Spring Mountains National Recreation Area Visitor Guide
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Correlation of Permian and Pennsylvanian Sections Between Egan Range and Spring Mountains Nevada
Correlation of Permian and Pennsylvanian Sections Between Egan Range and Spring Mountains Nevada By PATRICK J. BAROSH CONTRIBUTIONS TO STRATIGRAPHY GEOLOGICAL SURVEY BULLETIN 1254-1 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director U.S. GOVERNMENT PRINTING OFFICE, WASHINGTON : 1968 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 10 cents (paper cover) CONTENTS Page Abstract________________________________________________________ I 1 Introduction_ _____________________________________________________ 1 Egan Range____________________________________________ 3 Spring Mountains.________________________________________________ 3 Correlation _______________________________________________________ 3 Comparative ages.________________________________________________ 6 Conclusions.___________________ _ ________________________________ 7 References cited_________________________________________________ 7 ILLUSTRATIONS Page FIGURE 1. Index map showing location of Egan Range and Spring Mountains ____________________________________________ 12 2. Chart showing correlation of Permian and Pennsylvanian strata in the Egan Range and Spring Mountains..______ 5 in CONTRIBUTIONS TO STRATIGRAPHY CORRELATION OF PERMIAN AND PENNSYLVANIAN SECTIONS BETWEEN THE EGAN RANGE AND SPRING MOUNTAINS, NEVADA By PATRICK J. BAROSH ABSTRACT The Permian and Pennsylvanian parts of the Bird Spring Formation near Lee Canyon in the northern Spring Mountains, -
Cultural Background of the Spring Mountains National Recreation Area
American Indian Groups Recent studies of the Great Basin region, which includes the Las Vegas and Pahrump Valleys, have begun to show that people may have lived in this area as far back as 12,000 to 13,000 years ago. When people first began to arrive here, the environment was far more wet and lush than the world we know today. Lakes, playas, and marshes all existed in the area and this abundance of water led to a much greater variety of plants and animals that the people who lived here used. As the environment of the Spring Mountains changed over time, a unique physical history developed that helped it evolve into the fascinating place it is today. As the water began to dry up around 10,000 years ago, the Spring Mountains became isolated from the Great Basin mountain ecosystems and slowly the mountains were surrounded by the drier Mojave Desert. As it became warmer and drier, the mountain range also became isolated biologically. The valley floors surrounding the range act as a barrier to most plant and animal migrations, and thus many of the plants and animals found here today are either relic species or are new or evolved species found only to exist in this area. As the physical environment changed, so did the ways that people lived and used the land. American Indian groups have had a continuous presence in Southern Nevada for thousands of years and believe that the Spring Mountains are where their people were created. Because of this, the mountains are considered to be sacred and very special to them. -
Ecoregions of Nevada Ecoregion 5 Is a Mountainous, Deeply Dissected, and Westerly Tilting Fault Block
5 . S i e r r a N e v a d a Ecoregions of Nevada Ecoregion 5 is a mountainous, deeply dissected, and westerly tilting fault block. It is largely composed of granitic rocks that are lithologically distinct from the sedimentary rocks of the Klamath Mountains (78) and the volcanic rocks of the Cascades (4). A Ecoregions denote areas of general similarity in ecosystems and in the type, quality, Vegas, Reno, and Carson City areas. Most of the state is internally drained and lies Literature Cited: high fault scarp divides the Sierra Nevada (5) from the Northern Basin and Range (80) and Central Basin and Range (13) to the 2 2 . A r i z o n a / N e w M e x i c o P l a t e a u east. Near this eastern fault scarp, the Sierra Nevada (5) reaches its highest elevations. Here, moraines, cirques, and small lakes and quantity of environmental resources. They are designed to serve as a spatial within the Great Basin; rivers in the southeast are part of the Colorado River system Bailey, R.G., Avers, P.E., King, T., and McNab, W.H., eds., 1994, Ecoregions and subregions of the Ecoregion 22 is a high dissected plateau underlain by horizontal beds of limestone, sandstone, and shale, cut by canyons, and United States (map): Washington, D.C., USFS, scale 1:7,500,000. are especially common and are products of Pleistocene alpine glaciation. Large areas are above timberline, including Mt. Whitney framework for the research, assessment, management, and monitoring of ecosystems and those in the northeast drain to the Snake River. -
HISTORY of the TOIYABE NATIONAL FOREST a Compilation
HISTORY OF THE TOIYABE NATIONAL FOREST A Compilation Posting the Toiyabe National Forest Boundary, 1924 Table of Contents Introduction ..................................................................................................................................... 3 Chronology ..................................................................................................................................... 4 Bridgeport and Carson Ranger District Centennial .................................................................... 126 Forest Histories ........................................................................................................................... 127 Toiyabe National Reserve: March 1, 1907 to Present ............................................................ 127 Toquima National Forest: April 15, 1907 – July 2, 1908 ....................................................... 128 Monitor National Forest: April 15, 1907 – July 2, 1908 ........................................................ 128 Vegas National Forest: December 12, 1907 – July 2, 1908 .................................................... 128 Mount Charleston Forest Reserve: November 5, 1906 – July 2, 1908 ................................... 128 Moapa National Forest: July 2, 1908 – 1915 .......................................................................... 128 Nevada National Forest: February 10, 1909 – August 9, 1957 .............................................. 128 Ruby Mountain Forest Reserve: March 3, 1908 – June 19, 1916 .......................................... -
Framework for Springs Stewardship Program and Proposed Action Development: Spring Mountains National Recreation Area, Humboldt-Toiyabe National Forest
United States Department of Agriculture Framework for Springs Stewardship Program and Proposed Action Development: Spring Mountains National Recreation Area Humboldt-Toiyabe National Forest Forest Rocky Mountain General Technical Report Service Research Station RMRS-GTR-330 December 2014 Coles-Ritchie, Marc; Solem, Stephen J.; Springer, Abraham E.; Pendleton, Burton. 2014. Framework for Springs Stewardship Program and proposed action development: Spring Mountains National Recreation Area, Humboldt-Toiyabe National Forest. Gen. Tech. Rep. RMRS-GTR-330. Fort Collins, CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station. 63 p. Keywords: Spring stewardship, spring restoration, groundwater dependent ecosystems, watershed management, spring rehabilitation, spring maintenance AUTHORS Marc Coles-Ritchie, Ph.D., is a Vegetation Ecologist with Management and Engineering Technology International, Inc. (METI, Inc.), Salt Lake City, Utah. Stephen J. Solem is a senior advisor for natural resource planning and inventory with Management and Engineering Technology International, Inc. (METI, Inc.), Missoula, Montana. Abraham E. Springer, Ph.D., is a Hydrogeologist and Professor at Northern Arizona University and consultant to Management and Engineering Technology International, Inc. (METI, Inc.), Flagstaff, Arizona. Burton Pendleton, Ph.D., is a Research Ecologist Emeritus with the Rocky Mountain Research Station in Albuquerque, New Mexico. ACKNOWLEDGMENTS This effort was accomplished by using funding provided by the Southern Nevada Public Lands Management Act conservation initiative (Round 10). Work was performed using In-Service Agreements between the Humboldt-Toiyabe National Forest and the Rocky Mountain Research Station and under the terms and conditions of Management and Engineering Technologies International, Inc. Contract Number: AG- 3187-C-0028, Order Number: AG-3187-D-10-0126. -
The National Park System
January 2009 Parks and Recreation in the United States The National Park System Margaret Walls BACKGROUNDER 1616 P St. NW Washington, DC 20036 202-328-5000 www.rff.org Resources for the Future Walls Parks and Recreation in the United States: The National Park System Margaret Walls∗ Introduction The National Park Service, a bureau within the U.S. Department of the Interior, is responsible for managing 391 sites—including national monuments, national recreation areas, national rivers, national parks, various types of historic sites, and other categories of protected lands—that cover 84 million acres. Some of the sites, such as Yellowstone National Park and the Grand Canyon, are viewed as iconic symbols of America. But the National Park Service also manages a number of small historical sites, military parks, scenic parkways, the National Mall in Washington, DC, and a variety of other protected locations. In this backgrounder, we provide a brief history of the Park Service, show trends in land acreage managed by the bureau and visitation at National Park Service sites over time, show funding trends, and present the challenges and issues facing the Park Service today. History National parks were created before there was a National Park Service. President Ulysses S. Grant first set aside land for a “public park” in 1872 with the founding of Yellowstone. Yosemite, General Grant (now part of Kings Canyon), and Sequoia National Parks in California were created in 1890, and nine years later Mount Rainier National Park was set aside in Washington. With passage of the Antiquities Act in 1906, the President was granted authority to declare historic landmarks, historic and prehistoric structures, and sites of scientific interest as national monuments. -
Golden Gate National Recreation Area Foundation Document Overview
NATIONAL PARK SERVICE • U.S. DEPARTMENT OF THE INTERIOR Foundation Document Overview Golden Gate National Recreation Area California Contact Information For more information about the Golden Gate National Recreation Area Foundation Document, contact: [email protected] or (415) 561-4700 or write to: Superintendent, Golden Gate National Recreation Area, Building 201, Fort Mason, San Francisco, CA 94123-0022 Description The Golden Gate Bridge, constructed in the 1930s, is the most recognizable landmark in the region. The bridge and its plaza receive millions of visitors annually. Situated at the northern tip of the San Francisco Peninsula, the Presidio has been part of Golden Gate National Recreation Area since 1994. For more than 200 years, the Presidio area was used as a military base, first by Spain in the late 1700s, briefly by Mexico in the 1800s, and by the United States from 1846 onward. Golden Gate National Recreation Area is widely known for its rich natural resources as well. The park helps protect parts of 19 separate ecosystems and numerous watersheds. It is also home to more than 1,250 plant and animal species, including many sensitive, rare, threatened, and endangered Golden Gate National Recreation Area is one of the largest species such as the mission blue butterfly, northern spotted urban parks in the world. The park’s extensive collection owl, and California red-legged frog. Golden Gate National of natural, historic, and scenic resources and diverse Recreation Area lands are also coastal preserves that recreational opportunities fulfill the purpose of bringing encompass many miles of bay and ocean shoreline. “parks to the people,” particularly to the 7 million people who live in the San Francisco Bay Area. -
Mt. Baker Ski Area
Winter Activity Guide Mount Baker Ranger District North Cascades National Park Contacts Get ready for winter adventure! Head east along the Mt. Baker Mt. Baker-Snoqualmie National Forest State Road Conditions: /Mt. Baker Ranger District Washington State Dept. of Transportation Highway to access National Forest 810 State Route 20 Dial 511 from within Washington State lands and the popular Mt. Baker Ski Sedro-Woolley, WA 98284 www.wsdot.wa.gov Area. Travel the picturesque North (360) 856-5700 ext. 515 Glacier Public Service Center Washington State Winter Recreation and Cascades Highway along the Skagit 10091 Mt. Baker Highway State Sno-Park Information: Wild & Scenic River System into the Glacier, WA 98244 www.parks.wa.gov/winter heart of the North Cascades. (360) 599-2714 http://www.fs.usda.gov/mbs Mt. Baker Ski Area Take some time for winter discovery but North Cascades National Park Service Ski Area Snow Report: be aware that terrain may be challenging Complex (360) 671-0211 to navigate at times. Mountain weather (360) 854-7200 www.mtbaker.us conditions can change dramatically and www.nps.gov/noca with little warning. Be prepared and check Cross-country ski & snowshoe trails along the Mt. Baker Highway: forecasts before heading out. National Weather Service www.weather.gov www.nooksacknordicskiclub.org Northwest Weather & Avalanche For eagle watching information visit: Travel Tips Center: Skagit River Bald Eagle Interpretive Center Mountain Weather Conditions www.skagiteagle.org • Prepare your vehicle for winter travel. www.nwac.us • Always carry tire chains and a shovel - practice putting tire chains on before you head out. -
Science to Support Land Management in Southern Nevada
Chapter 6 Species of Conservation Concern and Environmental Stressors: Local, Regional, and Global Effects Steven M. Ostoja, Matthew L. Brooks, Jeanne C. Chambers, and Burton Pendleton Introduction Species conservation has traditionally been based on individual species within the context of their requisite habitat, which is generally defined as the communities and ecosystems deemed necessary for their persistence. Conservation decisions are ham- pered by the fact that environmental stressors that potentially threaten the persistence of species can operate at organizational levels larger than the habitat or home range of a focal species. Resource managers must therefore simultaneously consider local, regional, and/or global scale stressors for effective conservation and management of species of concern. The wide ranging effects associated with global stressors such as climate change may exceed or exacerbate the effects of local or regional stressors. Although resource managers may only be able to directly affect local and regional stressors, they still need to understand the direct and interactive effects of global stressors and ultimately how they affect the lands they manage. Conservation of species in southern Nevada is further complicated by the fact that the region includes one of the largest and fastest growing urban centers in North America. To accomplish the goal of species conserva- tion, resource managers must identify actionable management options that mitigate the effects of local and regional stressors in the context of the effects of global stressors that are beyond their control. Species conservation is typically focused on a subset of species often referred to as species of conservation concern that have either demonstrated considerable decline or are naturally rare or have limited distributions. -
Late Cenozoic Geomorphic History of Lee Canyon, Spring Mountains, Nevada
UNLV Theses, Dissertations, Professional Papers, and Capstones 6-1969 Late Cenozoic geomorphic history of Lee Canyon, Spring Mountains, Nevada John Henry Gucwa Pennsylvania State University - Main Campus Follow this and additional works at: https://digitalscholarship.unlv.edu/thesesdissertations Part of the Geology Commons, Geomorphology Commons, and the Sedimentology Commons Repository Citation Gucwa, John Henry, "Late Cenozoic geomorphic history of Lee Canyon, Spring Mountains, Nevada" (1969). UNLV Theses, Dissertations, Professional Papers, and Capstones. 1436. http://dx.doi.org/10.34917/3431545 This Thesis is protected by copyright and/or related rights. It has been brought to you by Digital Scholarship@UNLV with permission from the rights-holder(s). You are free to use this Thesis in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s) directly, unless additional rights are indicated by a Creative Commons license in the record and/ or on the work itself. This Thesis has been accepted for inclusion in UNLV Theses, Dissertations, Professional Papers, and Capstones by an authorized administrator of Digital Scholarship@UNLV. For more information, please contact [email protected]. The Pennsylvania State Universiti ( / . The Graduate School Department of Geology and Geophysics Late Cenozoic Geomorphic History of Lee Canyon, Spring Mountains, Nevada A Thesis in ., \ Geology \. \' by I John Henry Gucwa ( Submitted in Partial Fulfillment of the Requirements for the Degree of Master of Science June, 1969 · Date of Approval: • Head of the Department~ Geology and Geophysics i ii 1CKNOHLEDGMENTS ( 1be author wishes expressly to thank Dr. -
Lake Roosevelt National Recreation Area Foundation Document Overview
NATIONAL PARK SERVICE • U.S. DEPARTMENT OF THE INTERIOR Foundation Document Overview Lake Roosevelt National Recreation Area Washington Contact Information For more information about the Lake Roosevelt National Recreation Area Foundation Document, contact: [email protected] or (509) 754-7893 or write to: Superintendent, Lake Roosevelt National Recreation Area, 1008 Crest Drive, Coulee Dam, WA 99116 Purpose Significance Significance statements express why Lake Roosevelt National Recreation Area resources and values are important enough to merit national park unit designation. Statements of significance describe why an area is important within a global, national, regional, and systemwide context. These statements are linked to the purpose of the park unit, and are supported by data, research, and consensus. Significance statements describe the distinctive nature of the park and inform management decisions, focusing efforts on preserving and protecting the most important resources and values of the park unit. • Lake Roosevelt National Recreation Area, which includes some of the most publicly accessible shoreline in the Pacific Northwest, offers a wide range of visitor experiences and appropriate recreational opportunities. • Lake Roosevelt National Recreation Area is located within two distinct geologic provinces—the Okanogan Highlands and the Columbia Plateau—and is an outstanding and easily accessible landscape sculpted by a rare combination of sequential geologic processes: volcanism, collision of tectonic plates, continental glaciation, and cataclysmic ice age floods. • Lake Roosevelt National Recreation Area is located at a historic convergence point for numerous Pacific Northwest tribes and contains a central gathering place in their traditional homeland, including the site of the second-largest The purpose of LAKE ROOSEVELT NATIONAL prehistoric and historic Native American fishery on the RECREATION AREA is to protect, conserve, Columbia River. -
Las Vegas Is Fantastic for Destination Weddings! Residents Enjoy Our Wide-Ranging Venues Too
LAS VEGAS IS FILLED WITH EXCITING WEDDING DESTINATIONS Las Vegas is fantastic for Destination Weddings! Residents enjoy our wide-ranging venues too. Fabulous hotels and resorts present unimaginable options. Storied Las Vegas chapels and Elvis impersonators provide altogether different choices. We’ve done weddings in Madame Tussauds Wax Museum and are looking forward to our first at the Mob Museum and the Lou Ruvo Center for Brain Health. Beyond that, Las Vegas has high-end restaurants, clubs and studios that offer one-of-a-kind packages. But you may be looking for something more picturesque than any of these. You may want your wedding “in a cathedral not built by human hands”. Vegas weddings don’t have to be indoors. With sunny consistent weather, Las Vegas is a perfect place for outdoor weddings. And with hillside locations offering panoramic views, extending forty miles, you can choose among breathtaking backgrounds for your incredible day. Las Vegas weather is magnificent all year round. Our winters average 39ºF / 58ºF (December and January). In summer our mornings and nights are inviting (though in July and August our afternoon temperatures occasionally reach as high as 115ºF). Our breezes and gorgeous sunsets are legendary. Rain is infinitesimal. So terrace, gazebo, garden, lake side, golf course, park, and unique outdoor weddings are always possible – and always romantic! Whether you are hiring someone to arrange a huge wedding, or you’re preparing an intimate ceremony for just your partner and a witness or two, Las Vegas has it all. You can plan with confidence. We’ve officiated weddings while in a Limo travelling the Strip and a helicopter encir- cling the city (neither are technically “outdoors”).