Match the Names Below with Their Locations on the Map by Writing the Correct Letter in the Blank. ___1. Arctic Lowlands ___
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Canada GREENLAND 80°W
DO NOT EDIT--Changes must be made through “File info” CorrectionKey=NL-B Module 7 70°N 30°W 20°W 170°W 180° 70°N 160°W Canada GREENLAND 80°W 90°W 150°W 100°W (DENMARK) 120°W 140°W 110°W 60°W 130°W 70°W ARCTIC Essential Question OCEANDo Canada’s many regional differences strengthen or weaken the country? Alaska Baffin 160°W (UNITED STATES) Bay ic ct r le Y A c ir u C k o National capital n M R a 60°N Provincial capital . c k e Other cities n 150°W z 0 200 400 Miles i Iqaluit 60°N e 50°N R YUKON . 0 200 400 Kilometers Labrador Projection: Lambert Azimuthal TERRITORY NUNAVUT Equal-Area NORTHWEST Sea Whitehorse TERRITORIES Yellowknife NEWFOUNDLAND AND LABRADOR Hudson N A Bay ATLANTIC 140°W W E St. John’s OCEAN 40°W BRITISH H C 40°N COLUMBIA T QUEBEC HMH Middle School World Geography A MANITOBA 50°N ALBERTA K MS_SNLESE668737_059M_K.ai . S PRINCE EDWARD ISLAND R Edmonton A r Canada legend n N e a S chew E s kat Lake a as . Charlottetown r S R Winnipeg F Color Alts Vancouver Calgary ONTARIO Fredericton W S Island NOVA SCOTIA 50°WFirst proof: 3/20/17 Regina Halifax Vancouver Quebec . R 2nd proof: 4/6/17 e c Final: 4/12/17 Victoria Winnipeg Montreal n 130°W e NEW BRUNSWICK Lake r w Huron a Ottawa L PACIFIC . t S OCEAN Lake 60°W Superior Toronto Lake Lake Ontario UNITED STATES Lake Michigan Windsor 100°W Erie 90°W 40°N 80°W 70°W 120°W 110°W In this module, you will learn about Canada, our neighbor to the north, Explore ONLINE! including its history, diverse culture, and natural beauty and resources. -
Mountain Goat Population Ecology and Habitat Use Along the Juneau Access Road Corridor, Alaska
Final Wildlife Research Report, ADFG/DWC/WRR-2012-02 Mountain goat population ecology and habitat use along the Juneau Access road corridor, Alaska Kevin S. White, David P. Gregovich, Grey W. Pendleton, Neil L. Barten, Ryan Scott, Anthony Crupi and Doug N. Larsen ©2005 ADFG/photo by Kevin White May 2012 Alaska Department of Fish and Game Division of Wildlife Conservation Final Wildlife Research Reports are fi nal reports detailing the objectives, methods, data collected and fi ndings of a particular research project undertaken by ADF&G Division of Wildlife Conservation staff and partners. They are written to provide broad access to information obtained through the project. While these are fi nal reports, further data analysis may result in future adjustments to the conclusions. Please contact the author(s) prior to citing material in these reports. These reports are professionally reviewed by research staff in the Division of Wildlife Conservation. They are provided a number for internal tracking purposes. This Wildlife Research Report was reviewed and approved for publication by Rod Flynn, Reseach Coodinator for Region 1, for the Division of Wildlife Conservation. Wildlife Research Reports are available from the Alaska Department of Fish and Game’s Division of Wildlife Conservation, PO Box 115526, Juneau, Alaska 99811-5526; phone (907) 465-4190; email: dfg.dwc.publications@ alaska.gov; website: www.adfg.alaska.gov. The report may also be accessed through most libraries, via interlibrary loan from the Alaska State Library or the Alaska Resources Library and Information Service (www.arlis.org). This document should be cited as: White, K. S., D. -
Climate and Vegetation • Almost Every Type of Climate Is Found in the 50 United States Because They Extend Over Such a Large Area North to South
123-126-Chapter5 10/16/02 10:16 AM Page 123 Main Ideas Climate and Vegetation • Almost every type of climate is found in the 50 United States because they extend over such a large area north to south. • Canada’s cold climate is related to its location in the far northern latitudes. A HUMAN PERSPECTIVE A little gold and bitter cold—that is what Places & Terms thousands of prospectors found in Alaska and the Yukon Territory dur- permafrost ing the Klondike gold rushes of the 1890s. Most of these fortune prevailing westerlies hunters were unprepared for the harsh climate and inhospitable land of Everglades the far north. Winters were long and cold, the ground frozen. Ice fogs, blizzards, and avalanches were regular occurrences. You could lose fin- Connect to the Issues gers and toes—even your life—in the cold. But hardy souls stuck it out. urban sprawl The rapid Legend has it that one miner, Bishop Stringer, kept himself alive by boil- spread of urban sprawl has led US & CANADA ing his sealskin and walrus-sole boots and then drinking the broth. to the loss of much vegetation in both the United States and Canada. Shared Climates and Vegetation The United States and Canada have more in common than just frigid winter temperatures where Alaska meets northwestern Canada. Other shared climate and vegetation zones are found along their joint border at the southern end of Canada and the northern end of the United States. If you look at the map on page 125, you will see that the United MOVEMENT The snowmobile States has more climate zones than Canada. -
Challenges in the Paleoclimatic Evolution of the Arctic and Subarctic Pacific Since the Last Glacial Period—The Sino–German
challenges Concept Paper Challenges in the Paleoclimatic Evolution of the Arctic and Subarctic Pacific since the Last Glacial Period—The Sino–German Pacific–Arctic Experiment (SiGePAX) Gerrit Lohmann 1,2,3,* , Lester Lembke-Jene 1 , Ralf Tiedemann 1,3,4, Xun Gong 1 , Patrick Scholz 1 , Jianjun Zou 5,6 and Xuefa Shi 5,6 1 Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung Bremerhaven, 27570 Bremerhaven, Germany; [email protected] (L.L.-J.); [email protected] (R.T.); [email protected] (X.G.); [email protected] (P.S.) 2 Department of Environmental Physics, University of Bremen, 28359 Bremen, Germany 3 MARUM Center for Marine Environmental Sciences, University of Bremen, 28359 Bremen, Germany 4 Department of Geosciences, University of Bremen, 28359 Bremen, Germany 5 First Institute of Oceanography, Ministry of Natural Resources, Qingdao 266061, China; zoujianjun@fio.org.cn (J.Z.); xfshi@fio.org.cn (X.S.) 6 Pilot National Laboratory for Marine Science and Technology, Qingdao 266061, China * Correspondence: [email protected] Received: 24 December 2018; Accepted: 15 January 2019; Published: 24 January 2019 Abstract: Arctic and subarctic regions are sensitive to climate change and, reversely, provide dramatic feedbacks to the global climate. With a focus on discovering paleoclimate and paleoceanographic evolution in the Arctic and Northwest Pacific Oceans during the last 20,000 years, we proposed this German–Sino cooperation program according to the announcement “Federal Ministry of Education and Research (BMBF) of the Federal Republic of Germany for a German–Sino cooperation program in the marine and polar research”. Our proposed program integrates the advantages of the Arctic and Subarctic marine sediment studies in AWI (Alfred Wegener Institute) and FIO (First Institute of Oceanography). -
Description of the Ecoregions of the United States
(iii) ~ Agrl~:::~~;~":,c ullur. Description of the ~:::;. Ecoregions of the ==-'Number 1391 United States •• .~ • /..';;\:?;;.. \ United State. (;lAn) Department of Description of the .~ Agriculture Forest Ecoregions of the Service October United States 1980 Compiled by Robert G. Bailey Formerly Regional geographer, Intermountain Region; currently geographer, Rocky Mountain Forest and Range Experiment Station Prepared in cooperation with U.S. Fish and Wildlife Service and originally published as an unnumbered publication by the Intermountain Region, USDA Forest Service, Ogden, Utah In April 1979, the Agency leaders of the Bureau of Land Manage ment, Forest Service, Fish and Wildlife Service, Geological Survey, and Soil Conservation Service endorsed the concept of a national classification system developed by the Resources Evaluation Tech niques Program at the Rocky Mountain Forest and Range Experiment Station, to be used for renewable resources evaluation. The classifica tion system consists of four components (vegetation, soil, landform, and water), a proposed procedure for integrating the components into ecological response units, and a programmed procedure for integrating the ecological response units into ecosystem associations. The classification system described here is the result of literature synthesis and limited field testing and evaluation. It presents one procedure for defining, describing, and displaying ecosystems with respect to geographical distribution. The system and others are undergoing rigorous evaluation to determine the most appropriate procedure for defining and describing ecosystem associations. Bailey, Robert G. 1980. Description of the ecoregions of the United States. U. S. Department of Agriculture, Miscellaneous Publication No. 1391, 77 pp. This publication briefly describes and illustrates the Nation's ecosystem regions as shown in the 1976 map, "Ecoregions of the United States." A copy of this map, described in the Introduction, can be found between the last page and the back cover of this publication. -
Chapter 5: Canada
156-164 U2 CH05 S1 TWIP-860976 3/22/04 10:49 PM Page 156 pter ha C 55 CanadaCanada Social Studies To learn more about Canada’s people Chapter Overview Visit The World and Its and places, view The World and Its People Web site at twip.glencoe.com and People Chapter 5 video. click on Chapter 5—Chapter Overviews to preview information about Canada. 156 156-164 U2 CH05 S1 TWIP-860976 3/22/04 10:49 PM Page 157 Compare-Contrast Make this foldable to help you analyze the similarities and differences between the landforms, climate, and cultures of northern and southern Canada. Step 1 Mark the midpoint of the side Step 2 Turn the paper and fold the edge of a sheet of paper. outside edges in to touch at the midpoint. Draw a mark at the midpoint. Step 3 Turn and label your foldable as shown. Northern Canada Southern Canada Reading and Writing As you read the chapter, collect and write information under the appropriate tab that will help you compare and contrast northern and southern Canada. Sharing a Border The boundary line between Canada and the United States forms the longest unprotected border in the world. Citizens of these countries have been allowed to travel freely across the border, which is symbolic of the free trade between these nations. ▼ ▼ Vancouver, British Columbia 156-164 U2 CH05 S1 TWIP-860976 3/22/04 10:50 PM Page 158 Guide to Reading Main Idea 11 A Resource-Rich Canada is a vast country with many landforms and resources. -
British Columbia Coastal Range and the Chilkotins
BRITISH COLUMBIA COASTAL RANGE AND THE CHILKOTINS The Coast Mountains of British Columbia are remote with limited accessibility by float plane, helicopter or boating up its deep inlets along the coast and hiking in. The mountains along British Columbia and SE Alaska intermix with the sea in a complex maze of fjords, with thousands of islands. It is a true wilderness where not exploited by logging and salmon farming pens. But there are some areas accessible from roads that can be explored, including west of Lillooet, the Chilcotins, and the Garibaldi Range. The Coast Mountains extend approximately 1,600 kilometres (1,000 mi) long from the southeastern boundaries are surrounded by the Fraser River and the Interior Plateau while its far northwestern edge is delimited by the Kelsall and Tatshenshini Rivers at the north end of the Alaska Panhandle, beyond which are the Saint Elias Mountains. The western mountain slopes are covered by dense temperate rainforest with heavily glaciated peaks and icefields that include Mt Waddington and Mt Silverthrone. Mount Waddington is the highest mountain of the Coast Mountains and the highest that lies entirely within British Columbia, located northeast of the head of Knight Inlet with an elevation of 4,019 metres (13,186 ft). The range along its eastern flanks tapers to the dry Interior Plateau and the boreal forests of the southern Chilkotins north to the Spatsizi Plateau Wilderness Provincial Park. The mountain range's name derives from its proximity to the sea coast, and it is often referred to as the Coast Range. The range includes volcanic and non-volcanic mountains and the extensive ice fields of the Pacific and Boundary Ranges, and the northern end of the volcanic system known as the Cascade Volcanoes. -
REPORT Processes Controlling the Growth and Evolution Of
REPORT Processes Controlling the Growth and Evolution of Continental Batholiths, Coast Mountains, British Columbia, Canada Terrace, British Columbia, Canada 12–17 August 2018 CONVENERS SUMMARY OF EXISTING DATA Harold Stowell, Geological Sciences, University of Alabama, The Coast Mountains batholith includes 170 to 45 Ma plutons Tuscaloosa, Alabama, 35487-0338, USA, [email protected] that vary from gabbro to leucogranite that intruded host rocks Margaret Rusmore, Dept. of Geology, Occidental College, from two composite terranes (e.g., Cecil et al., 2018). These rocks Los Angeles, California 90041, USA, [email protected] have provided stimulus for numerous geological research and Glenn Woodsworth, Geological Survey of Canada, Vancouver, mapping projects, including the pioneering maps produced by the British Columbia V6B 5J3, Canada, [email protected] Geological Survey of Canada, particularly by the late W.W. Hutchison (1982) and J.A. Roddick (1970). These maps delineated INTRODUCTION the fundamental contacts for the Coast Mountains batholith and This Thompson Field Forum brought together 27 geoscientists the tectonostratigraphic framework that the plutons intruded. The in Terrace, British Columbia, Canada, to discuss the processes maps served as the foundation for decades of research, led chiefly responsible for production of batholiths in continental magmatic by Lincoln Hollister and Maria Crawford, who guided numerous arcs. The forum focused on how the existing petrologic, geo- projects with students, post-docs, and other colleagues. Their chronologic, and structural data for the Coast Mountains batholith work led to fundamental advances in knowledge of granulite can inform modern paradigms for batholith growth and magma metamorphism, crustal thickening during batholith growth, the genesis. Decades-old models based on a robust but limited dataset production of batholith melts, and collapse of thickened crust along the well-exposed Skeena River corridor between Terrace during the last stages of batholith growth. -
Subarctic Passive House Study
July 11, 2013 Subarctic Passive House Case Study: A Superinsulated Foundation and Vapor Diffusion‐ Open Walls Cold Climate Housing Research Center Written by Bruno Grunau, PE July 11, 2013 Disclaimer: The research conducted or products tested used the methodologies described in this report. CCHRC cautions that different results might be obtained using different test methodologies. CCHRC suggests caution in drawing inferences regarding the research or products beyond the circumstances described in this report. i Subarctic Passive House Case Study: A Superinsulated Foundation and Vapor Diffusion‐Open Walls CONTENTS Summary .................................................................................................................................................................................................... 1 Introduction ............................................................................................................................................................................................... 2 Overview ................................................................................................................................................................................................ 2 Description of Wall System .................................................................................................................................................................... 3 Properties of Cellulose ..................................................................................................................................................................... -
High-Latitude Climate Zones and Climate Types - E.I
ENVIRONMENTAL STRUCTURE AND FUNCTION: CLIMATE SYSTEM – Vol. II - High-Latitude Climate Zones and Climate Types - E.I. Khlebnikova HIGH-LATITUDE CLIMATE ZONES AND CLIMATE TYPES E.I. Khlebnikova Main Geophysical Observatory, St.Petersburg, Russia Keywords: annual temperature range, Arctic continental climate, Arctic oceanic climate, katabatic wind, radiation cooling, subarctic continental climate, temperature inversion Contents 1. Introduction 2. Climate types of subarctic and subantarctic belts 2.1. Continental climate 2.2. Oceanic climate 3. Climate types in Arctic and Antarctic Regions 3.1. Climates of Arctic Region 3.2. Climates of Antarctic continent 3.2.1. Highland continental region 3.2.2. Glacial slope 3.2.3. Coastal region Glossary Bibliography Biographical Sketch Summary The description of the high-latitude climate zone and types is given according to the genetic classification of B.P. Alisov (see Genetic Classifications of Earth’s Climate). In dependence on air mass, which is in prevalence in different seasons, Arctic (Antarctic) and subarctic (subantarctic) belts are distinguished in these latitudes. Two kinds of climates are considered: continental and oceanic. Examples of typical temperature and precipitation regime and other meteorological elements are presented. 1. IntroductionUNESCO – EOLSS In the high latitudes of each hemisphere two climatic belts are distinguished: subarctic (subantarctic) andSAMPLE arctic (antarctic). CHAPTERS The regions with the prevalence of arctic (antarctic) air mass in winter, and polar air mass in summer, belong to the subarctic (subantarctic) belt. As a result of the peculiarities in distribution of continents and oceans in the northern hemisphere, two types of climate are distinguished in this belt: continental and oceanic. In the southern hemisphere there is only one type - oceanic. -
Climate and Vegetation
Name _____________________________ Class _________________ Date __________________ Physical Geography of the United States and Canada Section 2 Climate and Vegetation Terms and Names permafrost permanently frozen ground prevailing westerlies winds that blow from west to east in the middle latitudes Everglades huge swampland in southern Florida Before You Read In the last section, you read about the landforms and resources of the United States and Canada. In this section, you will learn how climate and vegetation affect life in the United States and Canada. As You Read Use a graphic organizer to take notes about the climate and vegetation of the United States and Canada. SHARED CLIMATES AND The north central and northeastern VEGETATION (Pages 123–124) United States and much of southern Where is the mildest shared climate Canada have a humid continental climate. found? Winters are cold and summers are warm. The Arctic coastlines of Alaska and Climate and soil make this one of the Canada have tundra climate and world’s most productive agricultural areas. vegetation. Winters here are long and It yields an abundance of dairy products, bitterly cold. Summers are brief and chilly. grain, and livestock. The land is a huge, treeless plain. In the upper part of this zone, summers Much of the rest of Canada and Alaska are short. There are mixed forests of have a subarctic climate. This climate has deciduous and needle-leafed evergreen very cold winters and short, mild trees. Most of the population of Canada is summers. A vast forest of needle-leafed located here. The lower part of the zone is evergreens covers the region. -
Cc Step by Step Western Canada
A CARTOGRAPHIC APPROACH You may wonder: how do I get from the unfinished map to the finished map? We like to approach this in a step-by-step method. This is a sensible way to proceed to help you get all the information you want shown on the map. It insures that the map is legible and neat. We always stress neatness to our students. We tell them that the map is not just for them, but for other people to see and read also. The following step-by-step method works well with all of our classroom maps. Try it with your students, and they will end up with a map they will be proud of! A Step-by-Step Guide to WESTERN CANADA To help you label and complete the maps in the CANADA CartoCraze unit, we have shown the activities for Western Canada broken down in the following series. This Step-by-step approach to the cartography of the maps can be applied to all the CartoCraze units. LABELING PLACES! Print neatly! For a good start, begin by labeling the Provinces: BRITISH COLUMBIA ALBERTA Next, label the capitals: Victoria Edmonton Add a few large cities: Calgary Vancouver Prince Rupert Add others, such as Medicine Hat You can also identify neighboring places, such as: UNITED STATES ALASKA Yukon Territory Northwest Territory Saskatchewan WATER AND MOUNTAINS Continue labeling and begin to color! For a good start, begin by labeling the bodies of water already on the map: PACIFIC OCEAN Lake Athabasca Fraser River North Saskatchewan River South Saskatchewan River Add other bodies of water, such as: Peace River Start adding color to the map.