GC 225 Lecture Exam #2

Size: px
Start display at page:

Download "GC 225 Lecture Exam #2"

Transcription

1 GC 225 Lecture Exam #2 Direction- path along which something is moving. 3 Types; - COMPASS DIRECTIONAL NAME (32 in total) - BEARING (four 0 o - 90 o ) - AZIMUTHS (0 o o ) Compass (32 named points) N N W Bearings (4 quadrants) 0 N E Azimuth NW NE S S E SW 0 SE S E Baselines typically north south trending lines; - True North - Northerly direction along a line of longitude. - Magnetic North - Direction to the magnetic north pole of the earth. - Grid North - North trending direction aligned to specialized grid lines on the maps. Magnetic Declination angular difference between true north and magnetic north in a location. AGONIC LINE - an imaginary line on the earth's surface along which true north and magnetic north are identical. Magnetic North Agonic Line

2 MAP ORIENTATION 1.) INSPECTION looking for easily recognizable landmarks. 2.) RESECTION sighting on known ground positions. 3.) INTERSECTION object with unknown position. RESECTION INTERSECTION 3 Known Positions 2 1 Position is Known Unknown Position Map Your position on map Object with unknown position Map Route Selection planning the best route (path) from A to B using a map. GPS (GLOBAL POSITIONING SYSTEM) 1.) Space Segment - cluster of 24 satellites, orbiting in 6 planes (4 in each plane). 2.) Control Segment operates GPS in master stations close to the equator. (Colorado) 3.) User Segment small hand-held receiver unit. (Need 3 satellites to determine exact position, more the better) Spot Heights a known height of a point relative to a datum (sea level) (Exm. = Lake Superior 602 feet above sea level)

3 Contours imaginary lines that join points of equal elevation relative to a datum (sea level). - CONTOUR INTERVAL - vertical distance between contours. Types; Index (darker, every 5th line, often labeled) Intermediate (lighter) Supplementary (extra lines at half intervals) Depression (have ticks and are read downward) Approximate (dashed or dotted) Carrying (very close, indicates drastic slope) Layer Tints OTHER WAYS OF SHOWING RELIEF Colors or grey tones used to fill in between contours. Illuminated Contours Adds artificial brightness and shading to contours to further accentuate topography. Hill Shading Similar to above but with no contours. Physical Model Three dimensional model is made of plastic, etc. Block Diagrams (Armin K. Lobeck) Three-dimensional representation of landscape and below ground features. CONTOUR INTERPRETATION - Contours always close - Closed contours = hill or depression - Variations in horizontal spacing of contours reflect variations in slope. Close = steep Wide = flat (general) - Contours crossing valleys point upsteam - INTERFLUVES - Contours with closed ends indicate ridges of drainage divides.

4 CONTOUR APPLICATIONS - LINEAR INTERPOLATION point between contour lines, may be used to estimate. Z 6 mm 10 mm - PROFILING a simple cross-section view through a particular piece of terrain. - SLOPE a measure of the vertical difference in elevation of a surface at 2 different points in relation to the horizontal distance between same points. (rise over run) CLOSED DEPRESSIONS Causes; - Wind Erosion (deflation) - Glacial Activity (Kettle Lakes) - Impact Craters (Meteorites) - Karst Processes (Sink Holes) - Human Activity (Mining, Quarrying) STREAM & DRAINAGE PATTERNS

5 Delta landforms with flat surface that may form where a creek/river enters a large body of water. May have many shapes and outlines (birds foot). Alluvial Fan - Landform that is fan shaped that forms where a river, stream, or creek leaves its valley and enters a larger valley or basin. Common in arid, semi-arid settings and with areas of a great deal of runoff such as construction sites. COASTAL LANDFORMS Erosional wave cut (bluffs, cliffs, terraces) Depositional spits, barriers, tambolos, beach ridges TOMBOLO land locked island. (Presque Isle) LAGOON closed in water by a Bay Barrier. (Big Bay / Lake Independence) BEACH RIDGES old beach locations which are now above lake/sea level. (Alger County) SPIT small peninsula sticking out making a point. (Little Presque) Alpine (Mountain) Glacial Landforms U-Shaped Valleys (Troughs) Arêtes knife shaped feature. GLACIAL LANDFORMS Horns mountain top, created by a collection of Arêtes. Cols lowest dip between mountains. Cirques mountain 3-sided valley, where glaciers are or used to be. Tarns depression that has filled up with water.

6 Continental Glacial Landforms Moraines unsorted gravel/debris made by a glacier front. Outwash plains flat area, where glaciers stalled and dumped water/sand. Kettle Lakes lakes are formed from depressions & a reseeding glacier. Drumlins teardrop shape, stuck up under a glacier, causing debris to collect. Eskers an inverted valley, ahead of the old glacier. Roche Moutonnées causing one side to be rock & the other dirt. Eolian Features windblown or degraded features. Cuestas step slopes on a rock ledge. Transverse Dunes Barcain Dunes

c. 1 inch = 0.6 miles e. 1:100,000 f. 1:250,000 f. 1 inch = 4.0 miles

c. 1 inch = 0.6 miles e. 1:100,000 f. 1:250,000 f. 1 inch = 4.0 miles High School Advance Geology Map Test 2014 Name Use the information on each map to provide the best answer to the questions. Fill in the bubble of the best answer on your answer sheet. Answer questions

More information

LAB P - GLACIAL PROCESSES AND LANDSCAPES

LAB P - GLACIAL PROCESSES AND LANDSCAPES Introduction LAB P - GLACIAL PROCESSES AND LANDSCAPES Ice has been a significant force in modifying the surface of the earth at numerous times throughout Earth s history. Though more important during the

More information

1 Glacial Erosion and

1 Glacial Erosion and www.ck12.org Chapter 1. Glacial Erosion and Deposition CHAPTER 1 Glacial Erosion and Deposition Lesson Objectives Discuss the different erosional features formed by alpine glaciers. Describe the processes

More information

Recrystallization of snow to form LARGE. called FIRN: like packed snowballs. the weight of overlying firn and snow.

Recrystallization of snow to form LARGE. called FIRN: like packed snowballs. the weight of overlying firn and snow. Chapter 11 Glaciers BFRB P. 103-104, 104, 108, 117-120120 Process of Glacier Formation Snow does NOT melt in summer Recrystallization of snow to form LARGE crystals of ice (rough and granular) called

More information

Glaciers and Glaciation Earth - Chapter 18 Stan Hatfield Southwestern Illinois College

Glaciers and Glaciation Earth - Chapter 18 Stan Hatfield Southwestern Illinois College Glaciers and Glaciation Earth - Chapter 18 Stan Hatfield Southwestern Illinois College Glaciers Glaciers are parts of two basic cycles: 1. Hydrologic cycle 2. Rock cycle A glacier is a thick mass of ice

More information

PHYSICAL GEOGRAPHY GEOGRAPHY EARTH SYSTEMS COASTAL SYSTEMS FLUVIAL SYSTEMS

PHYSICAL GEOGRAPHY GEOGRAPHY EARTH SYSTEMS COASTAL SYSTEMS FLUVIAL SYSTEMS PHYSICAL GEOGRAPHY EARTH SYSTEMS FLUVIAL SYSTEMS COASTAL SYSTEMS PHYSICAL GEOGRAPHY CORRIES / CIRQUES A Corrie or Cirque is the armchair shaped hollow that was the birthplace of a glacier. It has steep,

More information

1.4 Understand how moving ice acts as an agent of erosion and deposition. (Chap. 2)

1.4 Understand how moving ice acts as an agent of erosion and deposition. (Chap. 2) 1.4 Understand how moving ice acts as an agent of erosion and deposition. (Chap. 2) There are two types of glaciation. Alpine Glaciation Continental Glaciation Distinguish between the terms alpine glaciation

More information

Glaciers. Glacier Dynamics. Glacier Dynamics. Glaciers and Glaciation. Types of Glaciers. Chapter 15

Glaciers. Glacier Dynamics. Glacier Dynamics. Glaciers and Glaciation. Types of Glaciers. Chapter 15 Chapter 15 Glaciers and Glaciation Glaciers A glacier is a large, permanent (nonseasonal) mass of ice that is formed on land and moves under the force of gravity. Glaciers may form anywhere that snow accumulation

More information

ENVI2030L - ALPINE AND CONTINENTAL GLACIATION

ENVI2030L - ALPINE AND CONTINENTAL GLACIATION NAME ENVI2030L - ALPINE AND CONTINENTAL GLACIATION I. Introduction Glaciers are slowly moving ice sheets. They are very effective erosional agents and can drastically modify the landscapes over which they

More information

12: MELTWATER LANDFORM IDENTIFICATION

12: MELTWATER LANDFORM IDENTIFICATION Glacial Geology 12. Meltwater Landform Identification 12: MELTWATER LANDFORM IDENTIFICATION 60 Points Objective: learn how to identify meltwater landforms and their characteristics in photos and on topographic

More information

glacial drift: all deposits associated with glaciation; covers 8% of Earth s surface above sealevel, and 25% of North America

glacial drift: all deposits associated with glaciation; covers 8% of Earth s surface above sealevel, and 25% of North America Glacial depositional features glacial drift: all deposits associated with glaciation; covers 8% of Earth s surface above sealevel, and 25% of North America i) nonstratified drift till: transported & deposited

More information

Glaciers Earth 9th Edition Chapter 18 Mass wasting: summary in haiku form Glaciers Glaciers Glaciers Glaciers Formation of glacial ice

Glaciers Earth 9th Edition Chapter 18 Mass wasting: summary in haiku form Glaciers Glaciers Glaciers Glaciers Formation of glacial ice 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 Earth 9 th Edition Chapter 18 Mass wasting: summary in haiku form Ten thousand years thence big glaciers began to melt - called "global warming." are parts of two basic

More information

GLACIATION. The Last Ice Age (see Chapter 12) and. Pleistocene Ice Cap. Glacial Dynamics 10/2/2012. Laurentide Ice Sheet over NYS

GLACIATION. The Last Ice Age (see Chapter 12) and. Pleistocene Ice Cap. Glacial Dynamics 10/2/2012. Laurentide Ice Sheet over NYS GLACIATION and New York State Prof. Anthony Grande The Last Ice Age (see Chapter 1) The Pleistocene Epoch began 1.6 mya. During this time, climates grew colder. There were numerous ice ages starting 100,000000

More information

Glaciers. Valley or Alpine glaciers. Ice sheets. Piedmont - foot of the mountain glaciers. Form in mountainous areas Move downslope in valleys

Glaciers. Valley or Alpine glaciers. Ice sheets. Piedmont - foot of the mountain glaciers. Form in mountainous areas Move downslope in valleys Glaciers & Ice Ages Glaciers Valley or Alpine glaciers Form in mountainous areas Move downslope in valleys Ice sheets Move outward from center Continental glaciers - large scale, ice age type. Presently

More information

Dynamic Planet Practice Test Written by Samuel Bressler

Dynamic Planet Practice Test Written by Samuel Bressler Dynamic Planet Practice Test 2013 Written by Samuel Bressler Part 1: Multiple Choice 1. Which of the following is NOT related to alpine glaciation? a) Serac b) Kame c) Col d) Paternoster Lake 2. The common

More information

Glacial Origins and Features of Long Island

Glacial Origins and Features of Long Island Glacial Origins and Features of Long Island Interior Coastal Plain Continental Shelf Long Island s Geology 0 Ma Phanerozoic 540 Ma Proterozoic 2500 Ma Archean 3800 Ma Hadean 4600 Ma C M P Geologic Time

More information

Dynamic Planet: Glaciers

Dynamic Planet: Glaciers Team Name+Number Teammate 1 name Teammate 2 name Dynamic Planet: Glaciers (by Shad160) The following test is 80 questions long, split up into four different sections. The first 20 questions are worth 40

More information

glacier Little Ice Age continental glacier valley glacier ice cap glaciation firn glacial ice plastic flow basal slip Chapter 14

glacier Little Ice Age continental glacier valley glacier ice cap glaciation firn glacial ice plastic flow basal slip Chapter 14 Little Ice Age glacier valley glacier continental glacier ice cap glaciation firn glacial ice plastic flow basal slip glacial budget zone of accumulation zone of wastage glacial surge abrasion glacial

More information

Chapter 16 Glaciers and Glaciations

Chapter 16 Glaciers and Glaciations Chapter 16 Glaciers and Glaciations Name: Page 419-454 (2nd Ed.) ; Page 406-439 (1st Ed.) Part A: Anticipation Guide: Please read through these statements before reading and mark them as true or false.

More information

Shaping of North America. Physical Geography II of the United States and Canada. The Last Ice Age. The Ice Age. Pleistocene Polar Ice Cap 2/14/2013

Shaping of North America. Physical Geography II of the United States and Canada. The Last Ice Age. The Ice Age. Pleistocene Polar Ice Cap 2/14/2013 Physical Geography II of the United States and Canada Prof. Anthony Grande AFG 2012 Shaping of North America The chief shaper of the landscape of North America is and has been running water. Glaciation

More information

READING QUESTIONS: Glaciers GEOL /WI 60 pts. a. Alpine Ice from larger ice masses flowing through a valley to the ocean

READING QUESTIONS: Glaciers GEOL /WI 60 pts. a. Alpine Ice from larger ice masses flowing through a valley to the ocean READING QUESTIONS: Glaciers GEOL 131 18/WI 60 pts NAME DUE: Tuesday, March 13 Glaciers: A Part of Two Basic Cycles (p. 192-195) 1. Match each type of glacier to its description: (2 pts) a. Alpine Ice from

More information

MiSP Topographic Maps Worksheet #1a SLOPE AND TOPOGRAPHIC CONTOURS

MiSP Topographic Maps Worksheet #1a SLOPE AND TOPOGRAPHIC CONTOURS MiSP Topographic Maps Worksheet #1a Name Date Introduction: SLOPE AND TOPOGRAPHIC CONTOURS Topographic contours are shown by lines of different widths. Each contour is a line of equal elevation; therefore,

More information

The Physical Geography of Long Island

The Physical Geography of Long Island The Physical Geography of Long Island A Bit About Long Island Length 118 miles Brooklyn to Montauk Geo202 Spring 2012 Width 23 miles at it s widest Area 1,400 square miles Formation of Long Island River

More information

MIDDLE SCHOOL CURRICULUM TR AILING ICE AGE M YST ERI E S SEARCHING GLACIAL FEATURES

MIDDLE SCHOOL CURRICULUM TR AILING ICE AGE M YST ERI E S SEARCHING GLACIAL FEATURES MIDDLE SCHOOL CURRICULUM TR AILING ICE AGE M YST ERI E S SEARCHING GLACIAL FEATURES CONTENTS I. Enduring Knowledge... 3 II. Teacher Background... 3 III. Before Viewing the Video... 5 IV. Viewing Guide...

More information

Glaciers. Glacier Dynamics. Glaciers and Glaciation. East Greenland. Types of Glaciers. Chapter 16

Glaciers. Glacier Dynamics. Glaciers and Glaciation. East Greenland. Types of Glaciers. Chapter 16 Chapter 16 Glaciers A glacier is a large, permanent (nonseasonal) mass of ice that is formed on land and moves under the force of gravity. Glaciers may form anywhere that snow accumulation exceeds seasonal

More information

Introduction to Topographic Maps

Introduction to Topographic Maps Introduction to Topographic Maps DIRECTIONS: Read all of the following content. READ EVERYTHING!! At the end of the packet, you will find two topographic maps. Your task is to indentify each of the elevations

More information

Great Science Adventures

Great Science Adventures Great Science Adventures Lesson 18 How do glaciers affect the land? Lithosphere Concepts: There are two kinds of glaciers: valley glaciers which form in high mountain valleys, and continental glaciers

More information

MiSP Topographic Maps Worksheet #1a L2

MiSP Topographic Maps Worksheet #1a L2 MiSP Topographic Maps Worksheet #1a L2 Name Date SLOPE AND TOPOGRAPHIC CONTOURS Introduction: Topographic contours are shown by lines of different widths. Each contour is a line of equal elevation; therefore,

More information

NYS Invitational Science Olympiad April 2005 DYNAMIC PLANET: GLACIERS

NYS Invitational Science Olympiad April 2005 DYNAMIC PLANET: GLACIERS NYS Invitational Science Olympiad April 2005 School Team # DYNAMIC PLANET: GLACIERS 1. What type of glacier is shown in the photo? 2. a. What is the name of the feature labeled A? b. How did feature A

More information

READING QUESTIONS: Chapter 7, Glaciers GEOL 131 Fall pts. a. Alpine Ice from larger ice masses flowing through a valley to the ocean

READING QUESTIONS: Chapter 7, Glaciers GEOL 131 Fall pts. a. Alpine Ice from larger ice masses flowing through a valley to the ocean READING QUESTIONS: Chapter 7, Glaciers GEOL 131 Fall 2018 63 pts NAME DUE: Tuesday, October 23 Glaciers: A Part of Two Basic Cycles (p. 192-195) 1. Match each type of glacier to its description: (2 pts)

More information

Glaciers. Clicker Question. Glaciers and Glaciation. How familiar are you with glaciers? West Greenland. Types of Glaciers.

Glaciers. Clicker Question. Glaciers and Glaciation. How familiar are you with glaciers? West Greenland. Types of Glaciers. Chapter 21 Glaciers A glacier is a large, permanent (nonseasonal) mass of ice that is formed on land and moves under the force of gravity. Glaciers may form anywhere that snow accumulation exceeds seasonal

More information

Gifts of the Glaciers

Gifts of the Glaciers Gifts of the Glaciers Gifts of the Glaciers Moving ice of glacier was responsible for water, landforms, and soil characteristics and patterns of today Sculpturing of bedrock materials Glacial Landforms

More information

Making glacial connections

Making glacial connections Student task A 1. Cut and arrange the cards below to make four sets of four connections: Four connections Matterhorn drumlin lateral U-shaped valley outwash plain truncated spur Lauterbrunnen ground medial

More information

Glaciers and Glaciation

Glaciers and Glaciation Chapter 18 Lecture Earth: An Introduction to Physical Geology Eleventh Edition Glaciers and Glaciation Tarbuck and Lutgens Glaciers: A Part of Two Basic Cycles A glacier is a thick mass of ice that forms,

More information

Chapter 14. Glaciers and Glaciation

Chapter 14. Glaciers and Glaciation Chapter 14 Glaciers and Glaciation Introduction Pleistocene Glaciations: A series of "ice ages" and warmer intervals that occurred 2.6 million to 10,000 years ago. The Little Ice Age was a time of colder

More information

Figure 1 Understanding Map Contours

Figure 1 Understanding Map Contours Figure 1 Understanding Map Contours The light brown lines overprinted on topographic maps are called contour lines. They indicate the elevation above sea level of land features and thus permit you to view

More information

Glaciers Earth Chapter 18 Chapter 18 Glaciers & Glaciation Glaciers: A Part of Two Basic Cycles Glaciers: A Part of Two Basic Cycles Valley Glacier

Glaciers Earth Chapter 18 Chapter 18 Glaciers & Glaciation Glaciers: A Part of Two Basic Cycles Glaciers: A Part of Two Basic Cycles Valley Glacier 1 2 3 4 5 6 7 8 9 10 11 12 Glaciers Earth Chapter 18 Chapter 18 Glaciers & Glaciation A glacier is a thick mass of ice that forms, over hundreds and thousands of years, by the accumulation, compaction,

More information

The Northeast: America's Gateway to the World

The Northeast: America's Gateway to the World The Northeast: America's Gateway to the World Living in the Shadow of the Ice a lesson on the impact of glaciation on Northeast landscapes INTRODUCTION: The region we call the Northeast has a very long

More information

Glaciers. Reading Practice

Glaciers. Reading Practice Reading Practice A Glaciers Besides the earth s oceans, glacier ice is the largest source of water on earth. A glacier is a massive stream or sheet of ice that moves underneath itself under the influence

More information

Camp Jack Wright PERMANENT ORIENTEERING COURSE (2004)

Camp Jack Wright PERMANENT ORIENTEERING COURSE (2004) Camp Jack Wright PERMANENT ORIENTEERING COURSE (2004) WHAT IS ORIENTEERING? The skill which enables a person to navigate with a map. In the competitive sport, the winner is the person who finishes in the

More information

Map & Compass so easy a caveman can do it!

Map & Compass so easy a caveman can do it! Map & Compass so easy a caveman can do it! Compass Basics Opening Comments Terms of a compass Boxing a needle Get a bearing (you to a point) Get a bearing (a point to you) Orienting a map Get a bearing

More information

MIDDLE SCHOOL CURRICULUM TR AILING ICE AGE M YST ERI E S ICE AGE TREKKING

MIDDLE SCHOOL CURRICULUM TR AILING ICE AGE M YST ERI E S ICE AGE TREKKING MIDDLE SCHOOL CURRICULUM TR AILING ICE AGE M YST ERI E S ICE AGE TREKKING CONTENTS I. Enduring Knowledge... 3 II. Teacher Background... 3 III. Before Viewing this Video... 5 IV. Viewing Guide... 5 V. Discussion

More information

Glacial Geomorphology Exercise

Glacial Geomorphology Exercise James Madison University Field Course in western Ireland Glacial Geomorphology Exercise 3-day road log (abbreviated) Striations Large kame terrace Cirque with moraines Kame delta Striations Eskers Raised

More information

Red Tarn, Lake District They are all features of glacial erosion

Red Tarn, Lake District They are all features of glacial erosion Ribbon Lake Lake Windermere, Lake District Arete Striding Edge, Lake District 1 2 3 Pyramidal Peak Corrie & Tarn 4 Matterhorn, Switzerland Red Tarn, Lake District They are all features of glacial erosion

More information

Alpine Glacial Features along the Chimney Pond Trail, Baxter State Park, Maine

Alpine Glacial Features along the Chimney Pond Trail, Baxter State Park, Maine Maine Geologic Facts and Localities September, 2009 Alpine Glacial Features along the Chimney Pond Trail, Baxter State Park, Maine 45 54 57.98 N, 68 54 41.48 W Text by Robert A. Johnston, Department of

More information

Chapter 17. Glacial & Periglacial Landscapes

Chapter 17. Glacial & Periglacial Landscapes Chapter 17 Glacial & Periglacial Landscapes Cryosphere Cryosphere - the portions of Earth's surface where water is in solid form, including sea ice, lake ice, river ice, snow cover, glaciers, ice caps,

More information

I. Types of Glaciers 11/22/2011. I. Types of Glaciers. Glaciers and Glaciation. Chapter 11 Temp. B. Types of glaciers

I. Types of Glaciers 11/22/2011. I. Types of Glaciers. Glaciers and Glaciation. Chapter 11 Temp. B. Types of glaciers Why should I care about glaciers? Look closely at this graph to understand why we should care? and Glaciation Chapter 11 Temp I. Types of A. Glacier a thick mass of ice that originates on land from the

More information

Glaciers. Chapter 17

Glaciers. Chapter 17 Glaciers Chapter 17 Vocabulary 1. Glacier 2. Snowfield 3. Firn 4. Alpine glacier 5. Continental glacier 6. Basal slip 7. Internal plastic flow 8. Crevasses 9. Glacial grooves 10. Ice shelves 11. Icebergs

More information

Road Scholar Gopher Science Olympiad Invitational January 6, Team #: Team Name: Names: Score:

Road Scholar Gopher Science Olympiad Invitational January 6, Team #: Team Name: Names: Score: Road Scholar Gopher Science Olympiad Invitational January 6, 2018 Team #: Team Name: Names: Score: Welcome to Road Scholar! Your Science Olympiad team is planning a trip to an invitational tournament in

More information

Parts of a Glacier Division A Study Guide- Part 2

Parts of a Glacier Division A Study Guide- Part 2 Parts of a Glacier Division A Study Guide- Part 2 Zones of a glacier Zone of Accumulation: The region where snowfall adds ice to the glacier. It occurs where the temperature remains cold enough year-round

More information

GLACIER STUDIES OF THE McCALL GLACIER, ALASKA

GLACIER STUDIES OF THE McCALL GLACIER, ALASKA GLACIER STUDIES OF THE McCALL GLACIER, ALASKA T John E. Sater* HE McCall Glacier is a long thin body of ice shaped roughly like a crescent. Its overall length is approximately 8 km. and its average width

More information

Lidar Imagery Reveals Maine's Land Surface in Unprecedented Detail

Lidar Imagery Reveals Maine's Land Surface in Unprecedented Detail Maine Geologic Facts and Localities December, 2011 Lidar Imagery Reveals Maine's Land Surface in Unprecedented Detail Text by Woodrow Thompson, Department of Agriculture, Conservation & Forestry 1 Introduction

More information

GEOMORPHOLOGY EXAM #3

GEOMORPHOLOGY EXAM #3 Formation of Glaciers GEOMORPHOLOGY EXAM #3 - Transformation of snow into glacial ice - Density; SNOW = 0.07 0.18 g/cc FIRN(Neve) = 0.4 0.8 g/cc (Pellets) GLACIAL ICE = 0.8 0.9 g/cc - Firn / Ice Boundary

More information

GY 301: Geomorphology Lab 9: Alpine Glaciers and Geomorphology

GY 301: Geomorphology Lab 9: Alpine Glaciers and Geomorphology Name: Raw score: /45 Percentage: /100% Your Task: Today s lab deals with the interpretation of geomorphological features that typically result from alpine glacial activity. The exercises should be able

More information

Lesson. Glaciers Carve the Land A QUICK LOOK. Overview. Big Idea. Process Skills Key Notes

Lesson. Glaciers Carve the Land A QUICK LOOK. Overview. Big Idea. Process Skills Key Notes EARTH S CHANGING SURFACE CLUSTER 2 HOW THE EARTH S SURFACE CHANGES Lesson 62 Glaciers Carve the Land A QUICK LOOK Big Idea Moving water, ice, and wind break down rock, transport materials, and build up

More information

CHAPTER 12: AERONAUTICAL CHARTS AND NAVIGATION

CHAPTER 12: AERONAUTICAL CHARTS AND NAVIGATION CHAPTER 12: AERONAUTICAL CHARTS AND NAVIGATION Once you start to venture out from your home gliderport, you need to be able to figure out where you are and how to get where you want to go. Aeronautical

More information

Topographic Maps. Background Sheet

Topographic Maps. Background Sheet Topographic Maps History: Background heet The Articles of Confederation (1777) was ratified when western lands were yielded to the Federal Government. This yielding of land gave the Federal Government

More information

Please make sure that all teachers and chaperones attending the field study are aware of the following information:

Please make sure that all teachers and chaperones attending the field study are aware of the following information: Dear Teacher, Thank you for signing up for The Ice Age at the Lost Valley Visitor Center in Glacial Park. The visitor center is located in the middle of Glacial Park. Follow the signs from the Harts Road

More information

A topographic map shows:,,,,

A topographic map shows:,,,, Name: Period: Mapping the Earth Notes What is a map? Label the compass directions: What does latitude measure? What is the name of the 0 latitude line? Where is 90 north latitude? Where is 90 south latitude?

More information

Formation of a Corrie

Formation of a Corrie Formation of a Corrie A corrie looks rather like a armchair has been cut out of the rock face When a hill has been heavily eroded with 3 or 4 corries the jagged hill that is left is known as a pyramidal

More information

Exam Review. Part 3- Deserts, Glaciers, and maps

Exam Review. Part 3- Deserts, Glaciers, and maps Exam Review Part 3- Deserts, Glaciers, and maps What causes a desert? Lots of sand Vegetation holds the arms Star Dunes- Star dunes form only in places where wind blows from varied directions over the

More information

47I THE LAS ANIMAS GLACIER.

47I THE LAS ANIMAS GLACIER. THE LAS ANIMAS GLACIER. ONE of the largest of the extinct glaciers of the Rocky Mountains was that which occupied the valley of the Las Animas river. This stream originates in the San Juan mountains in

More information

The Atlas of Hillforts of Britain and Ireland. Hillfort survey notes for guidance

The Atlas of Hillforts of Britain and Ireland. Hillfort survey notes for guidance The Atlas of Hillforts of Britain and Ireland Hillfort survey notes for guidance The collection of surveys for the Atlas is now finished but you can use this form and the accompanying Notes for Guidance

More information

Orientation and Traveling

Orientation and Traveling UNIT 4 Orientation and Traveling Chapter Title 4-1 Land Navigation 4-2 Navigation Using the Sun and the Stars 4-3 Land Travel 4-4 Signaling Techniques 4-5 Recovery Principles CHAPTER 4-1 Land Navigation

More information

There are actually six geographic sub-regions, three in both the uplands and the lowlands.

There are actually six geographic sub-regions, three in both the uplands and the lowlands. 6 Regions of AR Although Arkansas is most easily divided into two distinct geographical regions, the northwestern uplands and the southeastern lowlands, this description does not accurately portray the

More information

2. (1pt) From an aircraft, how can you tell the difference between a snowfield and a snow-covered glacier?

2. (1pt) From an aircraft, how can you tell the difference between a snowfield and a snow-covered glacier? 1 GLACIERS 1. (2pts) Define a glacier: 2. (1pt) From an aircraft, how can you tell the difference between a snowfield and a snow-covered glacier? 3. (2pts) What is the relative size of Antarctica, Greenland,

More information

Below is an example of a well laid-out template of a route card used by the Sionnach Team which is a good format to begin with.

Below is an example of a well laid-out template of a route card used by the Sionnach Team which is a good format to begin with. Route Card A route card is used as a navigational aid to hill walkers by setting out a step by step plan for an intended hike. It is good practice to make out a route card before every hike you or your

More information

Landscapes in the UK: Glaciation 1. Extent of ice cover across the UK during the last ice age.

Landscapes in the UK: Glaciation 1. Extent of ice cover across the UK during the last ice age. Landscapes in the UK: Glaciation 1. Extent of ice cover across the UK during the last ice age. Key idea: Ice was a powerful force in shaping the landscape of the UK. As the climate has changed in the past,

More information

THE DEPARTMENT OF HIGHER EDUCATION UNIVERSITY OF COMPUTER STUDIES FIFTH YEAR

THE DEPARTMENT OF HIGHER EDUCATION UNIVERSITY OF COMPUTER STUDIES FIFTH YEAR THE DEPARTMENT OF HIGHER EDUCATION UNIVERSITY OF COMPUTER STUDIES FIFTH YEAR (B.C.Sc./B.C.Tech.) RE- EXAMINATION SEPTEMBER 2018 Answer all questions. ENGLISH Time allowed: 3 hours QUESTION I Glaciers A

More information

Chapter 6: Morphotectonics of the Gödöllő Hills 91

Chapter 6: Morphotectonics of the Gödöllő Hills 91 Chapter 6: Morphotectonics of the Gödöllő Hills 91 - SE dipping ridges are typical in the study area, thus a separate symbol has been introduced for these landforms. They were formed by the incision of

More information

Stephens State Park Trails

Stephens State Park Trails TRAILS OF ALLAMUCHY MOUNTAIN & STEPHENS STATE PARKS Allamuchy Mountain and Stephens State Parks contain 28 marked trails providing access to diverse landscapes for walking, hiking, biking, bird-watching,

More information

Landscapes in the UK: Glaciation 1. Extent of ice cover across the UK during the last ice age.

Landscapes in the UK: Glaciation 1. Extent of ice cover across the UK during the last ice age. Landscapes in the UK: Glaciation 1. Extent of ice cover across the UK during the last ice age. Key idea: Ice was a powerful force in shaping the landscape of the UK. In the past the climate has got colder

More information

Geologic Trips, Sierra Nevada

Geologic Trips, Sierra Nevada ISBN 0-9661316-5-7 GeoPress Excerpt from Geologic Trips, Sierra Nevada by Ted Konigsmark All rights reserved. No part of this book may be reproduced without written permission, except for critical articles

More information

A trip to Steindalen. - geology and landscape on the way to the glacier. Geoffrey D. Corner

A trip to Steindalen. - geology and landscape on the way to the glacier. Geoffrey D. Corner A TRIP TO STEINDALEN Excursion guide Please take this with you on your trip, but don t leave it behind as litter. A trip to Steindalen - geology and landscape on the way to the glacier A part of Geologiskolen,

More information

October 18, SWBAT identify key features on topographic maps SWBAT identify landforms on topographic maps

October 18, SWBAT identify key features on topographic maps SWBAT identify landforms on topographic maps October 18, 2016 Aims: SWBAT identify key features on topographic maps SWBAT identify landforms on topographic maps Agenda 1. Do Now 2. Class Notes 3. Guided Practice 4. Independent Practice 5. Practicing

More information

5 MAP SPECIFICATION FOR SKI-ORIENTEERING

5 MAP SPECIFICATION FOR SKI-ORIENTEERING 5 MAP SPECIFICATION FOR SKI-ORIENTEERING 5.1 General Maps for ski orienteering are based on the specifications for foot-orienteering maps. However in order to meet the specific requirements put on the

More information

Kit Carson-Challenger Ridge Trail Project Annual Performance Report-2014 October 22, 2014

Kit Carson-Challenger Ridge Trail Project Annual Performance Report-2014 October 22, 2014 1 Kit Carson-Challenger Ridge Trail Project Annual Performance Report-2014 October 22, 2014 Willow Lake and Kit Carson Peak 2 SUMMARY The Rocky Mountain Field Institute began Phase 1 of a multi-phase,

More information

Geography 120, Instructor: Chaddock In Class 13: Glaciers and Icecaps Name: Fill in the correct terms for these descriptions: Ablation zone: n zne:

Geography 120, Instructor: Chaddock In Class 13: Glaciers and Icecaps Name: Fill in the correct terms for these descriptions: Ablation zone: n zne: Geography 120, Instructor: Chaddock In Class 13: Glaciers and Icecaps Name: Fill in the correct terms for these descriptions: Ablation zone: The area of a glacier where mass is lost through melting or

More information

Exam Review. Part 3- Deserts, Glaciers, and maps

Exam Review. Part 3- Deserts, Glaciers, and maps Exam Review Part 3- Deserts, Glaciers, and maps What causes a desert? Lots of sand Vegetation holds the arms Star Dunes- Star dunes form only in places where wind blows from varied directions over the

More information

2012 Oregon State Science Olympiad. B-Division Road Scholar Event National Wildlife Refuge Site Selection. Student Participants:

2012 Oregon State Science Olympiad. B-Division Road Scholar Event National Wildlife Refuge Site Selection. Student Participants: 2012 Oregon State Science Olympiad B-Division Road Scholar Event National Wildlife Refuge Site Selection Student Participants: School/Team: To answer the questions you will need a pencil, ruler, protractor,

More information

SHELTERS, OUTDOOR SURVIVAL AND ORIENTEERING REVIEW PAD30

SHELTERS, OUTDOOR SURVIVAL AND ORIENTEERING REVIEW PAD30 SHELTERS, OUTDOOR SURVIVAL AND ORIENTEERING REVIEW PAD30 Before you Build your shelter you should consider the following: Hours Before Dark Close to dark = build something easy Season Summer = Higher ground

More information

Section 2 North Slope Ecoregions and Climate Scenarios

Section 2 North Slope Ecoregions and Climate Scenarios Section 2 North Slope Ecoregions and Climate Scenarios North Slope Ecoregions The geographic/ecological scope of the workshop will be freshwater and terrestrial systems of the North Slope of Alaska, with

More information

Glaciers and Periglaciers

Glaciers and Periglaciers Glaciers and Periglaciers Chapter 9, page 132 Glaciation!1836 Louis Agassiz theorized that parts of Europe and North America were covered by huge ice sheets.!known as the Pleistocene Ice Ages Why do we

More information

4.1 Landforms. Note: dimensions are specified in mm at the scale of 1: All drawings are at 1:7 500 for clarity only.

4.1 Landforms. Note: dimensions are specified in mm at the scale of 1: All drawings are at 1:7 500 for clarity only. 4.1 Landforms Note: dimensions are specified in mm at the scale of 1:15 000. All drawings are at 1:7 500 for clarity only. OM = Outside measure IM = Inside measure CC = Centre to centre 0.2 0.4 OM 0.4

More information

IMPORTANT DEFINITIONS DEFINITIONS FROM TOPO MAPS

IMPORTANT DEFINITIONS DEFINITIONS FROM TOPO MAPS IMPORTANT DEFINITIONS DEFINITIONS FROM TOPO MAPS 1. REPRESENTATIVE FRACTION (RF): It is the ratio between the distances on the map to its corresponding distance on actual ground. The RF on this map is

More information

DEPARTMENT: CIVIL ENGINEERING SEMESTER: III SUBJECT CODE / Name: CE2303/ Railway, Airport and Harbors Engineering 2 MARK QUESTIONS AND ANSWERS

DEPARTMENT: CIVIL ENGINEERING SEMESTER: III SUBJECT CODE / Name: CE2303/ Railway, Airport and Harbors Engineering 2 MARK QUESTIONS AND ANSWERS DEPARTMENT: CIVIL ENGINEERING SEMESTER: III SUBJECT CODE / Name: CE2303/ Railway, Airport and Harbors Engineering 2 MARK QUESTIONS AND ANSWERS 1.Define wind Coverage (AUC NOV/DEC 2010),(AUC NOV/DEC 2011)

More information

MINIMUM FLIGHT ALTITUDES

MINIMUM FLIGHT ALTITUDES MINIMUM FLIGHT ALTITUDES 1. Introduction Minimum flight altitudes are created first to ensure safety, awareness and adequate radio navigation reception for aircraft flying at the same time in specific

More information

Region 1 Piney Woods

Region 1 Piney Woods Region 1 Piney Woods Piney Woods 1. This ecoregion is found in East Texas. 2. Climate: average annual rainfall of 36 to 50 inches is fairly uniformly distributed throughout the year, and humidity and temperatures

More information

Teacher s Guide For. Glaciers

Teacher s Guide For. Glaciers Teacher s Guide For Glaciers For grade 7 - College Program produced by Centre Communications, Inc. for Ambrose Video Publishing, Inc. Executive Producer William V. Ambrose Teacher's Guide by Mark Reeder

More information

Trail Assessment Report

Trail Assessment Report Trail Assessment Report Trail Options for the Bear Creek Canyon located in Pikes Peak Ranger District, Pike National Forest and on Colorado Springs Utility Lands Due to the presence of a unique species

More information

宇宙から見た中央アジア, パミールのフェドチェンコ氷河の特徴

宇宙から見た中央アジア, パミールのフェドチェンコ氷河の特徴 Geographical Studies 宇宙から見た中央アジア, パミールのフェドチェンコ氷河の特徴 * 岩田修二 キーワード 要旨 FG Shan, where precipitation is greatest in summer. 3 General configuration of Fedchenko Glacier (1) Plan form of the glacial basin Fedchenko

More information

Mearns Castle High School. Geography Department. Glaciated Landscapes

Mearns Castle High School. Geography Department. Glaciated Landscapes Mearns Castle High School Geography Department Glaciated Landscapes Lesson One: Location of Glaciated Uplands in the British Isles The Ice Age in Britain began about 1,000,000 years ago and lasted until

More information

DR1. OFFSET MEASUREMENTS OF DISPLACED FEATURES ALONG THE DENALI FAULT AND ERROR CALCULATIONS

DR1. OFFSET MEASUREMENTS OF DISPLACED FEATURES ALONG THE DENALI FAULT AND ERROR CALCULATIONS DR1. OFFSET MEASUREMETS OF DISPLACED FEATURES ALOG THE DEALI FAULT AD ERROR CALCULATIOS The Denali fault trace is marked by a red line in all the photos. Black and white air photos were taken during August

More information

traverse from the outwash plain terminal moraine and recessional (Sag Harbor, Greenport and Southold

traverse from the outwash plain terminal moraine and recessional (Sag Harbor, Greenport and Southold 1 27 DEGLACIATION OF EASTERN LONG ISLAND: THE TERMINAL MORAINE. RECESSIONAL MORAINES. OUTWASH PLAINS. PROGLACIAL LAKES AND MELTWATER CHANNELS LES SIRKIN. EARTH SCIENCE. ADELPHI UNIVERSITY. GARDEN CITY.

More information

United States Department of the Interior National Park Service. Boundary Expansion Listed in National Register January 11, 2017

United States Department of the Interior National Park Service. Boundary Expansion Listed in National Register January 11, 2017 NPS Form 10900-a (Rev. 8/2002) OMB No. 10240018 United States Department of the Interior National Park Service Boundary Expansion Listed in National Register January 11, 2017 National Register of Historic

More information

SYNOPSIS WEATHER AND SNOWPACK

SYNOPSIS WEATHER AND SNOWPACK Peak 6996 Avalanche Fatality Incident Report Glacier National Park, MT Date of Avalanche: 31 March 2010 Date of Investigation: 2 April 2010 Investigation Team: Erich Peitzsch (USGS), Ted Steiner (Chugach

More information

EXPLORING EARTH S SURFACE. Lesson 4

EXPLORING EARTH S SURFACE. Lesson 4 EXPLORING EARTH S SURFACE Lesson 4 Introduction Lewis and Clark In 1804, an expedition set out from near Saint Louis to explore the land between the Mississippi River and the Pacific Ocean, The United

More information

Q: What is a period of time whereby the average global temperature has decreased? Q: What is a glacier?

Q: What is a period of time whereby the average global temperature has decreased? Q: What is a glacier? Q: What is a glacier? A: A large sheet of ice which lasts all year round. Q: What is a period of time whereby the average global temperature has decreased? A: A glacial. Q: What is an interglacial? Q:

More information

Electronic Terrain and Obstacle Data

Electronic Terrain and Obstacle Data International Civil Aviation Organization Electronic Terrain and Obstacle Data David Lewtas Chief, Aeronautical Information Unit (MET/AIM) 24 November 2010 ICAO CAR AIM Seminar Kingston, Jamaica 22-24

More information

Dynamic Planet C Test

Dynamic Planet C Test Northern Regional: January 19 th, 2019 Dynamic Planet C Test Name(s): Team Name: School Name: Team Number: Rank: Score: Dynamic Planet B/C Glaciers (87 total points) Multiple choice/fill in the blank (23

More information