Shenandoah Valley History the Ride Site Was Once a Prime Location for Smelting Pig Iron and As a Mineral Springs Resort Area for Wealthy Spa-Goers

Total Page:16

File Type:pdf, Size:1020Kb

Shenandoah Valley History the Ride Site Was Once a Prime Location for Smelting Pig Iron and As a Mineral Springs Resort Area for Wealthy Spa-Goers flora hillman national championship news Behind the NC: Shenandoah Valley history The ride site was once a prime location for smelting pig iron and as a mineral springs resort area for wealthy spa-goers part three of five parts p until the mid-1800s the Massanutten TALES FROM THE TRAIL remained a barrier to be crossed only History, Stories, and Legends of Fort Valley and the byU the occasional traders. The mountain Shenandoah Valley • Site of the 2006 AERC NC Rides range is so rugged that, to this day, only two roads still cross it. Yet, adventurous Europeans, lured by the excellent farmland of the Shenandoah Valley, shouldered their way over the summit to settle and fence their claims in Powell’s Fort Valley. As these newcomers often traveled in cultural groups to build and live together, towns and settlements began to quickly proliferate. The benign tolerance of the na- Burner’s White Sulfur Springs Resort, nestled in the Shenandoah Valley, is shown in this 19th century lithograph. Photo tive Indians began to evaporate with the courtesy of the Winchester (Virginia) Archival Library. increased pressure of this growing popula- tion, and while the early inhabitants of the night following, the smell of blood would the Fort Valley in search of excellent farm- valley suffered no reported fatalities from bring the wolves howling all around the land and timbering. Others, following on Indian attacks, during the French and Indian settlers’ homes. the enterprising, albeit illegal, heels of the War the settlers were in constant danger notorious Powell (see June EN), came to try from the Indians. Profits from pig iron their own luck in searching for the legend- A series of forts were erected at strate- Despite these constant threats to life ary Indian mines of silver and gold. gic points throughout the valley, including and limb, many people were still lured to continued on next page Keller’s Fort near what is now the Old Dominion’s vet check at Fitchett’s Field. In 1758, 50 Indians led by four Frenchmen raided a small village just west of Fort Val- ley and took 48 prisoners. After nightfall, one young boy escaped and ran 15 miles shoeless, hatless and only scantily clad over the Massanutten into the Fort Valley to Keller’s Fort for aid. A small party came back with him the next morning, but when they learned how large the force was, they gave up pursuit. Three years later some of the captured returned home. Many of the children taken lived the remainder of their lives with the Indians. Years after the raid, one woman returned home married to an Indian trader. She had forgotten her native German tongue and spoke only the Indian tongue. The increasingly annoyed Indians were not the only concern to the settlers; wolves were an even larger threat, especially to livestock. Several packs roamed the valley, the most notorious pack making a home in the large caves in the cliffs of Culler’s Gap, today known as “Wolf Den.” Remote dwellings with sheep, calves and young horses were easy targets to these crafty predators, and on butchering days, or the july 2006 • endurance news 15 national championship news . The hunt for precious metal yielded little the healthful waters while spending copi- locations, spa resorts offered a full line of in the way of profit, but the more practical- ous amounts of money to keep themselves entertainment and recreation for visitors. minded quickly honed in on the abundance generously amused at the same time. Spacious white clapboard or brick build- of iron ore in the valley. Pig iron was in Thus, the “abundance of fine mountain ings sprang up not only to house guests great demand at the time for the country’s and mineral water in the Fort . not surpassed with space for elegant dining and dancing, growing economy, and in due time Fort or even equaled anywhere in the world” at but also to host concerts and plays. In ad- Valley would support three well-supplied Burner’s Spring, later known as Seven Foun- dition to a whirlwind social life, diversions iron furnaces: Mine Run Furnace, Caroline tains, was not to go unnoticed for long. available included horse racing, riding and Furnace (near the OD trail at the southern An 1850s ad for Burner’s White Sulphur carriage drives, gambling, bowling, billiards end of the valley), and Elizabeth Furnace Spa read: “This place lies in Powell’s Fort and shooting galleries. (near the OD trail at Sherman’s Gap in the Valley, Shenandoah County. The Valley is Transportation to the valley was over- northern end of the valley), last two being prettily situated, and in length twenty-five land by horseback or stagecoach. Livery named for the owner’s daughters. miles, affording on the West a fine view of companies provided daily stagecoach runs To smelt iron a vast forest was needed to the Green and Fort Mountains, and to the to the Fort Valley spa, often as many as make charcoal, along with limestone and co- South, the Massanutten Mountain. Eight three stages a day. A band of musicians met pious volumes of water. It took 180 bushels Springs of different waters are located and played for the arrival and departure of of charcoal, 1600 pounds of limestone and within a space of thirty yards, as follows: each stagecoach to the summer guests, who nearly three tons of ore to produce one ton White, Blue, and Black Sulphur; also Chaly numbered from 300 to 600 depending on the of pig iron. With an abundance of forest at beate, Limestone, Freestone, Slatestone and time of the season. their disposal, plus Passage Creek running Alum water; and in the diameter of a half Two stages came over the mountain through the center of the valley, and endless mile are twenty-two Springs. Accommoda- from Woodstock on the western side, while quantities of limestone, each furnace could tions ample for six hundred visitors. Visitors the remaining stage came up from the east, produce three tons of pig iron daily. leaving Baltimore in the morning will dine just above the resort, on a byway now called The smelting of iron in Fort Valley began at the Springs. The Spring s are eight miles Milford Gap. This pretty route, bordered before the American Revolution and lasted from Woodstock. A daily line will run from in mountain laurel in the springtime, and through the Civil War. Much of the iron was Woodstock to the Springs, and return.” shaded by cool trees in the summer, drops a sent north, while some was used in Harper’s A massive influx of visitors converged on blanket of colorful leaves in the fall to offer Ferry where the U.S. Armory turned out a Fort Valley and almost overnight the valley one of the most beautiful views coming into thousand rifles a month. At the northern became one of the most popular resorts spots the valley from the Massanutten Trail. Both end of the valley near the Bear Wallow Trail, in Virginia. Like a reformed sinner, the valley of these routes are part of the 2006 AERC close to the AERC National Championship flung aside its nefarious past to wrap itself in championship trail. 100-mile trail, one can see the old ore pits. the cloak of respectable enterprise. In the vicin- Even though the valley resort eventually By the mid-1800s the disgusted Indians ity of Seven Fountains, a grand hotel with a vast faded away with the turning tide of history, finally packed up their dignity and headed ballroom and many private cottages rose like war and fortunes, it would not be remiss of west. The wolves were less fortunate; the rare jewels in the center of the now fashionable the NC riders, as they enjoy the views along last one was recorded killed in the “Fort” and socially acceptable valley. A huge bath- these roads so well traveled by those long- in 1856 by Abraham Burner and Ephriam house accommodating hundreds of patrons ago vacationers, to perhaps find a moment Golladay near Habron Gap where the 50- was built containing pools for each of the water to hum a few bars of the favorite song of the and 100-mile trail for the 2006 NC rises types, capitalizing on the rare occurrence of day, “Listen to the Mocking Bird,” as their along the east slope of the Massanutten. seven varieties of mineral water bubbling from horses stop for a refreshing drink of the pure the ground in close proximity. mountain streams along the Woodstock and A resort is born The spa also provided a resident physi- Milford Gap trails. And maybe, just maybe, With the disappearance of the wolves cian since many of the patrons came seeking one might pause a moment to listen on the and Indians, the Massanutten suddenly medical cures for various ailments—from gentle Massanutten autumn breeze for the found itself swept up in an entirely new arthritis to dyspepsia and more. Even the faint echo of stagecoach wheels, the jingle invasion of newcomers—the resort and spa most avid pleasure-seekers walked to the of harness, and a soft band playing an wel- seekers. The pre-Revolutionary war pastime elegant spring houses several times a day coming refrain amid the ghostly laughter of frequenting spas and natural mineral to drink the healing waters. of those long ago who came to gentrify and springs to “take the waters” had re-emerged For the most part, the resort patrons were “imbibe the waters” of the valley.
Recommended publications
  • Syntectonic Deposition of Lower to Middle Silurian Sandstones, Central Shenandoah Valley, Virginia W
    Vol. 24 February 1978 No. 1 SYNTECTONIC DEPOSITION OF LOWER TO MIDDLE SILURIAN SANDSTONES, CENTRAL SHENANDOAH VALLEY, VIRGINIA W. P. Roberts1 and J. S. Kite2 The stratigraphy of the Upper Ordovician to It is proposed that the differences in thickness Middle Silurian rocks of the Massanutten between the quartz arenite formations to the west of synclinorium in the Shenandoah Valley of Virginia the Shenandoah Valley and the Massanutten contrasts sharply with the stratigraphy in the Sandstone are, at least partially, a result of defor- folded part of the Valley and Ridge province to the mation penecontemporaneously with deposition west (Figure 1).Five formations between the top of during the Taconic orogeny. Downfolding may have the Martinsburg Formation (Middle and Upper begun in the Massanutten synclinorium area while Ordovician) and the top of the Keefer Sandstone an arch may have been forming to the west (Figure (Middle Silurian) crop out in the Cove Mountain 2) (Rader and Perry, 1976). Assuming such a outcrop belt to the west of the Shenandoah Valley, pattern of deformation, the thickness of the quartz whereas the Massanutten Sandstone represents the sand deposits should be greater in the synclinal same time span in Massanutten Mountain (Figure 2). trough than over the arch. The direction of current Only two of the formations that are exposed west flow should also have been influenced by the of the Shenandoah Valley, the Tuscarora Formation tectonics. Currents would probably flow down the and the Keefer Sandstone, contain quartz arenite in axis of a synclinal trough whereas they would flow the same abundance as that found in the Massa- away from the crest of an arch.
    [Show full text]
  • Signal Knob Northern Massanutten Mountain Catback Mountain Browns Run Southern Massanutten Mountain Five Areas of Around 45,000 Acres on the Lee the West
    Sherman Bamford To: [email protected] <[email protected] cc: Sherman Bamford <[email protected]> > Subject: NiSource Gas Transmission and Storage draft multi-species habitat conservation plan comments - attachments 2 12/13/2011 03:32 PM Sherman Bamford Forests Committee Chair Virginia Chapter – Sierra Club P.O. Box 3102 Roanoke, Va. 24015 [email protected] (540) 343-6359 December 13, 2011 Regional Director, Midwest Region Attn: Lisa Mandell U.S. Fish and Wildlife Service Ecological Services 5600 American Blvd. West, Suite 990 Bloomington, MN 55437-1458 Email: [email protected] Dear Ms. Mandell: On behalf of the Virginia Chapter of Sierra Club, the following are attachments to our previously submitted comments on the the NiSource Gas Transmission and Storage (“NiSource”) draft multi-species habitat conservation plan (“HCP”) and the U.S. Fish & Wildlife Service (“Service”) draft environmental impact statement (“EIS”). Draft of Virginia Mountain Treasures For descriptions and maps only. The final version was published in 2008. Some content may have changed between 2007 and 2008. Sherman Bamford Sherman Bamford PO Box 3102 Roanoke, Va. 24015-1102 (540) 343-6359 [email protected] Virginia’s Mountain Treasures ART WORK DRAWING The Unprotected Wildlands of the George Washington National Forest A report by the Wilderness Society Cover Art: First Printing: Copyright by The Wilderness Society 1615 M Street, NW Washington, DC 20036 (202)-843-9453 Wilderness Support Center 835 East Second Avenue Durango, CO 81302 (970) 247-8788 Founded in 1935, The Wilderness Society works to protect America’s wilderness and to develop a nation- wide network of wild lands through public education, scientific analysis, and advocacy.
    [Show full text]
  • 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.
    [Show full text]
  • 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
    [Show full text]
  • 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.
    [Show full text]
  • Backpacking: Bird Knob
    1 © 1999 Troy R. Hayes. All rights reserved. Preface As a new Scoutmaster, I wanted to take my troop on different kinds of adventure. But each trip took a tremendous amount of preparation to discover what the possibilities were, to investigate them, to pick one, and finally make the detailed arrangements. In some cases I even made a reconnaissance trip in advance in order to make sure the trip worked. The Pathfinder is an attempt to make this process easier. A vigorous outdoor program is a key element in Boy Scouting. The trips described in these pages range from those achievable by eleven year olds to those intended for fourteen and up (high adventure). And remember what the Irish say: The weather determines not whether you go, but what clothing you should wear. My Scouts have camped in ice, snow, rain, and heat. The most memorable trips were the ones with "bad" weather. That's when character building best occurs. Troy Hayes Warrenton, VA [Preface revised 3-10-2011] 2 Contents Backpacking Bird Knob................................................................... 5 Bull Run - Occoquan Trail.......................................... 7 Corbin/Nicholson Hollow............................................ 9 Dolly Sods (2 day trip)............................................... 11 Dolly Sods (3 day trip)............................................... 13 Otter Creek Wilderness............................................. 15 Saint Mary's Trail ................................................ ..... 17 Sherando Lake .......................................................
    [Show full text]
  • Walter Dent<Br>
    Planning.comments.f To: [email protected] [email protected] cc: s Subject: 02/07/2009 09:20 AM Submitted by: Walter Dent<br>At: [email protected]<br>Remark: After attending the last meeting I would like to stress that I believe at this time we have enough wilderness areas in the state of Virginia. Untouched areas of \"wilderness\" may seem like a good idea to some but what it really does is cut the effectiveness of the Forest Service to manage the land. As you are aware of, wilderness areas can be devastated by Gypsy moth infestation, tree diseases, ice storms and fire to name a few and the FS will be helpless to implement any recovery plans. I also believe a lot of the interest for new wilderness is not brought here by local people that actually use the forest but by special interest groups who have never been to the GW/JNF and have their own agendas. I feel that the back country designation achieves everything a wilderness area designation does with out tying the hands of the FS. I would also like to voice my concerns over OHV trails in the national forest. At this time there are a documented 244 miles designated OHV trails in the forest. Unfortunately, I and many others can\'t tell the difference between a \"High vehicle clearance\" roads and a normal fire road. We as the OHV community are all for protecting the environment and treading lightly as witnessed by all the volunteer actions such as trail clean ups, trail repairs and assisting the forest service in various OHV projects, but if a trail is maintained at a level that a non high clearance vehicle can navigate it, then the \"High vehicle clearance\" designation is moot.
    [Show full text]
  • Guide to Camping, Hiking and History at the Elizabeth Furnace Recreation Area
    Guide to Camping, Hiking and History At the Elizabeth Furnace Recreation Area George Washington and Jefferson National Forests Lee Ranger District 95 Railroad Avenue Edinburg, VA 22824 WB-S7-598-11-1 (540) 984-4101 12 Elizabeth Furnace Recreation Area Family Campground: This campground has 33 first-come, first-serve camp sites, picnic tables, and fire rings. During the summer sea- son there are warm water showers and flush toilets. In winter, vault toilets are open and water is available from a hand pump. Fees: In Season - $14/night, Off Season - $10/night. Passage Creek Bridge Picnic Area: The day use area includes picnic tables, vault toi- lets, open fields, access to several well blazed and maintained hiking trails (most notably the Massanutten/Tuscarora Trail), and fishing in Passage Creek. There is No Fee. A Virginia state fishing license and National Forest Stamp are re- quired year round. A Trout Stamp is needed from October 1 through June 15. Group Camping: There are two group sites. Site A accommodates 50 people; Site B can accommodate 25 people. Each site has tent pads, picnic tables, benches and a fire ring. No water is available. Please pack out your trash. Reservations and permit are required. To reserve: www.reserveamerica.com or call 1-888-448-1474. 2 11 Directions: From Strasburg, Virginia, travel 5.1 miles east on State Highway 55 to Waterlick, Virginia. From Waterlick, take State Highway 678 southwest. Travel for 4.8 miles to the recreation area entrance. From the Washington, D.C. Beltway (I-495) take 1-66 West approx.
    [Show full text]
  • A Billion Years of Deformation in the Central Appalachians: Orogenic Processes and Products
    Downloaded from fieldguides.gsapubs.org on October 15, 2015 The Geological Society of America Field Guide 40 2015 A billion years of deformation in the central Appalachians: Orogenic processes and products Steven J. Whitmeyer Department of Geology and Environmental Science, James Madison University, Harrisonburg, Virginia 22807, USA Christopher M. Bailey Department of Geology, College of William & Mary, Williamsburg, Virginia 23187, USA David B. Spears Virginia Department of Mines, Minerals, and Energy, Division of Geology and Mineral Resources, Charlottesville, Virginia 22903, USA ABSTRACT The central Appalachians form a classic orogen whose structural architecture developed during episodes of contractional, extensional, and transpressional defor- mation from the Proterozoic to the Mesozoic. These episodes include components of the Grenville orogenic cycle, the eastern breakup of Rodinia, Appalachian orogenic cycles, the breakup of Pangea, and the opening of the Atlantic Ocean basin. This fi eld trip examines an array of rocks deformed via both ductile and brittle processes from the deep crust to the near-surface environment, and from the Mesoproterozoic to the present day. The trip commences in suspect terranes of the eastern Piedmont in central Vir- ginia, and traverses northwestward across the Appalachian orogen through the thick- skinned Blue Ridge basement terrane, and into the thin-skinned fold-and-thrust belt of the Valley and Ridge geologic province. The traverse covers a range of deformation styles that developed over a vast span of geologic time: from high-grade metamorphic rocks deformed deep within the orogenic hinterland, to sedimentary rocks of the fore- land that were folded, faulted, and cleaved in the late Paleozoic, to brittle extensional structures that overprint many of these rocks.
    [Show full text]
  • Signal Knob Hike in the George Washington National Forest Has Spectacular Views of Strausburg VA
    Signal Knob - Front Royal, Virginia Length Difficulty Streams Views Solitude Camping 9.9 mls Hiking Time: 5.0 hours plus a half hour for lunch Elev. Gain: 2,680 ft with two different ascents Parking: Signal Knob parking area on 678/Fort Valley Rd. 38.93503, -78.31956 The Signal Knob hike in the George Washington National Forest has spectacular views of Strausburg VA. in the Shenandoah Valley, as well as Buzzard Rock in Fort Valley to the east. Signal Knob, at 2,106ft, gets its name as both Confederate and Union troops used it as a lookout during the Civil War. The Confederate Signal Corps controlled the outlook from 1862 until August 14, 1864, when Union troops defeated the 61st Georgia Volunteer Infantry and took control of the peak. Mile 0.0 - Start the hike from the right side of the Signal Knob parking area. The trail is blazed orange which designates it as part of the Massanutten Trail. Start uphill on the orange blazed trail then shortly pass an old stone house on your left, cross a small stream, then follow the trail around the eastern section of the mountain. Mile 1.5 - Arrive at the Buzzard Rock Overlook. The trail will take a hairpin turn back to the south and becomes significantly more rocky. In 0.9 miles from the Buzzard rock overlook the trail turns back to the north passing another nice vista of Fort Valley. Continue to follow the orange blazed trail as it becomes less steep, then passes several nice camp spots just before arriving at the intersection of the Meneka Peak Trail.
    [Show full text]
  • Nomination Form
    NPS Form 10-900 OMB No. 1024-0018 (Rev. 10-90) 4~4 itl~rlo~ ,: United States Department of the Interior 1 /d kcip 317',10~ National Park Service NATIONAL REGISTER OF HISTORIC PLACES REGISTRATION FORM This form is for use in nominating or requesting determinations for individual properties and districts. See instructions in How to Complete the National Register of Historic Places Registration Form (National Register Bulletin 16A). Complete each item by marking nx" in the appropriate box or by entering the information requested. If any it& does not apply to the property being documented, enter "N/A1'for "not applicable." For functions, architectural classification, materials, and areas of significance, enter only categories and subcategories from the instructions. Place additional entries and narrative items on continuation sheets (NPS Form 10-900a). Use a typewriter, word processor, or computer, to complete all items. ===========================================----------=--------================= 1. Name of Property ............................................................................... historic name -Daniel Munch House other names/site number 85-363 2. Location =============================================================================== street & number -2588 Seven Fountains Rd. not for publication city or town -Fort Valley vicinity -X- state -Virginia code -VA- county -Shenandoah code -171 - zip code -22652- ============================================================================== 3. State/Federal Agency Certification
    [Show full text]
  • Start/Finish in Elizabeth Furnace Day Use Lot. Locate White-Blazed Botts
    Start/Finish in Elizabeth Furnace Day Use lot. Locate white-blazed Botts Trail head at southeastern (back left) edge of the big parking lot adjacent to Elizabeth's Furnace. Follow relatively level Botts Trail to junction with pink-blazed Sherman Gap Trail. (1.1 mi) Left on Sherman Gap Trail, and experience a roller coaster until the trail finally turns to ascend to the western ridge of the Massanutten Mountains. (2.6 mi) Right on combined Tuscarora and Massanutten Trails (orange- and blue-blazed) (0.2 mi) Left to descend on purple-blazed Sherman Gap trail to dirt road (Route 613/Panhandle Road). (2.1 mi; Cum = 6.0 mi) Right on the dirt road (Route 613/Panhandle Road) with general inclines to the blue-blazed Tuscarora Trail head at Veach Gap (blazes are alongside the road, but be alert, as the entrance to the trail head looks like a gravel driveway) (1.8 mi) Right off Route 613 onto the blue-blazed Tuscarora Trail, and ascend to junction with orange- blazed Massanutten Trail. (1.7 mi) Right on combined blue- and orange-blazed Tuscarora and Massanutten trails to junction with Veach Gap Trail at the bottom of this descent into Little Crease (two privies and a camping shelter are here; trail junction is immediately after a stream crossing) (1.0 mi) Left on yellow-blazed Veach Gap trail to parking lot at end of Veach Gap Road (Route 774). This gradual descent includes a short, early stretch where the trail is at times all but included in the Mill Run streambed.
    [Show full text]