Glacier National Park
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Peaks-Glacier
Glacier National Park Summit List ©2003, 2006 Glacier Mountaineering Society Page 1 Summit El Quadrangle Notes ❑ Adair Ridge 5,366 Camas Ridge West ❑ Ahern Peak 8,749 Ahern Pass ❑ Allen Mountain 9,376 Many Glacier ❑ Almost-A-Dog Mtn. 8,922 Mount Stimson ❑ Altyn Peak 7,947 Many Glacier ❑ Amphitheater Mountain 8,690 Cut Bank Pass ❑ Anaconda Peak 8,279 Mount Geduhn ❑ Angel Wing 7,430 Many Glacier ❑ Apgar Mountains 6,651 McGee Meadow ❑ Apikuni Mountain 9,068 Many Glacier ❑ Appistoki Peak 8,164 Squaw Mountain ❑ B-7 Pillar (3) 8,712 Ahern Pass ❑ Bad Marriage Mtn. 8,350 Cut Bank Pass ❑ Baring Point 7,306 Rising Sun ❑ Barrier Buttes 7,402 Mount Rockwell ❑ Basin Mountain 6,920 Kiowa ❑ Battlement Mountain 8,830 Mount Saint Nicholas ❑ Bear Mountain 8,841 Mount Cleveland ❑ Bear Mountain Point 6,300 Gable Mountain ❑ Bearhat Mountain 8,684 Mount Cannon ❑ Bearhead Mountain 8,406 Squaw Mountain ❑ Belton Hills 6,339 Lake McDonald West ❑ Bighorn Peak 7,185 Vulture Peak ❑ Bishops Cap 9,127 Logan Pass ❑ Bison Mountain 7,833 Squaw Mountain ❑ Blackfoot Mountain 9,574 Mount Jackson ❑ Blacktail Hills 6,092 Blacktail ❑ Boulder Peak 8,528 Mount Carter ❑ Boulder Ridge 6,415 Lake Sherburne ❑ Brave Dog Mountain 8,446 Blacktail ❑ Brown, Mount 8,565 Mount Cannon ❑ Bullhead Point 7,445 Many Glacier ❑ Calf Robe Mountain 7,920 Squaw Mountain ❑ Campbell Mountain 8,245 Porcupine Ridge ❑ Cannon, Mount 8,952 Mount Cannon ❑ Cannon, Mount, SW Pk. 8,716 Mount Cannon ❑ Caper Peak 8,310 Mount Rockwell ❑ Carter, Mount 9,843 Mount Carter ❑ Cataract Mountain 8,180 Logan Pass ❑ Cathedral -
Red River: the Northern Border of Texas!
“From Palo Duro Canyon outside Amarillo Texas The prairie dog town fork of the Red River flows Headed cross the plains along the coast of Oklahoma To the Mississippi River and the Gulf of Mexico” Red River by Guy Clark Red River: The northern Border of Texas! By Wm Davey Edwards, PhD Texas & Oklahoma Professional Land Surveyor Texas Licensed State Land Surveyor US Federal Land Surveyor Edwards Surveying, LLC Decatur, Texas Red River Boundary between Texas and Oklahoma South bank of the Red River in July 2015 the day after a rain. Objectives • Natural Boundaries • Accretion, Erosion, and Avulsion • BLM Claims • Conclusion Natural Boundaries for International Borders Adams – Onís Treaty of 1819 • Sabine, Red, and Arkansas Rivers • begin on the Gulf of Mexico, at the mouth of the River Sabine in the Sea, continuing North, along the Western Bank of that River, to the 32d degree of Latitude; thence by a Line due North to the degree of Latitude, where it strikes the Rio Roxo of Natchitoches, or Red-River, then following the course of the Rio-Roxo Westward to the degree of Longitude, 100 West from London and 23 from Washington, then crossing the said Red-River, and running thence by a Line due North to the River Arkansas, thence, following the Course of the Southern bank of the Arkansas to its source in Latitude, 42. North and thence by that parallel of Latitude to the South-Sea Caroline C. Stafford v. Adam C. King • SUPREME COURT OF TEXAS, 30 Tex. 257, April, 1867 Natural objects are mountains, lakes, rivers, creeks, rocks, and the like; artificial objects are marked trees, stakes, mounds, etc., constructed by others or the surveyor, and called for in the field- notes, and they should be inserted in the patent. -
Lesson 4: Sediment Deposition and River Structures
LESSON 4: SEDIMENT DEPOSITION AND RIVER STRUCTURES ESSENTIAL QUESTION: What combination of factors both natural and manmade is necessary for healthy river restoration and how does this enhance the sustainability of natural and human communities? GUIDING QUESTION: As rivers age and slow they deposit sediment and form sediment structures, how are sediments and sediment structures important to the river ecosystem? OVERVIEW: The focus of this lesson is the deposition and erosional effects of slow-moving water in low gradient areas. These “mature rivers” with decreasing gradient result in the settling and deposition of sediments and the formation sediment structures. The river’s fast-flowing zone, the thalweg, causes erosion of the river banks forming cliffs called cut-banks. On slower inside turns, sediment is deposited as point-bars. Where the gradient is particularly level, the river will branch into many separate channels that weave in and out, leaving gravel bar islands. Where two meanders meet, the river will straighten, leaving oxbow lakes in the former meander bends. TIME: One class period MATERIALS: . Lesson 4- Sediment Deposition and River Structures.pptx . Lesson 4a- Sediment Deposition and River Structures.pdf . StreamTable.pptx . StreamTable.pdf . Mass Wasting and Flash Floods.pptx . Mass Wasting and Flash Floods.pdf . Stream Table . Sand . Reflection Journal Pages (printable handout) . Vocabulary Notes (printable handout) PROCEDURE: 1. Review Essential Question and introduce Guiding Question. 2. Hand out first Reflection Journal page and have students take a minute to consider and respond to the questions then discuss responses and questions generated. 3. Handout and go over the Vocabulary Notes. Students will define the vocabulary words as they watch the PowerPoint Lesson. -
Glacier NATIONAL PARK, MONTANA
Glacier NATIONAL PARK, MONTANA, UNITED STATES SECTION WATERTON-GLACIER INTERNATIONAL PEACE PARK Divide in northwestern Montana, contains nearly 1,600 ivy. We suggest that you pack your lunch, leave your without being burdened with camping equipment, you may square miles of some of the most spectacular scenery and automobile in a parking area, and spend a day or as much hike to either Sperry Chalets or Granite Park Chalets, primitive wilderness in the entire Rocky Mountain region. time as you can spare in the out of doors. Intimacy with where meals and overnight accommodations are available. Glacier From the park, streams flow northward to Hudson Bay, nature is one of the priceless experiences offered in this There are shelter cabins at Gunsight Lake and Gunsight eastward to the Gulf of Mexico, and westward to the Pa mountain sanctuary. Surely a hike into the wilderness will Pass, Fifty Mountain, and Stoney Indian Pass. The shelter cific. It is a land of sharp, precipitous peaks and sheer be the highlight of your visit to the park and will provide cabins are equipped with beds and cooking stoves, but you NATIONAL PARK knife-edged ridges, girdled with forests. Alpine glaciers you with many vivid memories. will have to bring your own sleeping and cooking gear. lie in the shadow of towering walls at the head of great ice- Trail trips range in length from short, 15-minute walks For back-country travel, you will need a topographic map carved valleys. along self-guiding nature trails to hikes that may extend that shows trails, streams, lakes, mountains, and glaciers. -
Granite Park Chalet and Dormitory AND/OR COMMON N/A LOCATION
Form No. i0-306 (Rev 10-74) UNITED STATES DEPARTMENT OF THE INTERIOR lli|$|l;!tli:®pls NATIONAL PARK SERVICE NATIONAL REGISTER OF HISTORIC PLACES iliiiii: INVENTORY- NOMINATION FORM FOR FEDERAL PROPERTIES SEE INSTRUCTIONS IN HOW TO COMPLETE NATIONAL REGISTER FORMS TYPE ALL ENTRIES -- COMPLETE APPLICABLE SECTIONS NAME HISTORIC Granite Park Chalet and Dormitory AND/OR COMMON N/A LOCATION STREET & NUMBER Glacier National Park NOT FOR PUBLICATION CITY. TOWN CONGRESSIONAL DISTRICT West Glacier X- VICINITY OF 1 STATE CODE COUNTY CODE Montana 30 Flathead 029 QCLASSIFI CATION CATEGORY OWNERSHIP STATUS PRESENT USE _DISTRICT X.PUBLIC X_OCCUPIED _ AGRICULTURE —MUSEUM X_BUILDING(S) _PRIVATE —UNOCCUPIED X.COMMERCIAL X_RARK —STRUCTURE _BOTH —WORK IN PROGRESS —EDUCATIONAL —PRIVATE RESIDENCE —SITE PUBLIC ACQUISITION ACCESSIBLE —ENTERTAINMENT —RELIGIOUS —OBJECT N/AN PR OCESS —YES: RESTRICTED —GOVERNMENT —SCIENTIFIC _ BEING CONSIDERED X-YES: UNRESTRICTED —INDUSTRIAL —TRANSPORTATION —NO —MILITARY _OTHER: AGENCY REGIONAL HEADQUARTERS: (Happlicable) ______National Park Service, Rocky Mountain Region STREET & NUMBER ____655 Parfet, P.O. Box 25287 CITY. TOWN STATE N/A _____Denver VICINITY OF Colorado 80225 LOCATION OF LEGAL DESCRIPTION COURTHOUSE. REGISTRY OF DEEDS. ETC Qlacier National STREET & NUMBER N/A CITY. TOWN STATE West Glacier Montana REPRESENTATION IN EXISTING SURVEYS TITLE List of Classified Structures Inventory DATE August 1975 X-FEDERAL _STATE —COUNTY _LOCAL DEPOSITORY FOR SURVEY RECORDS National Park Service, Rocky Mountain Region CITY. TOWN STATE Colorado^ DESCRIPTION CONDITION CHECK ONE CHECK ONE —EXCELLENT —DETERIORATED —UNALTERED X-ORIGINALSITE X.GOOD —RUINS X-ALTERED —MOVED DATE- _FAIR _UNEXPOSED DESCRIBE THE PRESENT AND ORIGINAL (IF KNOWN) PHYSICAL APPEARANCE The Granite Park Chalet and Dormitory are situated near the Swiftcurrent Pass in Glacier National Park at an elevation of 7,000 feet. -
Topic 12 – Shaping the Earth Vocabulary
Topic 12 – Shaping the Earth Vocabulary Abrasion – physical action of scraping, rubbing, grinding or wearing away rock material Chemical weathering – the process of using natural chemical reactions to break down rock Cut bank – Outside bend in a stream where the water velocity is fastest and erosion is the greatest. Delta – the region of a stream mouth where sediment is deposited as it flows into a large body of water in graded beds of largest to smallest particles Deposition – the process where sediment is dropped out of the stream current and builds into layers Drumlin – a glacial feature that is created as a glacier flows. The blunt end shows the direction of flow Erosion – the removal of sediment and weather material from rock Glacier – a mass of ice that flows due to gravity Kettle lake – a small round lake that is formed when a large chunk of glacial ice creates a depression in the Earth’s surface and melts Landscape – regions on Earth’s surface with similar surface feature such as mountains, plains and plateaus Mass movement – the movement of large quantities of earth materials due to gravity, includes landslides, mudslides, rock slides and soil creep Meander – the curve or bend of a stream channel Moraine – a large ridge, pile or sheet of unsorted sediment deposited by a glacier Outwash plain – a glacial feature of sorted layered sediment as the result of the glacier melting Physical weathering – the mechanical breakdown of rock material at the earth’s surface into smaller pieces Point bar – Opposite the cut bank in a stream where the velocity is slowest and deposition is the greatest. -
Montana State Parks Guide Reservations for Camping and Other Accommodations: Toll Free: 1-855-922-6768 Stateparks.Mt.Gov
For more information about Montana State Parks: 406-444-3750 TDD: 406-444-1200 website: stateparks.mt.gov P.O. Box 200701 • Helena, MT 59620-0701 Montana State Parks Guide Reservations for camping and other accommodations: Toll Free: 1-855-922-6768 stateparks.mt.gov For general travel information: 1-800-VISIT-MT (1-800-847-4868) www.visitmt.com Join us on Twitter, Facebook & Instagram If you need emergency assistance, call 911. To report vandalism or other park violations, call 1-800-TIP-MONT (1-800-847-6668). Your call can be anonymous. You may be eligible for a reward. Montana Fish, Wildlife & Parks strives to ensure its programs, sites and facilities are accessible to all people, including those with disabilities. To learn more, or to request accommodations, call 406-444-3750. Cover photo by Jason Savage Photography Lewis and Clark portrait reproductions courtesy of Independence National Historic Park Library, Philadelphia, PA. This document was produced by Montana Fish Wildlife & Parks and was printed at state expense. Information on the cost of this publication can be obtained by contacting Montana State Parks. Printed on Recycled Paper © 2018 Montana State Parks MSP Brochure Cover 15.indd 1 7/13/2018 9:40:43 AM 1 Whitefish Lake 6 15 24 33 First Peoples Buffalo Jump* 42 Tongue River Reservoir Logan BeTableaverta ilof Hill Contents Lewis & Clark Caverns Les Mason* 7 16 25 34 43 Thompson Falls Fort3-9 Owen*Historical Sites 28. VisitorMadison Centers, Buff Camping,alo Ju mp* Giant Springs* Medicine Rocks Whitefish Lake 8 Fish Creek 17 Granite11-15 *Nature Parks 26DisabledMissouri Access Headw ibility aters 35 Ackley Lake 44 Pirogue Island* WATERTON-GLACIER INTERNATIONAL 2 Lone Pine* PEACE PARK9 Council Grove* 18 Lost Creek 27 Elkhorn* 36 Greycliff Prairie Dog Town* 45 Makoshika Y a WHITEFISH < 16-23 Water-based Recreation 29. -
General Correspondence, July 10-25, 1923
• 10. 19 ] • • • - • d ,. out of ill o. ',. V ./ ( ) , t . • July r .... • ., .. / t 0 • '" niotor ' 'to t 0 'fill· oocumr , , 0 , ~ ~u 1 or ttL • t of us f"o t . e .. ey• , y • • • .. ablu, .. .. ull., / 0 C py • .. v 1:. I -u . 7- 1ti-P~ ~ I ~ -• J . - ., ; . '" / • ! , .. o thorn e , J ly ],9. 1923. • Ir. ' . • ey: • I J On uth rn ~ci· ne, cT- ly 18. 1923 • • -~ --- -.-----.---. I t e t Cel., July 20, 1 23. .1"' . c. lb"ty: . I tntt to' th !.llk or l~ . tl"oubl to n~G u.p for move- c .. t f c~ to co £0 00- , the tr ythi.. ~ - t £i c;it moon. - f crrivc he~.., t.e c:::rbcf i "1 d,,, in i. 1;1 oJ i rin~ to Inci<J I of . fa 'I 1 • to (}ate I min- of y ur at rTf '10 1I:r· ill you about it ·urn .. • pt..sa 0 n. I , ., . • • • • u1 • • o • • • GREAT ORTHERN RAILWAY COMPA EXECUTIVE DEPARTMENT LOUIS W . HILL. CHAIRMAN OF THE BoARD (C 0 P y) -ST. PAUL. MINN .• At Pebble Beach, Cal., .July 21, 1923. Mr • .J . R. Eakin, Superintendent, Glacier National Park, Be 1 ton, Montana. Dear Mr . Eakin: After a few days' trip in Glacier Park, I feel 1'should write you very frankly my observations and impressions, I cannot help but be greatly interested in the development of the Park as we have a very large investment there - about $1 , 500 , 000 - in the hotels, camps, cost of roads, bridges, etc. The Logan Pass Trail is not as wide nor in as good con dition as when originally constructed. -
Protecting the Crown: a Century of Resource Management in Glacier National Park
Protecting the Crown A Century of Resource Management in Glacier National Park Rocky Mountains Cooperative Ecosystem Studies Unit (RM-CESU) RM-CESU Cooperative Agreement H2380040001 (WASO) RM-CESU Task Agreement J1434080053 Theodore Catton, Principal Investigator University of Montana Department of History Missoula, Montana 59812 Diane Krahe, Researcher University of Montana Department of History Missoula, Montana 59812 Deirdre K. Shaw NPS Key Official and Curator Glacier National Park West Glacier, Montana 59936 June 2011 Table of Contents List of Maps and Photographs v Introduction: Protecting the Crown 1 Chapter 1: A Homeland and a Frontier 5 Chapter 2: A Reservoir of Nature 23 Chapter 3: A Complete Sanctuary 57 Chapter 4: A Vignette of Primitive America 103 Chapter 5: A Sustainable Ecosystem 179 Conclusion: Preserving Different Natures 245 Bibliography 249 Index 261 List of Maps and Photographs MAPS Glacier National Park 22 Threats to Glacier National Park 168 PHOTOGRAPHS Cover - hikers going to Grinnell Glacier, 1930s, HPC 001581 Introduction – Three buses on Going-to-the-Sun Road, 1937, GNPA 11829 1 1.1 Two Cultural Legacies – McDonald family, GNPA 64 5 1.2 Indian Use and Occupancy – unidentified couple by lake, GNPA 24 7 1.3 Scientific Exploration – George B. Grinnell, Web 12 1.4 New Forms of Resource Use – group with stringer of fish, GNPA 551 14 2.1 A Foundation in Law – ranger at check station, GNPA 2874 23 2.2 An Emphasis on Law Enforcement – two park employees on hotel porch, 1915 HPC 001037 25 2.3 Stocking the Park – men with dead mountain lions, GNPA 9199 31 2.4 Balancing Preservation and Use – road-building contractors, 1924, GNPA 304 40 2.5 Forest Protection – Half Moon Fire, 1929, GNPA 11818 45 2.6 Properties on Lake McDonald – cabin in Apgar, Web 54 3.1 A Background of Construction – gas shovel, GTSR, 1937, GNPA 11647 57 3.2 Wildlife Studies in the 1930s – George M. -
The Spatial Distribution of Bed Sediment on Fluvial System: a Mini Review of the Aceh Meandering River
Aceh Int. J. Sci. Technol., 5(2): 82-87 August 2016 doi: 10.13170/aijst.5.2.4932 Aceh International Journal of Science and Technology ISSN: 2088-9860 Journal homepage: http://jurnal.unsyiah.ac.id/aijst The Spatial Distribution of Bed Sediment on Fluvial System: A Mini Review of the Aceh Meandering River Muhammad Irham Faculty of Marine and Fisheries Science, University of Syiah Kuala, Banda Aceh 23111, Indonesia. Corresponding author, email: [email protected] Received : 2 August 2016 Accepted : 28 August 2016 Online : 31 August2016 Abstract - Dynamic interactions of hydrological and geomorphological processes in the fluvial system result in accumulated deposit on the bed because the capacity to carry sediment has been exceeded. The bed load of the Aceh fluvial system is primarily generated by mechanical weathering resulting in boulders, pebbles, and sand, which roll or bounce along the river bed forming temporary deposits as bars on the insides of meander bends, as a result of a loss of transport energy in the system. This dynamic controls the style and range of deposits in the Aceh River. This study focuses on the spatial distribution of bed-load transport of the Aceh River. Understanding the spatial distribution of deposits facilitates the reconstruction of the changes in controlling factors during accumulation of deposits. One of the methods can be done by sieve analysis of sediment, where the method illuminates the distribution of sediment changes associate with channel morphology under different flow regimes. Hence, the purpose of this mini review is to investigate how the sediment along the river meander spatially dispersed. -
PDF of Montana
USDA Farm Service Agency - Montana Office Directory Montana FSA State Office | P.O. Box 670 | Bozeman, MT 59771 | Phone: 406.587.6872 State Executive Director Mike Foster | www.fsa.usda.gov/mt | Fax: 855.546.0264 FSA Service Center Offices (Listed by County/Reservation) Phone # Fax # Beaverhead 420 Barrett Street, Dillon, MT 59725 406/683-3830 855/556-1258 Big Horn, Crow Reservation, 724 West Third, Hardin, MT 59034 406/665-3442 855/556-1457 Northern Cheyenne Reservation Blaine, Fort PO Box 307, 228 Ohio, Chinook, MT 59523 406/357-2320 855/546-0388 Belknap Reservation Ft. Belknap Service Center, 158 Tribal Way, Harlem, MT 59526 406/353-8526 855/546-0388 Broadwater 415 South Front Street, Townsend, MT 59644 406/266-4253 855/575-2506 PO Box 509, 606 W Front Street, Joliet, MT 59041- Carbon 406/962-3300 855/558-5641 0136 Carter PO Box 5, 308 S. Mormon Ave., Ekalaka, MT 59324 406/775-6355 855/556-1271 Cascade 12 3rd St NW, Suite 300, Great Falls, MT 59404 406/727-7580 866/609-8434 PO Box 309, 1210 25th Street, Fort Benton, Chouteau 406/622-5401 855/556-1450 MT 59442-0309 Custer 3120 Valley Drive East, Miles City, MT 59301-5599 406/232-7905 855/558-5665 Daniels 131 B Highway 5 East, Scobey, MT 59263 406/487-5366 855/575-2501 Dawson 102 Fir Street, Glendive, MT 59330-3196 406/377-5566 855/556-1455 1002 Hollenback Road, Suite B, Deer Lodge, Deer Lodge 406/846-2337 855-547-5750 MT 59722 PO Box 1516, 141 South 4th Street West, Baker, Fallon 406/778-2238 855-510-7029 MT 59313-1516 Fergus 211 McKinley St., Suite 2, Lewistown, MT 59457 406/538-3489 855/558-5654 Flathead 133 Interstate LN, Kalispell, MT 59901-2877 406/752-4242 855/558-5653 Gallatin 3710 W. -
GLACIERS and GLACIATION in GLACIER NATIONAL PARK by J Mines Ii
Glaciers and Glacial ion in Glacier National Park Price 25 Cents PUBLISHED BY THE GLACIER NATURAL HISTORY ASSOCIATION IN COOPERATION WITH THE NATIONAL PARK SERVICE Cover Surveying Sperry Glacier — - Arthur Johnson of U. S. G. S. N. P. S. Photo by J. W. Corson REPRINTED 1962 7.5 M PRINTED IN U. S. A. THE O'NEIL PRINTERS ^i/TsffKpc, KALISPELL, MONTANA GLACIERS AND GLACIATTON In GLACIER NATIONAL PARK By James L. Dyson MT. OBERLIN CIRQUE AND BIRD WOMAN FALLS SPECIAL BULLETIN NO. 2 GLACIER NATURAL HISTORY ASSOCIATION. INC. GLACIERS AND GLACIATION IN GLACIER NATIONAL PARK By J Mines Ii. Dyson Head, Department of Geology and Geography Lafayette College Member, Research Committee on Glaciers American Geophysical Union* The glaciers of Glacier National Park are only a few of many thousands which occur in mountain ranges scattered throughout the world. Glaciers occur in all latitudes and on every continent except Australia. They are present along the Equator on high volcanic peaks of Africa and in the rugged Andes of South America. Even in New Guinea, which many think of as a steaming, tropical jungle island, a few small glaciers occur on the highest mountains. Almost everyone who has made a trip to a high mountain range has heard the term, "snowline," and many persons have used the word with out knowing its real meaning. The true snowline, or "regional snowline" as the geologists call it, is the level above which more snow falls in winter than can he melted or evaporated during the summer. On mountains which rise above the snowline glaciers usually occur.