Skyline Drive - South District Shenandoah National Park Table of Contents
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SNP Spring Opening Dates 2021
National Park Service Office of the Superintendent U.S. Department of the Interior 3655 U.S. Highway 211 East Luray, VA 22835 FOR IMMEDIATE RELEASE Sally Hurlbert (540) 999-3500 x3300 March 24, 2021 [email protected] Shenandoah National Park News Release Shenandoah National Park Announces Spring Opening Dates Luray, Virginia: Facilities in Shenandoah National Park are beginning to open and will continue to open throughout the spring. The park’s two visitor centers are now open with rangers providing information at outdoor contact stations and the Park Stores located inside are open with limited capacity. They are operating on the following schedules: Dickey Ridge Visitor Center (mile 4.6 Skyline Drive) • Open Fridays through Tuesdays, 9:00 a.m. – 5:00 p.m. (closed on Wednesdays and Thursdays), No indoor exhibits or films. Byrd Visitor Center (mile 51 Skyline Drive) • Open 7 days a week, 9:00 a.m. – 5:00 p.m., No indoor exhibits or films. Campgrounds will open on the following schedule: • March 25: Lewis Mountain Campground (mile 57.5) • March 26: Big Meadows Campground (mile 51.2) • May 5: Mathews Arm Campground (mile 22.2), Loft Mountain Campground (mile 79.5), and Dundo Group Campground (mile 83.7) Picnic Grounds will open on the following schedule: • March 25: Lewis Mountain Picnic Grounds (mile 57.5) • March 26: Big Meadows Picnic Grounds (mile 51.2) • Open year round: Dickey Ridge Picnic Grounds (mile 4.7), Elkwallow Picnic Grounds (mile 24.1), Pinnacles Picnic Grounds (mile 36.7), South River Picnic Grounds (mile 62.8), and -
Birds Rockingham County
BIRDS OF ROCKINGHAM COUNTY VIRGINIA Clair Mellinger, Editor Rockingham Bird Club o DC BIRDS OF ROCKINGHAM COUNTY VIRGINIA Clair Mellinger, Editor Rockingham Bird Club November 1998 TABLE OF CONTENTS FOREWORD AND ACKNOWLEDGEMENTS............................1 THE ENVIRONMENT....................................................................3 THE PEOPLE AND THE RECORDS........................................11 THE LOCATIONS........................................................................23 DEFINITIONS AND EXPLANATIONS......................................29 SPECIES ACCOUNTS...............................................................33 LITERATURE CITED................................................................ 113 INDEX...........................................................................................119 PHOTOGRAPHS OF THE AMERICAN GOLDFINCHES ON THE FRONT AND BACK COVER WERE GENEROUSLY PROVIDED BY JOHN TROTT. The American Goldfinch has been used as the emblem for the Rockingham Bird Club since the club’s establishment in 1973. Copyright by the Rockingham Bird Club November 1998 FOREWORD AND ACKNOWLEDGMENTS This book is the product and a publication of the Rockingham Bird Club. It is a compilation of many historical and more recent records of bird sightings in Rockingham County. The primary purpose of the book is to publish Rockingham County bird records that may otherwise be unavailable to the general public. We hope that these records will serve a variety of useful purposes. For example, we hope that it will be useful to new (and experienced) birders as a guide to when and where to look for certain species. Researchers may find records or leads to records of which they were unaware. The records may support or counterbalance ideas about the change in species distribution and abundance. It is primarily a reference book, but fifty years from now some persons may even find the book interesting to read. In the Records section we have listed some of the persons who contributed to this book. -
Where Is Afton Mountain? Christopher M
Worthy Field Locales THE GEOLOGY of VIRGINIA Mind the Gap! Where is Afton Mountain? Christopher M. Bailey, College of William & Mary Ask Virginians where the top of Afton y e Mountain is located, and they will ll likely tell you “it’s the place where a V s Interstate 64 crosses the Blue Ridge h n Mountains between Charlottesville and a i o ta Staunton”. The trouble with that de- d n n u scription is this: Interstate 64 crests the a o Blue Ridge Mountains at Rockfish Gap. n M e So where exactly is Afton Mountain? h Waynesboro S Look on the U.S. Geological Survey’s ge topographic map of the area and you’ll id not find an Afton Mountain. Afton is a R I-64 small town located on the slopes of the Blue Ridge about a mile to the east of Rockfish Gap. Interstate 64 cuts a long e gentle grade across the southern slope lu Rockfish of the Blue Ridge topping out at 1900 ft B Gap (580 m) above sea level at Rockfish Gap before descending westward into the 0 3 miles Shenandoah Valley. Rockfish Gap has 0 5 N long been an important nexus between kilometers the Piedmont and Shenandoah Valley, False color satellite image of the Blue Ridge Mountains, Shenandoah but as we shall see it is also a fascinat- Valley, and Rockfish Gap. ing geological locale. Rockfish Gap C. M. Bailey, W&M Geology Oblique aerial photo of Rockfish Gap and the crest of the Blue Ridge Mountains as viewed from the south-southeast. -
Scenic Landforms of Virginia
Vol. 34 August 1988 No. 3 SCENIC LANDFORMS OF VIRGINIA Harry Webb . Virginia has a wide variety of scenic landforms, such State Highway, SR - State Road, GWNF.R(T) - George as mountains, waterfalls, gorges, islands, water and Washington National Forest Road (Trail), JNFR(T) - wind gaps, caves, valleys, hills, and cliffs. These land- Jefferson National Forest Road (Trail), BRPMP - Blue forms, some with interesting names such as Hanging Ridge Parkway mile post, and SNPMP - Shenandoah Rock, Devils Backbone, Striped Rock, and Lovers Leap, National Park mile post. range in elevation from Mt. Rogers at 5729 feet to As- This listing is primarily of those landforms named on sateague and Tangier islands near sea level. Two nat- topographic maps. It is hoped that the reader will advise ural lakes occur in Virginia, Mountain Lake in Giles the Division of other noteworthy landforms in the st& County and Lake Drummond in the City of Chesapeake. that are not mentioned. For those features on private Gaps through the mountains were important routes for land always obtain the owner's permission before vis- early settlers and positions for military movements dur- iting. Some particularly interesting features are de- ing the Civil War. Today, many gaps are still important scribed in more detail below. locations of roads and highways. For this report, landforms are listed alphabetically Dismal Swamp (see Chesapeake, City of) by county or city. Features along county lines are de- The Dismal Swamp, located in southeastern Virginia, scribed in only one county with references in other ap- is about 10 to 11 miles wide and 15 miles long, and propriate counties. -
Blue Ridge Park Way DIRECTORY TRAVEL PLANNER
65 TH Edition Blue Ridge Park way www.blueridgeparkway.org DIRECTORY TRAVEL PLANNER Includes THE PARKWAY MILEPOST Biltmore Asheville, NC Exit at Milepost 388.8 Grandfather Mountain Linville, NC Exit at Milepost 305.1 Roanoke Star and Overlook Roanoke, VA Exit at Milepost 120 Official Publication of the Blue Ridge Parkway Association The 65th Edition OFFICIAL PUBLICATION BLUE RIDGE PARKWAY ASSOCIATION, INC. P. O. BOX 2136, ASHEVILLE, NC 28802 (828) 670-1924 www.blueridgeparkway.org • [email protected] COPYRIGHT 2014 NO Portion OF THIS GUIDE OR ITS MAPS may BE REPRINTED WITHOUT PERMISSION. ALL RIGHTS RESERVED. PRINTED IN THE USA. Some Parkway photographs by William A. Bake, Mike Booher, Vicki Dameron and Jeff Greenberg © Blue Ridge Parkway Association Layout/Design: Imagewerks Productions: Arden, NC This free Directory & Travel PROMOTING Planner is published by the 500+ member Blue Ridge TOURISM FOR Parkway Association to help Chimney Rock at you more fully enjoy your Chimney Rock State Park Parkway area vacation. MORE THAN Members representing attractions, outdoor recre- ation, accommodations, res- Follow us for more Blue Ridge Parkway 60 YEARS taurants, shops, and a variety of other services essential to information and resources: the traveler are included in this publication. When you visit their place of business, please let them know www.blueridgeparkway.org you found them in the Blue Ridge Parkway Directory & Travel Planner. This will help us ensure the availability of another Directory & Travel Planner for your next visit -
Full Press Release of Shenandoah National Park Changes Entrance
National Park Service Office of the Superintendent U.S. Department of the Interior 3655 U.S. Highway 211 East Luray, VA 22835 540-999-3500 phone www.nps.gov/shen Shenandoah National Park News Release Release Date: April 13, 2018 Contact: Sally Hurlbert, [email protected], 540-999-3500 ext. 3300 Shenandoah National Park Changes Entrance Fee to Address Infrastructure Needs & Improve Visitor Experience Luray, Virginia: The National Park Service (NPS) announced today that Shenandoah National Park will modify its entrance fees beginning June 1, 2018 to provide additional funding for infrastructure and maintenance needs that enhance the visitor experience. Effective June 1, 2018 the park entrance fee will be $30 per vehicle, $25 per motorcycle and $15 per person. These fees are good for 7 days. An annual park pass will cost $55. In October 2017, the NPS proposed a plan to adopt seasonal pricing at Shenandoah and 16 other national parks to raise additional revenue for infrastructure and maintenance needs. The fee structure announced today addresses many concerns and ideas provided by the public on how best to address fee revenue for parks. Revenue from entrance fees remains in the National Park Service and helps ensure a quality experience for all who visit. Here in Shenandoah National Park, 80 percent of entrance fees stay in the park and are devoted to spending that supports the visitor. We share the other 20 percent of entry fee income with other national parks for their projects. The additional revenue from entrance fees at Shenandoah -
Appendix C Historic Resources
APPENDIX C HISTORIC RESOURCES HISTORIC RESOURCES APPENDIX – Adopted November 14, 2013 Page 1 HISTORIC RESOURCES The following Historic Resources appendix resources have been studied and documented to satisfy Virginia State Code Sec. 15.2-2224, Surveys and studies to be made in preparation of plan; implementation of plan. Additionally, the information is an educational resource for the community, offering valuable insights into environmental and land use planning within Spotsylvania County. HISTORY OF SPOTSYLVANIA COUNTY A timeless sense of self, place and community are at the center of life. Spotsylvania’s heritage supports this truth as the foundation for present and future change. A preservation plan, therefore, includes a summary of character defining history. The following time periods have been established by the Virginia Department of Historic Resources for use in cultural resource documentation. Pre Historic Native American, Late Woodland Period, Pre 1607 Before European settlement, present day Spotsylvania County was home to the Siouan tribes. While these Native Americans were dominantly nomadic, there tended to be an ethnic division of land among them. The Fall Line marked the boundary between the Coastal Algonquians and the Piedmont Siouan- speakers at the end of the Late Woodland period. The land between the North Anna and Rappahannock Rivers, principally roamed by the Manahoacs, formed the region that later became Spotsylvania County. Settlement to Society, 1607-1750 Forts and friendly Indian settlements were established as the first colonists arrived from Europe. Alexander Spotswood was appointed Lieutenant Governor to the Colony of Virginia in 1710, and playing a significant role in westward expansion. Importing German immigrants, mainly indentured servants, he devised a settlement based on iron ore discoveries along the Rapidan River, and founded the County of Spotsylvania in 1721. -
Quaternary Deposits and Landscape Evolution of the Central Blue Ridge of Virginia
Geomorphology 56 (2003) 139–154 www.elsevier.com/locate/geomorph Quaternary deposits and landscape evolution of the central Blue Ridge of Virginia L. Scott Eatona,*, Benjamin A. Morganb, R. Craig Kochelc, Alan D. Howardd a Department of Geology and Environmental Science, James Madison University, Harrisonburg, VA 22807, USA b U.S. Geological Survey, Reston, VA 20192, USA c Department of Geology, Bucknell University, Lewisburg, PA 17837, USA d Department of Environmental Sciences, University of Virginia, Charlottesville, VA 22904, USA Received 30 August 2002; received in revised form 15 December 2002; accepted 15 January 2003 Abstract A catastrophic storm that struck the central Virginia Blue Ridge Mountains in June 1995 delivered over 775 mm (30.5 in) of rain in 16 h. The deluge triggered more than 1000 slope failures; and stream channels and debris fans were deeply incised, exposing the stratigraphy of earlier mass movement and fluvial deposits. The synthesis of data obtained from detailed pollen studies and 39 radiometrically dated surficial deposits in the Rapidan basin gives new insights into Quaternary climatic change and landscape evolution of the central Blue Ridge Mountains. The oldest depositional landforms in the study area are fluvial terraces. Their deposits have weathering characteristics similar to both early Pleistocene and late Tertiary terrace surfaces located near the Fall Zone of Virginia. Terraces of similar ages are also present in nearby basins and suggest regional incision of streams in the area since early Pleistocene–late Tertiary time. The oldest debris-flow deposits in the study area are much older than Wisconsinan glaciation as indicated by 2.5YR colors, thick argillic horizons, and fully disintegrated granitic cobbles. -
Catoctin Formation
Glimpses of the Past: THE GEOLOGY of VIRGINIA The Catoctin Formation — Virginia is for Lavas Alex Johnson and Chuck Bailey, Department of Geology, College of William & Mary Stony Man is a high peak in Virginia’s Blue Ridge Mountains that tops out at just over 1200 m (4,000’). Drive south from Thornton Gap along the Skyline Drive and you’ll see the impressive cliffs of Stony Man’s northwestern face. These are the cliffs that give the mountain its name, as the cliffs and slopes have a vague resemblance to a reclining man’s forehead, eye, nose, and beard. Climb to the top and you’ll see peculiar bluish-green rocks exposed on the summit that are ancient lava flows, part of a geologic unit known as the Catoctin Formation. From the presidential retreat at Camp David to Jefferson’s Monticello, from Harpers Ferry to Humpback Rocks, the Catoctin Formation underlies much of the Blue Ridge. This distinctive geologic unit tells us much about the long geologic history of the Blue Ridge and central Appalachians. Stony Man’s summit and northwestern slope, Shenandoah National Park, Virginia. Cliffs expose metabasaltic greenstone of the Neoproterozoic Catoctin Formation. (CMB photo). Geologic cross section of Stony Man summit area (modified from Badger, 1999). The Catoctin Formation was first named by Arthur Keith in 1894 and takes its name for exposures on Catoctin Mountain, a long ridge that stretches from Maryland into northern Virginia. The word Catoctin is rooted in the old Algonquin term Kittockton. The exact meaning of the term has become a point of contention; among historians the translation “speckled mountain” is preferred, however local tradition holds that that Catoctin means “place of many deer” (Kenny, 1984). -
Shenandoah National Park Project Virginia
SHENANDOAH NATIONAL PARK PROJECT VIRGINIA White Oak Canyon UNITED STATES SHENANDOAH NATIONAL PARK PROJECT DEPARTMENT OF THE INTERIOR Harold L. Ickes, Secretary In the Blue Ridge Mountains of Virginia NATIONAL PARK SERVICE Arno B. Cammerer, Director national park in the Virginia section of the Blue Ridge Mountains was authorized by an act of Congress approv A ed May 22, 1926. The act specified that when title to 250,000 acres of a tract of land approved by the Secretary of the Interior should be vested in the United States, it would constitute a national park dedicated and set apart for the benefit and enjoyment of the people, and the Government would VIRGINIA STATE COMMISSION proceed with the installation of accommodations for visitors, ON the development of an adequate road and trail system, the CONSERVATION AND DEVELOPMENT stocking of fishing streams, and the inauguration of an educa William E. Carson, Chairman tional service to acquaint the public with the historical back ground and natural beauty of this famous region. Upon the passage of the act, the State of Virginia, through its Commission on Conservation and Development, im mediately began the work of acquiring the money to purchase SHENANDOAH NATIONAL PARK PROJECT the necessary land. This was a tremendous undertaking as the approved area was made up of thousands of parcels of privately VIRGINIA owned land. Funds were raised through State appropriations, contributions from citizens of Virginia, and from outside sources. The work moved forward with all possible expediency until the period of general depression set in, and it became increasingly difficult to obtain funds. -
Acid Rain in Shenandoah National Park, Virginia
Prepared in cooperation with the National Park Service Acid Rain in Shenandoah National Park, Virginia Visitors to Shenandoah National Park (SNP) enjoy the animal and plant The pH scale is a measure of how acidic (low pH) or alkaline life and the scenery but may not real- (high pH) a solution is. Rainwater is considered normal at 5.6 pH ize how vulnerable these features are to units. Shenandoah National Park rain typically is 10 times more various threats, such as invasion of exotic acidic than normal rain. plants and insects, improper use of park resources by humans, and air and water pollution. The National Park Service rain (currently about 4.6 pH units) falling mic, which means that each whole-num- strives to protect natural resources from onto an environment that has little inher- ber change indicates a 10-fold change in such threats to ensure that the resources ent ability to neutralize the acidic input acidity or alkalinity. For example, a pH of will be available for enjoyment now and and decades of exposure to acid rain have 4 is 10 times more acidic than a pH of 5. in the future. Because SNP has limited resulted in a fragile environment. When Rainwater is considered normal at 5.6 pH influence over the air pollution that the effects of acid rain are combined units; therefore, rain with a pH of 4.6, envelops the region, acidic deposition— with stressors, such as forest defoliation which typically occurs in SNP, is about commonly known as acid rain—is one of caused by the gypsy moth or conifer- 10 times more acidic than normal rain. -
History of Virginia
14 Facts & Photos Profiles of Virginia History of Virginia For thousands of years before the arrival of the English, vari- other native peoples to form the powerful confederacy that con- ous societies of indigenous peoples inhabited the portion of the trolled the area that is now West Virginia until the Shawnee New World later designated by the English as “Virginia.” Ar- Wars (1811-1813). By only 1646, very few Powhatans re- chaeological and historical research by anthropologist Helen C. mained and were policed harshly by the English, no longer Rountree and others has established 3,000 years of settlement even allowed to choose their own leaders. They were organized in much of the Tidewater. Even so, a historical marker dedi- into the Pamunkey and Mattaponi tribes. They eventually cated in 2015 states that recent archaeological work at dissolved altogether and merged into Colonial society. Pocahontas Island has revealed prehistoric habitation dating to about 6500 BCE. The Piscataway were pushed north on the Potomac River early in their history, coming to be cut off from the rest of their peo- Native Americans ple. While some stayed, others chose to migrate west. Their movements are generally unrecorded in the historical record, As of the 16th Century, what is now the state of Virginia was but they reappear at Fort Detroit in modern-day Michigan by occupied by three main culture groups: the Iroquoian, the East- the end of the 18th century. These Piscataways are said to have ern Siouan and the Algonquian. The tip of the Delmarva Penin- moved to Canada and probably merged with the Mississaugas, sula south of the Indian River was controlled by the who had broken away from the Anishinaabeg and migrated Algonquian Nanticoke.