Landforms and Landscapes
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Physical Geography of Southeast Asia
Physical Geography of Southeast Asia Creating an Annotated Sketch Map of Southeast Asia By Michelle Crane Teacher Consultant for the Texas Alliance for Geographic Education Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 Guiding Question (5 min.) . What processes are responsible for the creation and distribution of the landforms and climates found in Southeast Asia? Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 2 Draw a sketch map (10 min.) . This should be a general sketch . do not try to make your map exactly match the book. Just draw the outline of the region . do not add any features at this time. Use a regular pencil first, so you can erase. Once you are done, trace over it with a black colored pencil. Leave a 1” border around your page. Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 3 Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 4 Looking at your outline map, what two landforms do you see that seem to dominate this region? Predict how these two landforms would affect the people who live in this region? Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 5 Peninsulas & Islands . Mainland SE Asia consists of . Insular SE Asia consists of two large peninsulas thousands of islands . Malay Peninsula . Label these islands in black: . Indochina Peninsula . Sumatra . Label these peninsulas in . Java brown . Sulawesi (Celebes) . Borneo (Kalimantan) . Luzon Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 6 Draw a line on your map to indicate the division between insular and mainland SE Asia. -
Part 629 – Glossary of Landform and Geologic Terms
Title 430 – National Soil Survey Handbook Part 629 – Glossary of Landform and Geologic Terms Subpart A – General Information 629.0 Definition and Purpose This glossary provides the NCSS soil survey program, soil scientists, and natural resource specialists with landform, geologic, and related terms and their definitions to— (1) Improve soil landscape description with a standard, single source landform and geologic glossary. (2) Enhance geomorphic content and clarity of soil map unit descriptions by use of accurate, defined terms. (3) Establish consistent geomorphic term usage in soil science and the National Cooperative Soil Survey (NCSS). (4) Provide standard geomorphic definitions for databases and soil survey technical publications. (5) Train soil scientists and related professionals in soils as landscape and geomorphic entities. 629.1 Responsibilities This glossary serves as the official NCSS reference for landform, geologic, and related terms. The staff of the National Soil Survey Center, located in Lincoln, NE, is responsible for maintaining and updating this glossary. Soil Science Division staff and NCSS participants are encouraged to propose additions and changes to the glossary for use in pedon descriptions, soil map unit descriptions, and soil survey publications. The Glossary of Geology (GG, 2005) serves as a major source for many glossary terms. The American Geologic Institute (AGI) granted the USDA Natural Resources Conservation Service (formerly the Soil Conservation Service) permission (in letters dated September 11, 1985, and September 22, 1993) to use existing definitions. Sources of, and modifications to, original definitions are explained immediately below. 629.2 Definitions A. Reference Codes Sources from which definitions were taken, whole or in part, are identified by a code (e.g., GG) following each definition. -
Owyhee High Plateau Major Land Resource Area (MLRA)
MLRA 25 – Owyhee High Plateau (Utah portion) MLRA 25 – Owyhee High Plateau (Utah portion) Ecological Zone Upland Mountain High Mountain Subalpine Precipitation (inches) 12-17 inches 16-22 inches 16-22 inches 20-27 inches Elevation 5,000 -7,000 6,000 – 8,600 8,000-9,000 9,000 - 9,300 Soil Moisture Regime Typic Xeric Typic Xeric Typic Xeric Udic Soil Temp Regime Mesic Frigid Cryic Cryic Freeze free Days 80-120 60 - 90 30 - 40 20 -35 Mountain mahogany, Sagebrushes and Mountain big Aspen, Mountain big Subalpine Fir, browse Notes sagebrush sagebrush Subalpine sagebrush 300 – 500 and 1,100-2,100 and 2,400-2,500 lbs/ac 800 – 1000 lbs.ac 400-600 lbs/ac All values in this table are approximate and should be used as guidelines. Different combinations of temperature, precipitation and soil type can place an ecological site into different zones. Major Land Resource Area (MLRA) D25 D25 - Owyhee High Plateau E47A - and Ui D28A 030 60 120 Miles Great Salt 1:3,000,000 Lake Area 25—Owyhee High Plateau This area is in Nevada (52 percent),Idaho (29 percent), Oregon (16 percent), and Utah (3 percent). It makes up about 28,930 square miles (74,960 square kilometers). The city of Elko, Nevada, which is along Interstate 80, occurs in this MLRA. The Humboldt-Toiyabe and Sawtooth National Forests and numerous wilderness study areas also occur in this MLRA. Most of the wilderness study areas are in the high desert canyon lands of southern Idaho. The Duck Valley, South Fork, Ruby Valley, and Te-Moak Indian Reservations are in this area. -
A Guide to the Geology of Rocky Mountain National Park, Colorado
A Guide to the Geology of ROCKY MOUNTAIN NATIONAL PARK COLORADO For sale by the Superintendent of Documents, Washington, D. C. Price 15 cents A Guide to the Geology of ROCKY MOUNTAIN NATIONAL PARK [ COLORADO ] By Carroll H. Wegemann Former Regional Geologist, National Park Service UNITED STATES DEPARTMENT OF THE INTERIOR HAROLD L. ICKES, Secretary NATIONAL PARK SERVICE . NEWTON B. DRURY, Director UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1944 Table of Contents PAGE INTRODUCTION in BASIC FACTS ON GEOLOGY 1 THE OLDEST ROCKS OF THE PARK 2 THE FIRST MOUNTAINS 3 The Destruction of the First Mountains 3 NATURE OF PALEOZOIC DEPOSITS INDICATES PRESENCE OF SECOND MOUNTAINS 4 THE ROCKY MOUNTAINS 4 Time and Form of the Mountain Folding 5 Erosion Followed by Regional Uplift 5 Evidences of Intermittent Uplift 8 THE GREAT ICE AGE 10 Continental Glaciers 11 Valley Glaciers 11 POINTS OF INTEREST ALONG PARK ROADS 15 ROAD LOGS 18 Thompson River Entrance to Deer Ridge Junction 18 Deer Ridge Junction to Fall River Pass via Fall River .... 20 Fall River Pass to Poudre Lakes 23 Trail Ridge Road between Fall River Pass and Deer Ridge Junction 24 Deer Ridge Junction to Fall River Entrance via Horseshoe Park 29 Bear Lake Road 29 ILLUSTRATIONS LONGS PEAK FROM BEAR LAKE Front and back covers CHASM FALLS Inside back cover FIGURE PAGE 1. GEOLOGIC TIME SCALE iv 2. LONGS PEAK FROM THE EAST 3 3. PROFILE SECTION ACROSS THE ROCKY MOUNTAINS 5 4. ANCIENT EROSIONAL PLAIN ON TRAIL RIDGE 6 5. ANCIENT EROSIONAL PLAIN FROM FLATTOP MOUNTAIN ... 7 6. VIEW NORTHWEST FROM LONGS PEAK 8 7. -
Landform Clue Hill a Naturally Raised Area of Land, Not As High Or Craggy
Landform Clue a naturally raised area of land, not as high or craggy as a mountain http://baytrail.abag.ca.gov/vtour/map4/access/CyteHils/Cyte Hils1.htm Hill a low area of land between hills or mountains, typically with a river or stream flowing through it http://pubs.usgs.gov/of/2004/1216/h/h.html Valley a large natural elevation of the earth's surface rising abruptly from the surrounding level; a large steep hill http://www.nps.gov/lavo/planyourvisit/hiking_brokeoff_mou ntain.htm Mountain a large area of flat land with few trees http://geomaps.wr.usgs.gov/parks/province/intplain.html Plain a piece of land surrounded by water http://www.nytimes.com/2012/08/22/world/asia/dispute- over-islands-reflect-japanese-fear-of-chinas-rise.html?_r=0 Island a very large expanse of sea, in particular, each of the main areas into which the sea is divided geographically http://www.nasa.gov/jpl/oco2/quikscat-rapidscat- 20140619/#.U-AA3-NdVik Ocean a large natural stream of water flowing in a channel to the sea, a lake, or another such stream http://www.blm.gov/or/districts/roseburg/recreation/wild_a nd_scenic_river/ River a large body of water surrounded by land http://www.nsf.gov/news/news_summ.jsp?cntn_id=119359 Lake a small body of still water formed naturally or by hollowing or embanking http://www.fairfaxcounty.gov/dpwes/watersheds/ponds.htm Pond a dry, barren area of land, especially one covered with sand, that is characteristically desolate, waterless, and without vegetation http://www.oregon.gov/dsl/DO/Pages/map_bend.aspx Desert a mountain or hill, typically conical, having a crater or vent through which lava, rock fragments, hot vapor, and gas are being or have been erupted from the earth's crust http://hvo.wr.usgs.gov/volcanowatch/archive/2009/09_07_23.html Volcano an area of relatively level high ground http://www.nature.nps.gov/geology/tour/cplateau.cfm Plateau . -
Geography of Coachella Valley Curriculum Guide
Exploring the Geography of Coachella Valley A Curriculum Guide for Grade 3, Standard 1 Table of Contents Acknowledgements i Table of Contents 1 Unit Overview 2 Common Core State Standards: Reading Standards for Information Text 2 Academic History-Social Science Content Standards for Grade 3 2 Kindergarten to Grade 5 Historical and Social Sciences Analysis Skills 3 Focus Questions and Assessment 3 Geography of the Coachella Valley – Background Information for the Teacher 4 Supplies Needed 6 Lesson 1: Location Match-Up 8 Lesson 2: Looking at Earth 11 Lesson 3: Where I Live 14 Lesson 4: Geographic Terms and Definitions 16 Lesson 5: Right Here in the Coachella Valley 20 Lesson 6: Geographical Features of Coachella Valley 24 Lesson 7: Human-Made Features of Coachella Valley 29 Lesson 8: Communityville 31 Extended Activities 39 Unit 3.1 Exploring the Geography of Coachella Valley Page 1 Unit Overview: Exploring the Geography of Coachella Valley __________________________________________________________________________________ Description of the Unit The unit begins with Matching Vocabulary Cards that help students learn the name of their city, county, state, nation, continent, hemisphere, and planet. In Lesson 2, students use a variety of maps to find these geographic locations while in Lesson 3 they construct a “Flip-Book” titled “Where I Live.” In Lessons 4 and 5, students study geographic terms and definitions and use local maps to identify key geographical features in the Coachella Valley. In Lessons 5 and 6, students construct a map of the Coachella Valley and identify key geographical features and human-made features. The focus in Lesson 8 is on how the natural environment of “Communityville” has been changed over time. -
The Physical Features of Europe 6Th Grade World Studies LABEL the FOLLOWING FEATURES on the MAP
The Physical Features of Europe 6th Grade World Studies LABEL THE FOLLOWING FEATURES ON THE MAP: Danube River Rhine River English Channel Physical Mediterranean Sea Features European Plain Alps Pyrenees Ural Mountains Iberian Peninsula Scandinavian Peninsula Danube River . The Danube is Europe's second-longest river, after the Volga River. It is located in Central and Eastern Europe. Rhine River . Begins in the Swiss canton of Graubünden in the southeastern Swiss Alps then flows through the Rhineland and eventually empties into the North Sea in the Netherlands. English Channel . The English Channel, also called simply the Channel, is the body of water that separates southern England from northern France, and links the southern part of the North Sea to the Atlantic Ocean. Mediterranean Sea . The Mediterranean Sea is a sea connected to the Atlantic Ocean, surrounded by the Mediterranean Basin and almost completely enclosed by land: on the north by Southern Europe and Anatolia, on the south by North Africa, and on the east by the Levant. European Plain . The European Plain or Great European Plain is a plain in Europe and is a major feature of one of four major topographical units of Europe - the Central and Interior Lowlands. Alps . The Alps are the highest and most extensive mountain range system that lies entirely in Europe Pyrenees . The Pyrenees mountain range separates the Iberian Peninsula from the rest of Europe. Ural Mountains . The Ural Mountains, or simply the Urals, are a mountain range that runs approximately from north to south through western Russia, from the coast of the Arctic Ocean to the Ural River and northwestern Kazakhstan. -
Sunshine Coast and Hinterland National Parks
Journey guide Sunshine Coast and Hinterland national parks Refresh naturally Contents Parks at a glance ............................................................................... 2 Glass House Mountains National Park ............................... 14–15 Welcome .............................................................................................3 Kondalilla National Park ..............................................................16 Be refreshed .......................................................................................3 Mapleton Falls National Park ..................................................... 17 Map of Sunshine Coast and Hinterland ....................................... 4 Mapleton National Park.........................................................18–19 Publication maps legend ................................................................. 4 Conondale National Park ..................................................... 20–21 Plan your getaway .............................................................................5 Imbil State Forest ................................................................. 20–21 Choose your adventure ............................................................... 6–7 Jimna State Forest ................................................................ 22–23 Track and trail classifications ......................................................... 7 Amamoor State Forest ......................................................... 22–23 Noosa National Park ....................................................................8–9 -
Surrounded by Mountains
Surrounded by Mountains he Gallatin Valley is one of the most picturesque and Rockies into the jagged peaks we see today. Over the last 50 Geo-Facts: agriculturally productive valleys in Montana. From million years, western Montana experienced several phases of • From the summit of Sacagawea Peak (9,596 ft.) in the northern here, you can see four prominent Montana mountain regional extension and block-faulting, resulting in the creation Bridger Range, you can see even more ranges in a spectacular Tranges: the Bridger Range (east), Gallatin Range (south), of modern Basin-and-Range topography. The crest of the 360o panorama of southwest Montana. Spanish Peaks (southwest), and the Big Belt Mountains Bridger Range arch slowly down-dropped one earthquake at a • A pluton is an intrusive igneous rock body that crystallized from (north). Each range has its own unique geology and topography. time to form the modern Gallatin Valley. Thick layers of mid- magma slowly cooling below the surface of the Earth. Its name The high peaks of the Gallatin Range are carved from volcanic and late Cenozoic sedimentary rocks and more recent stream comes from Pluto, the Roman god of the underworld. rocks and volcanic-derived mudflows that erupted during the deposits have been deposited in the Gallatin Valley, producing • One of the richest gold strikes in Montana history was made at Eocene, approximately 45 million years ago. The Spanish Peaks the fertile landscape that Native Americans called the “Valley of Confederate Gulch in the Big Belt Mountains in 1864. Miners expose metamorphic rocks that date back to the Earth’s early Flowers” – the Gallatin Valley. -
European Mountain Ranges
European Mountain Ranges The Pyrenees The Pyrenees are a mountain range between France and Spain. They stretch 270 miles (435km) from the Bay of Biscay to the Mediterranean Sea. The highest peak is Pico de Aneto, which is 3,404 metres high. There are two rail lines which cross the Pyrenees. There are also a number of roads, some of which use tunnels to pass through the mountains. In the winter months, these roads are often closed due to bad weather. The Alps The Alps stretch from Slovenia to Austria. They pass through: • Italy • Switzerland • France • Germany. People come to see the wonderful scenery, to go mountaineering, hiking, mountain biking and even paragliding. In the winter months, people mainly visit to ski or snowboard. The highest peak here is Mont Blanc (White Mountain) which stands at 4,810 metres in height. It is the highest peak in Western Europe. A nearby town named Chamonix was where the first ever Winter Olympics took place in 1924. The Alps play an important role when it comes to the weather too. They act as a wind barrier meaning that south of the Alps is slightly drier and warmer. Page 1 of 4 visit twinkl.com European Mountain Ranges The Carpathians This huge mountain range stretches through seven different countries. They are: • the Czech Republic • Slovakia • Poland • Hungary • Ukraine • Romania • Serbia The mountains are home to 18 million people as well as animals such as wolves, bears and lynx. The Apennines This mountain range runs straight down the centre of Italy. It ends on the island of Sicily. -
Reviewing the Status of Our Natural Assets in South East Queensland: Have Your Say!
Reviewing the status of our natural assets in South East Queensland: Have your say! We are asking your input as we conduct a review of the condition of natural assets across South East Queensland (SEQ). Please Your opinion will feed into the broadscale analysis we are conducting, review these which will feed into the re-invigorated Natural Resource Management Plan (NRM Plan) and targets across the region. two maps for Below you will see two maps. Please look at them and let us know if your area you think they are accurate and whether anything is missing. and have your The first map represents the status of natural assets across the Brisbane local government area. The second is a high-level summary of threats say! across the SEQ region more broadly. Step 1: View natural assets map CLICK HERE FOR LARGER Step 2: View risks map ASSETS MAP CLICK HERE FOR LARGER RISK MAP Step 3: Give your feedback CLICK HERE TO GIVE YOUR Please provide FEEDBACK your feedback Turn over for more information about why this is such an important1 project for building the resilience of our growing region. South East Queensland’s NRM Plan: South East Queensland’s Focussing action to protect our natural assets natural assets: Under pressure The NRM Plan for South East Queensland is the region’s The strong population growth forecasted for South East Queensland in the coming decades plan to guide the protection and enhancement of our which will put significant additional pressures on region’s natural assets. our natural assets, many of which are already under threat. -
The Glass House Mountains
The Glass House Mountains Jutting into the air like shards of glass, the Glass House Mountains form a distinctive backdrop to the Sunshine Coast. This stunningly volcanic landscape holds a special significance in Indigenous legend and culture, with each of the mountains representing a member of a family, and their spirits dominating the area. Although climbing many of the mountains is only for the experienced, there are a number of easy to moderate tracks in the area accessible to a wider range of walkers. The circuit around Mount Tibrogargan passes through shady forest, and offers the chance to learn about, and view, several of the other mountains. The short hike up Wild Horse Mountain is rewarded with expansive views. For something a bit different, the Soldier’s Walk at Beerburrum explores the history of the town as a settlement area for retired soldiers, while Ewen Maddock Dam is a peaceful haven for bird and nature lovers with a walk that takes in lakes and forest. 141 27 Ewen Maddock 27 Ewen Maddock Dam Walk directions Dam Start at the dam-side 1 car park where there are picnic benches, toilets, The sounds of wind rustling in gum a BBQ and a children’s trees and melodic birdsong follow At a glance play park. There is a notice you on this dam-side walk on the Grade: Moderate board here detailing the 15 kilometres of tracks in the northern fringes of the Glass House Time: 3.5 hrs area. Much of your walk Mountains. The first half of the walk Distance: 8.5 km return follows the Tallowood track tracks the edge of the lake while the Conditions: Shady, path muddy which is listed as number second half goes through a mixture after rain 3.