Through Yellowstone National Park
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Recreational Trails Master Plan
Beaverhead County Recreational Trails Master Plan Prepared by: Beaverhead County Recreational Trails Master Plan Prepared for: Beaverhead County Beaverhead County Commissioners 2 South Pacific Dillon, MT 59725 Prepared by: WWC Engineering 1275 Maple Street, Suite F Helena, MT 59601 (406) 443-3962 Fax: (406) 449-0056 TABLE OF CONTENTS Executive Summary ...................................................................................................... 1 Overview ...................................................................................................................... 1 Public Involvement .................................................................................................... 1 Key Components of the Plan ..................................................................................... 1 Intent of the Plan ....................................................................................................... 1 Chapter 1 - Master Plan Overview................................................................................ 3 1.1 Introduction ........................................................................................................... 3 1.1.1 Project Location ............................................................................................... 3 1.2 Project Goals ......................................................................................................... 3 1.2.1 Variety of Uses ................................................................................................ -
Blacktail Deer Creek
U.S. Department of the Interior National Park Service Yellowstone Center for Resources Fisheries and Aquatic Sciences Program P.O. Box 168 Yellowstone National Park, Wyoming 82190 Cutthroat Trout Restoration Across Yellowstone’s Northern Range Phase I Completion Report YCR-2007-05 By: Michael E. Ruhl and Todd M. Koel 30 September 2007 Suggested citation: Ruhl, M.E. and T.M. Koel. 2007. Cutthroat trout restoration across Yellowstone’s Northern Range: Phase I completion report. National Park Service, Yellowstone Center for Resources, Fisheries & Aquatic Sciences Program, Yellowstone National Park, Wyoming, YCR-2007-05. ii CONTENTS EXECUTIVE SUMMARY...................................................................................... iv INTRODUCTION ....................................................................................................... 1 BACKGROUND .......................................................................................................... 4 Yellowstone National Park and Native Species Restoration ........................................ 4 The National Park Service and Native Fish Restoration............................................. 5 METHODS..................................................................................................................... 6 Literature Review ........................................................................................................... 6 Field Investigations....................................................................................................... -
Magnitude and Frequency of Floods in the United States Part 6-A
Magnitude and Frequency of Floods in the United States Part 6-A. Missouri River Basin above Sioux Cit'% Iowa By JAMES L. PATTERSON GEOLOGICAL SURVEY WATER-SUPPLY PAPER 1679 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1966 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director Library of Congress catalog-card No. GS 64-192 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Abstract _________________________________________ 1 Introduction _______________________________ 1 Purpose and scope_________________________ 1 Acknowledgments ________________________ _ 3 Application of flood-frequency data_____________________ _ 3 Regional application_____________________________ _ 4 Special application______________________________ 7 Streams affected by regulation or diversion________________ 11 Description of the area__________ ____________ _ 12 River basins____________________________________ 12 Topography ____________________________________ 12 Climate ______________________________________ 13 Flood-frequency analysis______________________________ 13 Method of analysis_______________________________ 13 Records used___________________________________ 14 Flood frequency at a gaging station___________________.__ 14 Types of flood series_____________________ 14 Flood-frequency curves___________________ 15 Regional flood frequency______________________________ 17 Mean annual flood__________________________ 17 Composite -
Beaverhead River and Splits Enhanced Hydraulic Analysis and Floodplain Mapping Report Beaverhead County, MT
Beaverhead River and Splits Enhanced Hydraulic Analysis and Floodplain Mapping Report Beaverhead County, MT October 2018 Beaverhead River and Splits Enhanced Hydraulic Analysis And Floodplain Mapping Report Beaverhead County, MT Prepared For: Montana Department of Natural Resources and Conservation Prepared By: Michael Baker International Table of Contents 1. INTRODUCTION AND BACKGROUND ....................................................................................................... 1 1.1. COMMUNITY DESCRIPTION ........................................................................................................................... 3 1.2. BASIN DESCRIPTIONS .................................................................................................................................... 6 1.2.1 Beaverhead River ..................................................................................................................................... 6 1.2.2 Beaverhead River Overbank .................................................................................................................... 8 1.2.3 Dillon Canal ............................................................................................................................................ 9 1.2.4 Guidici Ditch ......................................................................................................................................... 10 1.2.5 Murray Gilbert Slough.......................................................................................................................... -
YELLOWSTONE National Park WYOMING - MONTANA- IDAHO
YELLOWSTONE National Park WYOMING - MONTANA- IDAHO UNITED STATES RAILROAD ADMINISTRATION N AT IONAU PARK SERIES Copyright by Hayncs, St. Paul Riverside Geyser—Unlike most Geysers it spouts obliquely instead of vertically. Its arching column of water is thrown into the Fireholc River Page two An Appreciation of Yellowstone National Park By EMERSON HOUGH Author oj "<CTic Mississippi Bubble" "54-40 or Fight" "'Che Way to the West," etc. Written Especially for the United States Railroad Administration FTER every war there comes a day of diligence. Usually war is followed by a rush of soldiers back to the soil. We have 3,000,000 soldiers, a large per cent of whom are seeking farms. This means the early use of every reclaimable acre of American soil. 11 means that the wildernesses of America soon will be no more. Our great National Parks are sections of the old American wilder ness preserved practically unchanged. They are as valuable, acre for acre, as the richest farm lands. They feed the spirit, the soul, the character of America. Who can measure the value, even to-day, of a great national reserve such as the Yellowstone Park? In twenty years it will be beyond all price, for in twenty years we shall have no wild America. The old days are gone forever. Their memories are ours personally. We ought personally to understand, to know, to prize and cherish them. Of all the National Parks Yellowstone is the wildest and most universal in its appeal. There is more to see there—more different sorts of things, more natural wonders, more strange and curious things, more scope, more variety—a longer list of astonishing sights—than any half dozen of the other parks combined could offer. -
OVERCOMING OBSCURITY the Yellowstone Architecture of Robert C
OVERCOMING OBSCURITY The Yellowstone Architecture of Robert C. Reamer Ruth Quinn MONTANA HISTORICAL SOCIETY LIBRARY, F.J. HAYNES ARCHITECTURAL DRAWINGS COLLECTION A Reamer drawing of the proposed Canyon Hotel, built in 1910. COURTESY QUINN RUTH “His friends know he appears to be looking down, while he builds looking up.…The effort to impress is not his. He is too busy looking down…creating.” IRST-TIME CALLERS to the Xanterra Central Reservations Offi ce in Yellow- Fstone frequently make their fi rst request a stay at the Old Faithful Inn. They do not always know what to call it; they say “Old Faithful Lodge” more often than not. Yet it is the lodging facility in Yellowstone that everyone seems to know. It may well be the second most famous feature in Yellowstone, after Old Faithful Geyser itself. By contrast, last summer a woman came into the inn looking for the plaque bearing the architect’s name—and, rare among visitors, she already knew it. She was visiting from name a handful. Most of us are aware of his contributions Oberlin, Ohio, the place of Robert Reamer’s birth. Unfortu- to the Old Faithful Inn, the Lake Hotel, the Mammoth Hot nately, she found no such plaque at the Old Faithful Inn. It Springs Hotel, and the demolished Grand Canyon Hotel. is diffi cult to fi nd Reamer’s name anywhere around the park, His name is also well associated with the Executive House at even in the Yellowstone building that has come to be so power- Mammoth. (He has also received credit, in error I believe, for fully linked with him—the building that has for many people the Norris Soldier Station, the Roosevelt Arch, and the Lake come to defi ne what they admiringly, if inaccurately, think of Lodge.) But these well-known projects account for only a part as the “Reamer style.” of the work he did for Yellowstone, work that should arguably Ten years ago, when I fi rst read that Robert Reamer had have made his name among the best-known in the history of designed more than 25 projects for the park, I was astonished the park. -
Compiled by C.J. Harksen and Karen S. Midtlyng Helena, Montana June
WATER-RESOURCES ACTIVITIES OF THE U.S. GEOLOGICAL SURVEY IN MONTANA, OCTOBER 1989 THROUGH SEPTEMBER 1991 Compiled by C.J. Harksen and Karen S. Midtlyng U.S. GEOLOGICAL SURVEY Open-File Report 91-191 Prepared in cooperation with the STATE OF MONTANA AND OTHER AGENCIES Helena, Montana June 1991 U.S. DEPARTMENT OF THE INTERIOR MANUEL LUJAN, JR., Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director For additional information Copies of this report can be write to: purchased from: District Chief U.S. Geological Survey U.S. Geological Survey Jooks and Open-File Reports Section 428 Federal Building federal Center, Building 810 301 South Park, Drawer 10076 iox 25425 Helena, MT 59626-0076 Denver, CO 80225-0425 CONTENTS Page Message from the District Chief. ....................... 1 Abstract ................................... 3 Basic mission and programs .......................... 3 U.S. Geological Survey ........................... 3 Water Resources Division .......................... 4 District operations. ............................. 4 Operating sections ............................. 5 Support units. ............................... 5 Office addresses .............................. 5 Types of funding .............................. 8 Cooperating agencies ............................ 10 Hydrologic conditions ............................ 10 Data-collection programs ........................... 13 Surface-water stations (MT001) ....................... 16 Ground-water stations (MT002)........................ 17 Water-quality stations (MT003) ...................... -
Structural Geology of the Northern Snowcrest Range, Beaverhead and Madison Counties, Montana
Western Michigan University ScholarWorks at WMU Master's Theses Graduate College 4-1984 Structural Geology of the Northern Snowcrest Range, Beaverhead and Madison Counties, Montana Mark Kenneth Sheedlo Follow this and additional works at: https://scholarworks.wmich.edu/masters_theses Part of the Geology Commons Recommended Citation Sheedlo, Mark Kenneth, "Structural Geology of the Northern Snowcrest Range, Beaverhead and Madison Counties, Montana" (1984). Master's Theses. 1571. https://scholarworks.wmich.edu/masters_theses/1571 This Masters Thesis-Open Access is brought to you for free and open access by the Graduate College at ScholarWorks at WMU. It has been accepted for inclusion in Master's Theses by an authorized administrator of ScholarWorks at WMU. For more information, please contact [email protected]. STRUCTURAL GEOLOGY OF THE NORTHERN SNOWCREST RANGE, BEAVERHEAD AND MADISON COUNTIES, MONTANA by Mark Kenneth Sheedlo A Thesis Submitted to the Faculty of The Graduate College in partial fu lfillm e n t of the requirements for the Degree of Master of Science Department of Geology Western Michigan University Kalamazoo, Michigan April 1984 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission STRUCTURAL GEOLOGY OF THE NORTHERN SNOWCREST RANGE, BEAVERHEAD AND MADISON COUNTIES, MONTANA Mark Kenneth Sheedlo, M.S. Western Michigan University, 1984 The Snowcrest Range was uplifted in Late Cretaceous and Early •Tertiary time as a consequence of thrusting in Precambrian basement and Phanerozoic cover rocks. The Snowcrest-Greenhorn thrust system is associated with large- scale overturned, eastward verging folds. Mean orientation of the thrust system is N.40°E., 35°N.W.. The trend of the thrust system and associated transverse faults appear to be controlled by earlier structures. -
WORK PLAN BEAVERHEAD RIVER WATERSHED UPDATED:September, 2007
WORK PLAN BEAVERHEAD RIVER WATERSHED UPDATED:September, 2007 INTRODUCTION PURPOSE The purpose for this watershed plan is to: (1) Identify and document resource concerns within the watershed, both water and non- water related. (2) Prioritize those concerns (3) Outline objectives and methods of addressing those concerns (4) Provide guidance in the implementation of action plans and other associated watershed activities. This document will be maintained as a guide for watershed activities, and will be updated on a regular basis to reflect current circumstances in the watershed including reprioritization of concerns and addition of new areas of concentration. BEAVERHEAD RIVER WATERSHED COMMITTEE – MISSION STATEMENT The mission of the Beaverhead Watershed Committee is to seek an understanding of the watershed – how it functions and supports the human communities dependent upon it – and to build agreement on watershed-related planning issues among stakeholders with diverse viewpoints. Goals: . Provide a mechanism and forum for landowners, citizens, and agencies to work together to: . Identify problems and concerns both riparian and non-riparian, urban and rural. Reach agreement upon the priority of and methods for addressing those concerns. Act as a conduit between local interests and agencies for purposes of procuring the funding and non-monetary assistance necessary to begin systematically addressing priority concerns. Foster a cooperative environment where conflict is avoided, and work to resolve conflict as necessary for the watershed effort to move forward. Stay abreast of opportunities, issues, and developments that could be either beneficial or detrimental to the watershed or segments of the watershed. Keep stakeholders appropriately informed. Objectives: . Continuous Improvement – Maintain a broad range of active improvement projects/programs relating to diverse attributes of the watershed. -
YELLOWSTONE NATIONAL PARK R N C Hard-Sided Camping Units Only C E Perc an Ez Pelic N See Detail Map Above PE L LICAN
Services and Facilities Mammoth Hot Springs Old Faithful Canyon Village West Thumb Fishing Bridge, Lake Village 6239ft 1902m 7365ft 2254m 7734ft 2357m and Grant Village 7733ft 2357m and Bridge Bay 7784ft 2373m 0 0.1 0.5 Km To Gardiner To Madison To Tower-Roosevelt To Lake Village 0 0.5 Km To Canyon Emergencies Check the park news- Mammoth Hot Springs Hotel Grand Geyser Amphitheater For medical or other emer- paper for seasonal dates Fi Duck 0 0.1 Mi 0.5 Post Amphitheater re To Norris 0 0.5 Mi h gencies contact a ranger or of services and facilities. Office o Lake Fishing Bridge le West Thumb Ice Visitor Education call 307-344-7381 or 911. Geyser Amphitheater Hill West Thumb Castle Center Showers-Laundry Ranger station To Geyser Basin Geyser Ri Old Ice Upper Terrace Drive: Park ve Canyon Lodge Medical clinic r Faithful Visitor Headquarters no buses, RVs, or trailers; y Information Station Campground a closed in winter Center To East HISTORIC w Bookstore - Showers Entrance Winter road closures FORT e n Laundry YELLOWSTONE o YELLOWSTONE From early November to Lodging Lake Village Post early May most park roads LOWER Office Lake Lodge UPPER TERRACES Chapel Old Faithful Inn Old Faithful LAKE are closed. The exception Food service TERRACES AREA Geyser Lower Falls is the road in the park AREA Old 308ft Upper Lookout between the North one-way Faithful Falls 94m Fishing Bridge Picnic area To Point Amphitheater North Lodge View Grand Recreational Vehicle Park Entrance and Cooke City. Inspiration hard-sided camping units only Entrance Post Office View Point It is open all year. -
Geology GEOLOGY
The landscape of Yellowstone National Park is the result of many geological processes. Here, glacial erratics (foreground), ground moraines (midground), and Cutoff Mountain (background) appear near Junction Butte. Geology GEOLOGY The landscape of the Greater Yellowstone Ecosystem miles in diameter) is extremely hot but solid due to is the result various geological processes over the last immense pressure. The iron and nickel outer core 150 million years. Here, Earth’s crust has been com- (1,400 miles thick) is hot and molten. The mantle pressed, pulled apart, glaciated, eroded, and subjected (1,800 miles thick) is a dense, hot, semi-solid layer to volcanism. All of this geologic activity formed the of rock. Above the mantle is the relatively thin crust, mountains, canyons, and plateaus that define the natu- three to 48 miles thick, forming the continents and ral wonder that is Yellowstone National Park. ocean floors. While these mountains and canyons may appear In the key principles of Plate Tectonics, Earth’s to change very little during our lifetime, they are still crust and upper mantle (lithosphere) is divided into highly dynamic and variable. Some of Earth’s most active volcanic, hydrothermal (water + heat), and Yellowstone’s Geologic Significance earthquake systems make this national park a price- less treasure. In fact, Yellowstone was established as Yellowstone continues today as a natural geologic the world’s first national park primarily because of laboratory of active Earth processes. its extraordinary geysers, hot springs, mudpots and • One of the most geologically dynamic areas on Earth due to a shallow source of magma and resulting steam vents, as well as other wonders such as the volcanic activity Grand Canyon of the Yellowstone River. -
Yellowstone National Park Resources and Issues: Geology
The landscape of Yellowstone National Park is the result of many geological processes. Here, glacial erratics (foreground), ground moraines (midground), and Cutoff Mountain (background) appear near Junction Butte. Geology GEOLOGY The landscape of the Greater Yellowstone Ecosystem miles in diameter) is extremely hot but solid due to is the result various geological processes over the last immense pressure. The iron and nickel outer core 150 million years. Here, Earth’s crust has been com- (1,400 miles thick) is hot and molten. The mantle pressed, pulled apart, glaciated, eroded, and subjected (1,800 miles thick) is a dense, hot, semi-solid layer to volcanism. This geologic activity formed the moun- of rock. Above the mantle is the relatively thin crust, tains, canyons, plateaus, and hydrothermal features three to 48 miles thick, forming the continents and that define the natural wonder that is Yellowstone. ocean floors. While these mountains and canyons may appear In the key principles of Plate Tectonics, Earth’s to change very little during our lifetime, they are still crust and upper mantle (lithosphere) is divided into highly dynamic and variable. Some of Earth’s most active volcanic, hydrothermal (water + heat), and Yellowstone’s Geologic Signifcance earthquake systems make this national park a price- less treasure. In fact, Yellowstone was established as Yellowstone continues today as a natural geologic the world’s first national park primarily because of laboratory of active Earth processes. its extraordinary geysers, hot springs, mudpots and • One of the most geologically dynamic areas on Earth due to a shallow source of magma and resulting steam vents, as well as other wonders such as the volcanic activity.