin the experiment as a class. Every 30 seconds, have students place a small sticky note at the far end of the glacier and measure the distance travelled. After 6 measurements, have students place the chute on the table, and put their hands in their pockets to await cleanup instructions. After cleaning up the activity, have students write up the final distance travelled on the board, and compare results. 1 ScienceLIVE

Class Schedule  20 minutes: Interactive PowerPoint slide show that introduces students to glaciology: what glaciers are, how they form, and the kind of landscapes created by glaciers.  5 minutes: Introduce activity, set up each chute, and designate “flubber handler” in each group. Wait until all groups are ready with the flubber held at the top of the chute before beginning experiment.  15 minutes: Run glacier experiment.  5 minutes: Graph results. Compare class results.  5 minutes: Write up conclusions and wrap up. Prediction Which glacier will travel the fastest? Why? Discussion Questions  Which glacier travelled the fastest? Why do you think so?  The steep slope, smooth surface glacier travelled the fastest due to higher momentum because of gravity, and lower friction due to the smooth surface.  Was every experiment run the same? Were there sources of human error?  Did any groups touch their flubber during the experiment? Did the chute fall during the experiment?  What is the difference between glacier movement and glacier melt? Can they happen at the same time?  Glacier movement occurs throughout the year, and is the movement of the entire glacier downhill. Glacier melt usually happens only in the summer or during warm temperatures, and happens more at the bottom of the glacier. Yes, both happen at the same time. Trouble Shooting Tips  Classroom management is essential with this activity, as it can become messy fast! Designating a “flubber handler” is an excellent way to keep the activity clean and ordered.  Flubber temperature and consistency and be variable. Do your best to keep the flubber at a constant temperature (refrigerated), as warmer flubber will travel faster than cold flubber. Acknowledge this as an issue with the kids if the class gets different results than expected. Sources ScienceLIVE