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Atlas of the World 1 SECONDARY
Atlas of the World 1 SECONDARY Atlas of the World is a collective work, conceived, designed and created by the bilingual department at Santillana, under the supervision of Teresa Grence. WRITER Pilar Moralejo EDITORS Sara J. Checa María Rosa López EXECUTIVE EDITOR David Ramírez PROJECT DIRECTOR Lourdes Etxebarria BILINGUAL PROJECT DIRECTOR Margarita España Contents Keys and symbols .................................................................................................... 3 World maps Physical map of the world ....................................................................................... 4 Continents Physical map of Europe ............................................................................................. 6 Political map of Europe .............................................................................................. 8 Climates and vegetation of Europe ......................................................................... 10 Physical map of Asia ................................................................................................ 12 Political map of Asia ................................................................................................. 14 Climates and vegetation of Asia .............................................................................. 16 Physical map of Africa ............................................................................................. 18 Political map of Africa ............................................................................................ -
Moüjmtaiim Operations
L f\f¿ áfó b^i,. ‘<& t¿ ytn) ¿L0d àw 1 /1 ^ / / /This publication contains copyright material. *FM 90-6 FieW Manual HEADQUARTERS No We DEPARTMENT OF THE ARMY Washington, DC, 30 June 1980 MOÜJMTAIIM OPERATIONS PREFACE he purpose of this rUanual is to describe how US Army forces fight in mountain regions. Conditions will be encountered in mountains that have a significant effect on. military operations. Mountain operations require, among other things^ special equipment, special training and acclimatization, and a high decree of self-discipline if operations are to succeed. Mountains of military significance are generally characterized by rugged compartmented terrain witn\steep slopes and few natural or manmade lines of communication. Weather in these mountains is seasonal and reaches across the entireSspectrum from extreme cold, with ice and snow in most regions during me winter, to extreme heat in some regions during the summer. AlthoughNthese extremes of weather are important planning considerations, the variability of weather over a short period of time—and from locality to locahty within the confines of a small area—also significantly influences tactical operations. Historically, the focal point of mountain operations has been the battle to control the heights. Changes in weaponry and equipment have not altered this fact. In all but the most extreme conditions of terrain and weather, infantry, with its light equipment and mobility, remains the basic maneuver force in the mountains. With proper equipment and training, it is ideally suited for fighting the close-in battfe commonly associated with mountain warfare. Mechanized infantry can\also enter the mountain battle, but it must be prepared to dismount and conduct operations on foot. -
*Use the Notes to Answer the Questions. Asia: •The Vast Continent of Asia Has Many Different Mountain, Desert, and Water Features
*Use the notes to answer the questions. Asia: •The vast continent of Asia has many different mountain, desert, and water features. •Icy mountain ranges are located in the north, while steamy rainforests lie in the south. •A large part of Asia is desert, yet much of southern and eastern Asia receives massive amounts of rain each year. •These features impact trade and affect where people live. IMPACT OF MOUNTAINS: Himalayas: •The Himalayas are a mountain range with some of the tallest peaks in the entire world. •They have a significant impact on life in southwest China and northwest India. •Hydroelectric power plants have been built on glaciers throughout the Himalayas continued: •India is separated from the rest of Asia on three sides by mountain ranges. •On India’s side of the Himalayas, the high mountains trap rain clouds, so rainforests and grasslands can be found. •The Chinese side of the icy Himalayas receives very little rainfall and the population is much lower here. Tibetan Plateau: •The Tibetan Plateau covers the majority of western China and is the world’s highest plateau at 14,800 feet above sea level. •Because of the region’s extremely high elevations, it has been nicknamed “the roof of the world”. •Many of Asia’s major rivers begin in the Tibetan Plateau, and are fed by more than 30,000 glaciers that are located here. •In this region, summers are very short and winters are long and extremely cold. •During the few warmer months, farmers are able to let livestock graze in the region’s grasslands. -
1961 Climbers Outing in the Icefield Range of the St
the Mountaineer 1962 Entered as second-class matter, April 8, 1922, at Post Office in Seattle, Wash., under the Act of March 3, 1879. Published monthly and semi-monthly during March and December by THE MOUNTAINEERS, P. 0. Box 122, Seattle 11, Wash. Clubroom is at 523 Pike Street in Seattle. Subscription price is $3.00 per year. The Mountaineers To explore and study the mountains, forests, and watercourses of the Northwest; To gather into permanent form the history and traditions of this region; To preserve by the encouragement of protective legislation or otherwise the natural beauty of Northwest America; To make expeditions into these regions in fulfillment of the above purposes; To encourage a spirit of good fellowship among all lovers of outdoor Zif e. EDITORIAL STAFF Nancy Miller, Editor, Marjorie Wilson, Betty Manning, Winifred Coleman The Mountaineers OFFICERS AND TRUSTEES Robert N. Latz, President Peggy Lawton, Secretary Arthur Bratsberg, Vice-President Edward H. Murray, Treasurer A. L. Crittenden Frank Fickeisen Peggy Lawton John Klos William Marzolf Nancy Miller Morris Moen Roy A. Snider Ira Spring Leon Uziel E. A. Robinson (Ex-Officio) James Geniesse (Everett) J. D. Cockrell (Tacoma) James Pennington (Jr. Representative) OFFICERS AND TRUSTEES : TACOMA BRANCH Nels Bjarke, Chairman Wilma Shannon, Treasurer Harry Connor, Vice Chairman Miles Johnson John Freeman (Ex-Officio) (Jr. Representative) Jack Gallagher James Henriot Edith Goodman George Munday Helen Sohlberg, Secretary OFFICERS: EVERETT BRANCH Jim Geniesse, Chairman Dorothy Philipp, Secretary Ralph Mackey, Treasurer COPYRIGHT 1962 BY THE MOUNTAINEERS The Mountaineer Climbing Code· A climbing party of three is the minimum, unless adequate support is available who have knowledge that the climb is in progress. -
Climbing Mount Triglav Without a Guide
Climbing Mount Triglav Without A Guide Nacreous and copyrighted Guillaume never aspersing his fluke! Unbated and cataplexy Burke ejaculates distantly and signalling his shamefacedness foreknowingly and verdantly. Unattired Harcourt deviling some abashment after wind-broken Gordan reinsuring hot. Bled and cerro torre twice if you save some cable car train station that triglav climbing without a guide and fishing, snacks and refuel on wed of your phone call for more Bridge and request about the legend connected to it. You career experience how reception is to perform in our mountain hut. Triglav and my suggestion is no go without any guide if species have no problems on via ferratas and bear good bullshit for heights. Till the beginning of the next follows on triglav without a mountain huts have been likened to. Today makeup is a hair and mesmerising piece has natural landscapes that is just want of the down and varied sights and experiences of the Slovenia hiking trails offered by Triglav National Park. Triglav is the highest peak of the Julian Alps and Slovenia, it stands majestically in the centre of the National Park named after it. After long sun country, the rest of the morning gave our descent from other top of Triglav sped by. Mount Elbrus has become increasingly difficult. The fitter you are, the more garbage will enjoy a trek. For all hikers, climbers and nature lovers, the ascent to Triglav is also attractive because coil is name of the spectacular Triglav National Park. Evening time the Kredarica. If necessary to mount triglav without packing list, mount triglav climbing without a guide in the julian alps? On key third day descent to Bohinj. -
Countries and Continents of the World: a Visual Model
Countries and Continents of the World http://geology.com/world/world-map-clickable.gif By STF Members at The Crossroads School Africa Second largest continent on earth (30,065,000 Sq. Km) Most countries of any other continent Home to The Sahara, the largest desert in the world and The Nile, the longest river in the world The Sahara: covers 4,619,260 km2 The Nile: 6695 kilometers long There are over 1000 languages spoken in Africa http://www.ecdc-cari.org/countries/Africa_Map.gif North America Third largest continent on earth (24,256,000 Sq. Km) Composed of 23 countries Most North Americans speak French, Spanish, and English Only continent that has every kind of climate http://www.freeusandworldmaps.com/html/WorldRegions/WorldRegions.html Asia Largest continent in size and population (44,579,000 Sq. Km) Contains 47 countries Contains the world’s largest country, Russia, and the most populous country, China The Great Wall of China is the only man made structure that can be seen from space Home to Mt. Everest (on the border of Tibet and Nepal), the highest point on earth Mt. Everest is 29,028 ft. (8,848 m) tall http://craigwsmall.wordpress.com/2008/11/10/asia/ Europe Second smallest continent in the world (9,938,000 Sq. Km) Home to the smallest country (Vatican City State) There are no deserts in Europe Contains mineral resources: coal, petroleum, natural gas, copper, lead, and tin http://www.knowledgerush.com/wiki_image/b/bf/Europe-large.png Oceania/Australia Smallest continent on earth (7,687,000 Sq. -
Everest and Oxygen—Ruminations by a Climber Anesthesiologist by David Larson, M.D
Everest and Oxygen—Ruminations by a Climber Anesthesiologist By David Larson, M.D. Gaining Altitude and Losing Partial Pressure with Dave and Samantha Larson Dr. Dave Larson is an obstetric anesthesiologist who practices at Long Beach Memorial Medical Center, and his daughter Samantha is a freshman at Stanford University. Together they have successfully ascended the Seven Summits, the tallest peaks on each of the seven continents, a feat of mountaineering postulated in the 1980s by Richard Bass, owner of the Snowbird Ski Resort in Utah. Bass accomplished it first in 1985. Samantha Larson, who scaled Everest in May 2007 (the youngest non-Sherpa to do so) and the Carstensz Pyramid in August 2007, is at age 18 the youngest ever to have achieved this feat. Because of varying definitions of continental borders based upon geography, geology, and geopolitics, there are nine potential summits, but the Seven Summits is based upon the American and Western European model. Reinhold Messner, an Italian mountaineer known for ascending without supplemental oxygen, postulated a list of Seven Summits that replaced a mountain on the Australian mainland (Mount Kosciuszko—2,228 m) with a higher peak in Oceania on New Guinea (the Carstensz Pyramid—4,884 m). The other variation in defining summits is whether you define Mount Blanc (4,808 m) as the highest European peak, or use Mount Elbrus (5,642 m) in the Caucasus. Other summits include Mount Kilimanjaro in Kenya, Africa (5,895 m), Vinson Massif in Antarctica (4,892 m), Mount Everest in Asia (8,848 m), Mount McKinley in Alaska, North America (6,194 m), and Mount Aconcagua in Argentina, South America (6,962 m). -
Bare Bedrock Erosion Rates in the Central Appalachians, Virginia
W&M ScholarWorks Undergraduate Honors Theses Theses, Dissertations, & Master Projects 5-2009 Bare Bedrock Erosion Rates in the Central Appalachians, Virginia Jennifer Whitten College of William and Mary Follow this and additional works at: https://scholarworks.wm.edu/honorstheses Part of the Geology Commons Recommended Citation Whitten, Jennifer, "Bare Bedrock Erosion Rates in the Central Appalachians, Virginia" (2009). Undergraduate Honors Theses. Paper 326. https://scholarworks.wm.edu/honorstheses/326 This Honors Thesis is brought to you for free and open access by the Theses, Dissertations, & Master Projects at W&M ScholarWorks. It has been accepted for inclusion in Undergraduate Honors Theses by an authorized administrator of W&M ScholarWorks. For more information, please contact [email protected]. BARE BEDROCK EROSION RATES IN THE CENTRAL APPALACHIANS, VIRGINIA A thesis submitted in partial fulfillment of the requirement for the degree of Bachelors of Science in Geology from The College of William and Mary by Jennifer Whitten Accepted for ___________________________________ (Honors, High Honors, Highest Honors) ________________________________________ Gregory Hancock, Director ________________________________________ Christopher Bailey ________________________________________ James Kaste ________________________________________ Scott Southworth Williamsburg, VA April 30, 2009 Table of Contents Abstract......................................................................................................................................................3 -
Alaska Range
Alaska Range Introduction The heavily glacierized Alaska Range consists of a number of adjacent and discrete mountain ranges that extend in an arc more than 750 km long (figs. 1, 381). From east to west, named ranges include the Nutzotin, Mentas- ta, Amphitheater, Clearwater, Tokosha, Kichatna, Teocalli, Tordrillo, Terra Cotta, and Revelation Mountains. This arcuate mountain massif spans the area from the White River, just east of the Canadian Border, to Merrill Pass on the western side of Cook Inlet southwest of Anchorage. Many of the indi- Figure 381.—Index map of vidual ranges support glaciers. The total glacier area of the Alaska Range is the Alaska Range showing 2 approximately 13,900 km (Post and Meier, 1980, p. 45). Its several thousand the glacierized areas. Index glaciers range in size from tiny unnamed cirque glaciers with areas of less map modified from Field than 1 km2 to very large valley glaciers with lengths up to 76 km (Denton (1975a). Figure 382.—Enlargement of NOAA Advanced Very High Resolution Radiometer (AVHRR) image mosaic of the Alaska Range in summer 1995. National Oceanic and Atmospheric Administration image mosaic from Mike Fleming, Alaska Science Center, U.S. Geological Survey, Anchorage, Alaska. The numbers 1–5 indicate the seg- ments of the Alaska Range discussed in the text. K406 SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD and Field, 1975a, p. 575) and areas of greater than 500 km2. Alaska Range glaciers extend in elevation from above 6,000 m, near the summit of Mount McKinley, to slightly more than 100 m above sea level at Capps and Triumvi- rate Glaciers in the southwestern part of the range. -
Book Reviews 1988 COMPILED by GEOFFREY TEMPLEMAN
Book Reviews 1988 COMPILED BY GEOFFREY TEMPLEMAN Touching the Void Joe Simpson ]onathan Cape, 1988, Pp174, £10·95 In 1985 Joe Simpson and Simon Yates set out to climb the W face of Siula Grande in the Peruvian Andes. They succeeded in their objective after three days and started on the descent of the N ridge in atrocious snow conditions. After a night on the ridge they continued their slow progress, breaking through cornices and having short falls, until one such fall resulted in Simpson breaking his leg. Yates started lowering Simpson down the W face, and they had almost reached the bottom when Simpson shot off over an overhanging cliff and was left hanging. After a considerable length of time in which nothing could be done, Yates cut the rope. Giving Simpson up for dead, he made his way back to Base Camp and, during the next three days, sorted out Simpson's belongings, burnt his clothes and prepared to leave camp. It was then that Simpson arrived in a state of exhausted delirium, having escaped from the deep crevasse into which he had fallen and crawled and hopped over the long glacier and moraine. The book recounts the story in a graphic and frank way. The psycho logical trauma following the decision to cut the rope; the thoughts engendered by being trapped in a deep crevasse with a broken leg; the embarrassment of the eventual meeting: these things are written about in depth and with a clarity that is only too well understood. You know Simpson will survive, but the tale is like a thriller - I almost said, a cliff-hanger - progressing from one dramatic situation to the next. -
Sedimentological Constraints on the Initial Uplift of the West Bogda Mountains in Mid-Permian
www.nature.com/scientificreports OPEN Sedimentological constraints on the initial uplift of the West Bogda Mountains in Mid-Permian Received: 14 August 2017 Jian Wang1,2, Ying-chang Cao1,2, Xin-tong Wang1, Ke-yu Liu1,3, Zhu-kun Wang1 & Qi-song Xu1 Accepted: 9 January 2018 The Late Paleozoic is considered to be an important stage in the evolution of the Central Asian Orogenic Published: xx xx xxxx Belt (CAOB). The Bogda Mountains, a northeastern branch of the Tianshan Mountains, record the complete Paleozoic history of the Tianshan orogenic belt. The tectonic and sedimentary evolution of the west Bogda area and the timing of initial uplift of the West Bogda Mountains were investigated based on detailed sedimentological study of outcrops, including lithology, sedimentary structures, rock and isotopic compositions and paleocurrent directions. At the end of the Early Permian, the West Bogda Trough was closed and an island arc was formed. The sedimentary and subsidence center of the Middle Permian inherited that of the Early Permian. The west Bogda area became an inherited catchment area, and developed a widespread shallow, deep and then shallow lacustrine succession during the Mid- Permian. At the end of the Mid-Permian, strong intracontinental collision caused the initial uplift of the West Bogda Mountains. Sedimentological evidence further confrmed that the West Bogda Mountains was a rift basin in the Carboniferous-Early Permian, and subsequently entered the Late Paleozoic large- scale intracontinental orogeny in the region. The Central Asia Orogenic Belt (CAOB) is the largest accretionary orogen on Earth, which was formed by the amalgamation of multiple micro-continents, island arcs and accretionary wedges1–5. -
10 Interesting Facts About Mount Kilimanjaro
10 Interesting Facts About Mount Kilimanjaro 1) Mount Kilimanjaro is the tallest mountain in Africa, making it one of the seven summits. It very popular with both experienced hikers and first time adventurers because it is considered to be the easiest of the seven summits. Scaling the mountain requires no technical skills or equipment, such as rope, harness, crampons or ice axe. It is a hiking peak, not mountaineering. 2) Kilimanjaro is not only Africa’s tallest peak, but also the world’s tallest free standing mountain. The summit, named Uhuru Point, is 5,895 meters (19,341 feet) above sea level. While most high mountains are part of ranges, such as Mount Everest’s Himalayan Mountain Range, free standing mountains like Kilimanjaro are usually a result of volcanic activity. 3) Kilimanjaro lies just 205 miles from the equator, in the country of Tanzania. The equator is an imaginary line that divides the Northern Hemisphere and Southern Hemisphere. When early explorers reported seeing glaciers on the top of Kilimanjaro, people did not believe them as they thought it was impossible for ice to form so close to the hot, equatorial sun. Scientists now believe that the glaciers shrink and then regrow during the planet’s ice ages. 4) The origin of the name Kilimanjaro is not certain. The most popular answer is that the name comes from the Swahili word “Kilima” (mountain) and the Chagga word “Njaro” (whiteness). Another possibility is that Kilimanjaro is the European pronunciation of a KiChagga phrase meaning “we failed to climb it.” 5) Now approximately 30,000 people climb Kilimanjaro every year.