EXPLANATORY TEXT for GEOLOGIC MAP of NORTH CAROLINA By
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Lexington Quadrangle Virginia
COMMONWEALTH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES GEOLOGY OF THE LEXINGTON QUADRANGLE VIRGINIA KENNETH F. BICK REPORT OF INVESTIGATIONS I VIRGINIA DIVISION OF MINERAL RESOURCES Jomes L. Colver Commissioner of Minerol Resources ond Stote Geologist CHARLOTTESVI LLE, VI RGI N IA 1960 COMMONWEALTH OF VIRGINIA DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT DIVISION OF MINERAL RESOURCES GEOLOGY OF THE LEXINGTON QUADRANGLE VIRGINIA KENNETH F. BICK REPORT OF INVESTIGATIONS I VIRGINIA DIVISION OF MINERAL RESOURCES Jomes L. Colver Commissioner of Minerol Resources ond Stote Geologist CHARLOTTESVI LLE, VI RGI N IA 1960 Couuowwoer,rn op Vtncrwre DopenrupNr op Puncnesrs exo Supptv Rrculroxn 1960 DEPARTMENT OF CONSERVATION AND ECONOMIC DEVELOPMENT Richmond. Virginia MenvrN M. SurHnnr,eNn, Director BOARD Vrcron W. Stnwenr, Petersburg, Chairtnan G. Ar,vrn MessnNnunc, Hampton, Viee'Chairman A. Pr,urvrnr BmnNn, Orange C. S. Cenrnn, Bristol ANpnpw A. Fenr,pv, Danville WonrnrrvcroN FauLKNEn, Glasgow SvoNpv F. Slter,r,, Roanoke EnwrN H. Wrr,r,, Richmond Wrr,r,renr P. Wooor,nv. Norfolk CONTENTS Pece Abstract. '"*i"#:;;;;: . : ::: , : ::.:::::::::..::::::. :.::.::::::: ::,r Z Geography 8 Purpose. 4 Previous Work. Present Work and Acknowledgements. 5 Geologic Formations. 6 Introduction. 6 Precambrian System. 6 Pedlar formation 6 Precambrian and Cambrian Systems. 6 Discussion. 6 Swift Run formation 8 Catoctin greenstone. I Unieoiformation...... ......... I Hampton(Harpers)formation. .......... I Erwin (Antietam) quartzite. Cambrian System . I0 Shady (Tomstown) dolomite 10 Rome (Waynesboro) formation.... ll Elbrook formation. 12 Conococheague limestone. l3 Ordovician System. ......., 14 Chepultepeclimestone. .......... 14 Beekmantown formatron. 14 New Market limestone. 15 Lincolnshire limestone. 16 Edinburg formation. 16 Martinsburg shale... 17 SilurianSystem. ......... 18 Clinchsandstone..... .......... 18 Clinton formation. -
U.S. Geological Survey Bulletin 1839-G, H
Stratigraphic Framework of Cambrian and Ordovician Rocks in the Central Appalachian Basin from Morrow County, Ohio, to Pendleton County, West Virginia Depositional Environment of the Fincastle Conglomerate near Roanoke, Virginia U.S. GEOLOGICAL SURVEY BULLETIN 1839-G, H i i i I ' i ' i ' X- »-v l^,:^ Stratigraphic Framework of Cambrian and Ordovician Rocks in the Central Appalachian Basin from Morrow County, Ohio, to Pendleton County, West Virginia By ROBERT T. RYDER Depositional Environment of the Fincastle Conglomerate near Roanoke, Virginia By CHRYSA M. CULLATHER Chapters G and H are issued as a single volume and are not available separately U.S. GEOLOGICAL SURVEY BULLETIN 1839-G, H EVOLUTION OF SEDIMENTARY BASINS-APPALACHIAN BASIN U.S. DEPARTMENT OF THE INTERIOR MANUEL LUJAN, Jr., Secretary U.S. GEOLOGICAL SURVEY DALLAS L. PECK, Director Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government UNITED STATES GOVERNMENT PRINTING OFFICE: 1992 For sale by Book and Open-File Report Sales U.S. Geological Survey Federal Center, Box 25425 Denver, CO 80225 Library of Congress Cataloging in Publication Data (revised for vol. G-H) Evoluation of sedimentary basins Appalachian basin. (U.S. Geological Survey bulletin ; 1839 A-D, G-H) Includes bibliographies. Supt. of Docs. no.:19.3:1839-G Contents: Horses in fensters of the Pulaski thrust sheet, southwestern Virginia / by Arthur P. Schultz [etc.] Stratigraphic framework of Cam brian and Ordovician rocks in central Appalachian basin from Morrow County, Ohio, to Pendleton County, West Virginia / by Robert T. -
Breeding Season Habitat and Distribution of the Red-Breasted Nuthatch in the Southern Blue Ridge Mountain Province
BREEDING SEASON HABITAT AND DISTRIBUTION OF THE RED-BREASTED NUTHATCH IN THE SOUTHERN BLUE RIDGE MOUNTAIN PROVINCE MARCUS B. SIMPSON JR. According to the A.O.U. Check-list (1957) the Red-breasted Nuthatch (Sitta canadensis) nests widely through Canada, the northern United States, and down the Appalachian highlands to its southern breeding limit in eastern Tennessee and western North Carolina. Pearson et al. (1959) state that the species breeds on "some of the higher mountains" but give no details of habitat selection. Despite evidence to the contrary, it is commonly believed that the bird is strictly confined during the breeding season to forests of red spruce (Picea rubens) and Fraser fir (Abies fraseri) in the mountain re- gion. This paper reviews data indicating that the Red-breasted Nuthatch utilizes at least three distinct forest types in the southern Blue Ridge Province during the spring and summer months. HABITAT TYPES 1. Spruce-fir Forests. The so-called Canadian zone or boreal forests of red spruce and Fraser fir are the major habitat used by the Red-breasted Nuthatch in the southern Appalachians, and the bird has been reported during the breeding season from every known stand of this community-type in the region. Briefly, the nuthatch has been thoroughly documented as a common summer resident in spruce-fir forests of the Great Smoky Mountains (Stupka 1963); northern Great Balsam Mountains, Plott Balsam Mountains, southern Great Balsam Mountains, Pisgah Ridge, Shining Rock Ledge, Blue Ridge Mountains, Nantahala Mountains, and Long Hope Creek in Watauga County (Simpson, present study); Black Mountains (Brewster 1886, Cairns 1889, Simpson 1972); Grandfather Mountain (Alexander 1973; Simpson, present study); Roan Mountain (Ganier 1936; Fred Behrend, pers. -
Annual Meeting 2002
Newsletter 51 74 Newsletter 51 75 The Palaeontological Association 46th Annual Meeting 15th–18th December 2002 University of Cambridge ABSTRACTS Newsletter 51 76 ANNUAL MEETING ANNUAL MEETING Newsletter 51 77 Holocene reef structure and growth at Mavra Litharia, southern coast of Gulf of Corinth, Oral presentations Greece: a simple reef with a complex message Steve Kershaw and Li Guo Oral presentations will take place in the Physiology Lecture Theatre and, for the parallel sessions at 11:00–1:00, in the Tilley Lecture Theatre. Each presentation will run for a New perspectives in palaeoscolecidans maximum of 15 minutes, including questions. Those presentations marked with an asterisk Oliver Lehnert and Petr Kraft (*) are being considered for the President’s Award (best oral presentation by a member of the MONDAY 11:00—Non-marine Palaeontology A (parallel) Palaeontological Association under the age of thirty). Guts and Gizzard Stones, Unusual Preservation in Scottish Middle Devonian Fishes Timetable for oral presentations R.G. Davidson and N.H. Trewin *The use of ichnofossils as a tool for high-resolution palaeoenvironmental analysis in a MONDAY 9:00 lower Old Red Sandstone sequence (late Silurian Ringerike Group, Oslo Region, Norway) Neil Davies Affinity of the earliest bilaterian embryos The harvestman fossil record Xiping Dong and Philip Donoghue Jason A. Dunlop Calamari catastrophe A New Trigonotarbid Arachnid from the Early Devonian Windyfield Chert, Rhynie, Philip Wilby, John Hudson, Roy Clements and Neville Hollingworth Aberdeenshire, Scotland Tantalizing fragments of the earliest land plants Steve R. Fayers and Nigel H. Trewin Charles H. Wellman *Molecular preservation of upper Miocene fossil leaves from the Ardeche, France: Use of Morphometrics to Identify Character States implications for kerogen formation Norman MacLeod S. -
Geological Notes on the Northern Natural Gas Company Well Near Oakland, Iowa
Proceedings of the Iowa Academy of Science Volume 53 Annual Issue Article 28 1946 Geological Notes on the Northern Natural Gas Company Well Near Oakland, Iowa Stanley E. Harris Jr. Iowa Geological Survey Let us know how access to this document benefits ouy Copyright ©1946 Iowa Academy of Science, Inc. Follow this and additional works at: https://scholarworks.uni.edu/pias Recommended Citation Harris, Stanley E. Jr. (1946) "Geological Notes on the Northern Natural Gas Company Well Near Oakland, Iowa," Proceedings of the Iowa Academy of Science, 53(1), 233-246. Available at: https://scholarworks.uni.edu/pias/vol53/iss1/28 This Research is brought to you for free and open access by the Iowa Academy of Science at UNI ScholarWorks. It has been accepted for inclusion in Proceedings of the Iowa Academy of Science by an authorized editor of UNI ScholarWorks. For more information, please contact [email protected]. Harris: Geological Notes on the Northern Natural Gas Company Well Near Oa GEOLOGICAL NOTES ON THE NORTHERN NATURAL GAS COMPANY WELL NEAR OAKLAND, IOWA1 STANLEY E. HARRIS, JR. PREVIOUS WORK AND ACKNOWLEDGEMENTS The study for this paper is based on the work of the many geolo gists who have studied and correlated the stratigraphy of Iowa. The writer is particularly indebted to the subsurface geologists who have traced the geological formations from the surface outcrop areas into the subsurface by means of examination of well cuttings. The foun <1ation for this work was laid by W. H. Norton who continued to be the principal contributer for many years. In 1934, under the direction of A. -
Craggy Pinnacle Hike
Craggy Pinnacle - Craggy Gardens, Blue Ridge Parkway, NC Length Difficulty Streams Views Solitude Camping 1.1 mls N/A N/A Hiking Time: 45 minutes Elev. Gain: 230 ft Parking: Park at the Craggy Dome Overlook. 35.70419, -82.37355 By Trail Contributor: Zach Robbins Craggy Pinnacle is considered one of the most scenic, short hikes along the entire length of the Blue Ridge Parkway. Located 40 minutes northeast of Asheville, this crown jewel of the Great Craggy Mountains features spectacular 360° views from the stone observation deck on its summit. From the airy heights of this dramatic heath bald you’ll be able to pick out all of the highest ranges in North Carolina and Tennessee, including the Black Mountains and Great Smoky Mountains. Because of its proximity to Asheville, views, and lack of difficulty, this hike is popular and will likely be overrun on the weekends. Try to arrive early or hike on a weekday to avoid crowds. This section of the Blue Ridge Parkway is closed normally during winter due to ice and inclement weather. Check the road closure website for alerts and the real-time closure map. Nearby hike options: Big Butt Trail | Douglas Falls and Craggy Gardens | Snowball Trail Mile 0.0 – Park at the Craggy Dome Overlook and follow the Craggy Pinnacle Trail towards the summit. The trail passes by dense stands of gnarled northern hardwoods and Catawba rhododendrons, which bloom spectacularly in June and draw huge crowds. Mile 0.3 – Three-way trail junction below the summit. The trail on the left leads to the summit and the trail behind you leads to the north overlook. -
Characteristics of Thin-Skinned Style of Deformation in the Southern Appalachians, and Potential Hydrocarbon Traps
Characteristics of Thin-Skinned Style of Deformation in the Southern Appalachians, and Potential Hydrocarbon Traps GEOLOGICAL SURVEY PROFESSIONAL PAPER 1O18 Characteristics of Thin-Skinned Style of Deformation in the Southern Appalachians, and Potential Hydrocarbon Traps By LEONARD D. HARRIS and ROBERT C. MILICI GEOLOGICAL SURVEY PROFESSIONAL PAPER 1018 Description of and field guide to large- and small-scale features of thin-skinned tectonics in the southern Appalachians, and a discussion of hydrocarbon production and potential UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1977 UNITED STATES DEPARTMENT OF THE INTERIOR JAMES G. WATT, Secretary GEOLOGICAL SURVEY Doyle G. Frederick, Acting Director First printing 1977 Second printing 1981 Library of Congress Cataloging in Publication Data Harris, Leonard D. Characteristics of thin-skinned style of deformation in the southern Appalachians, and potential hydrocarbon traps. (Geological Survey professional paper ; 1018) Bibliography: p. Supt. of Docs, no.: I 19.16:1018 1. Rock deformation. 2. Geology Appalachian Mountains. 3. Petroleum -Geology Appalachian Mountains. I. Milici, Robert C., 1931- joint author. II. Title: Characteristics of thin-skinned style of deformation in the southern Appalachians . III. Series: United States. Geological Survey. Professional paper ; 1018. QE604.H37 551.8'7'09768 76-608283 For sale by the Distribution Branch, U.S. Geological Survey, 604 South Pickett Street, Alexandria, VA 22304 CONTENTS Page Abstract ———_—___________________________——_——————————— -
Breeding Season Habitats of the Golden-Crowned Kinglet in the Southern Blue Ridge Mountains
BREEDING SEASON HABITATS OF THE GOLDEN-CROWNED KINGLET IN THE SOUTHERN BLUE RIDGE MOUNTAINS MARCUS B. SIMPSON JR. The Golden-crowned Kinglet (Regulus satrapa) occurs through much of Canada, the northern United States, and down the Appalachian highlands to the southern limit of its breeding range in the mountains of western North Carolina (A.O.U. 1957). Pear son et al. (1959) state that the bird breeds on "some of the higher mountains" but they give no details of habitat selection. In the southern Blue Ridge Mountains, the species occurs during the summer months in three distinct types of coniferous forests. 1. Spruce-fir forests. The majority of kinglets inhabit the forests of red spruce (Picea rubens) and Fraser fir (Abies fraseri) at elevations above 1372 m (4500 feet). The species is well documented as a common summer resident in the Great Smoky Mountains (Stupka 1963); northern Great Balsam Mountains, Plott Balsam Mountains, southern Great Balsam Mountains, Shining Rock Ledge, Blue Ridge Mountains, and Nantahala Mountains (Simpson, present study); Black Mountains (Simpson 1972a); Grandfather Mountain (Pearson et al. 1959, Alexander 1973); Roan Mountain (Fred Behrend, pers. com .; Simpson, present study); the Mt. Rogers-Whitetop area of Vir- ginia (Murray 1952; Simpson, present study); and apparently at Cone Lake, Watauga County, N.C. (Murray 1946). Breeding reports have been obtained in the Smokies (Stupka 1963), Black Mountains (Burleigh 1941), and Grandfather Mountain (Pearson et al. 1959); while breeding season densities have been reported by Adams (1959) and Alsop (1970). 2. Hemlock forests. The eastern hemlock (Tsuga canadensis) is a common forest tree throughout the southern Blue Ridge, where it often occurs as a major dominant in sheltered ravines and moist slopes. -
Nesting of the Yellow-Bellied Sapsucker in Great Craggy and Southern Great Balsam Mountains of North Carolina MARCUS B
Nesting of the Yellow-bellied Sapsucker in Great Craggy and Southern Great Balsam Mountains of North Carolina MARCUS B. SIMPSON JR. P.O. Box 167, Statesville, N.C. 24 January 1972 Pearson, Brimley, and Brimley (1942) regarded the Yellow-bellied Sapsucker (Sphyrapicus varius) as a breeding summer resident in the higher mountains of North Carolina, but they mentioned only four specific localities where the bird had been observed: Roan Mountain, Highlands, Joannana Bald Mountain, and Greybeard Moun- tain. Elsewhere, the bird has been reported during summer in the Unicoi Mountains by Ganier and Clebsch (1944), the Great Smoky Mountains by Stupka (1963), and Mt. Mitchell by Burleigh (1941). To date, however, there appear to be no specific records from the Great Craggy or southern Great Balsam Mountains; and the following observations are therefore of interest. SOUTHERN GREAT BALSAM MOUNTAINS: Based on my field work in this range from 1963 to 1971, the Yellow-bellied Sapsucker is an uncommon summer resident above 3,500 feet in deciduous forests that have been disturbed by logging or fires. During the months of May through August, I have a total of 16 records of individual birds at elevations from 3,600 feet to 5,800 feet. In addition to these individual sightings, groups of two or more birds have been noted at three localities in the range. At Wet Camp Gap (5,360 feet), Jackson County, a pair has been noted repeatedly in June 1963, 1965, and 1969, while on 15 June 1968 two adults were carrying food into a nesting hole some 25 feet up in a large white oak (Quercus alba). -
Mineral Resources of the Craggy Mountain Wilderness Study Area and Extension, Buncombe County, North Carolina
STUDIES RELATED TO WILDERNESS Mineral Resources of the Craggy Mountain Wilderness Study Area and Extension, Buncombe County, North Carolina By F. G. LESURE and A. E. GROSZ, U.S. GEOLOGICAL SURVEY, and by· B. B. WILLIAMS and G. C. GAZDIK, U.S. BUREAU OF MINES STUDIES RELATED TO WILDERNESS-WILDERNESS AREAS GEOLOGICAL SURVEY BULLETIN 1515 An evaluation of the mineral potential of the area UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1982 UNITED STATES DEPARTMENT OF THE INTERIOR JAMES G. WATT, Secretary GEOLOGICAL SURVEY Dallas L. Peck, Director Library of Congress Cataloging in Publication Data Lesure, Frank Gardner, 1927- Mineral resources of the Craggy Mountain Wilderness Study Area and Extension, Bunc1m County, North Carolina. (Geological Survey bulletin ; 1515) Bibliography: p. Supt. of Docs. no.: I 19.3:1515 1. Mines and mineral resources-North Carolina-Buncombe Co. I. Grosz, Andrew E., jof author. II. Title. III. Series: United States. Geological Survey. Bulletin ; 1515. QE75.B9 no. 1515 [TN24.N8] 557.3s [553'.09756'88] 80-607863 For sale by the Distribution Branch, U.S. Geological Survey, 604 South Pickett Street, Alexandria, VA 22304 STUDIES RELATED TO WILDERNESS WILDERNESS AREAS In accordance with the provisions of the Wilderness Act (Public Law 88-577, September 3, 1964) and the Joint Con ference Report on Senate Bill 4, 88th Congress, and as specifically designated by PL 93-622, January 3, 1975, the U.S. Geological Survey and U.S. Bureau of Mines have been conduct ing mineral surveys of wilderness and primitive areas. Studies and reports of all primitive areas have been completed. Areas officially designated as "wilderness," "wild," or "canoe" when the act was passed were incorporated into the National Wilderness Preservation System, and some of them are presently being studied. -
Systematics, Phylogenetics, and Biogeography of Early Mississippian Camerate Crinoids of the Nunn Member, Lake Valley Formation, in South-Central New Mexico
Graduate Theses, Dissertations, and Problem Reports 2011 Systematics, Phylogenetics, and Biogeography of Early Mississippian Camerate Crinoids of the Nunn Member, Lake Valley Formation, in south-central New Mexico Elizabeth C. Rhenberg West Virginia University Follow this and additional works at: https://researchrepository.wvu.edu/etd Recommended Citation Rhenberg, Elizabeth C., "Systematics, Phylogenetics, and Biogeography of Early Mississippian Camerate Crinoids of the Nunn Member, Lake Valley Formation, in south-central New Mexico" (2011). Graduate Theses, Dissertations, and Problem Reports. 3414. https://researchrepository.wvu.edu/etd/3414 This Dissertation is protected by copyright and/or related rights. It has been brought to you by the The Research Repository @ WVU with permission from the rights-holder(s). You are free to use this Dissertation in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you must 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 Dissertation has been accepted for inclusion in WVU Graduate Theses, Dissertations, and Problem Reports collection by an authorized administrator of The Research Repository @ WVU. For more information, please contact [email protected]. Systematics, Phylogenetics, and Biogeography of Early Mississippian Camerate Crinoids of the Nunn Member, Lake Valley Formation, in south-central New Mexico Elizabeth C. Rhenberg Dissertation submitted to the Eberly College of Arts and Sciences at West Virginia University in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Geology Thomas Kammer, Ph.D., Chair William Ausich, Ph.D. -
The High Peaks and Asheville—MST Segment 3
1 | Mountains-to-Sea Trail Last Updated 1/1/2017 Approaching Blackstock Knob Photo by Jeff Clark www.internetbrothers.org The High Peaks and Asheville—MST Segment 3 PISGAH INN TO BLACK MOUNTAIN CAMPGROUND By Jim Grode Segment 3 is where Asheville comes to play. It is the most heavily used part of the MST within the mountains, and you are likely to encounter hikers, dog walkers, and trail runners at any time throughout the year. Virtually all of it is easily accessible from the Blue Ridge Parkway (BRP), and there are road crossings every few miles for most of the length. Don’t let its accessibility and popularity fool you, however: With eleva- tions ranging from 2,000 feet at the French Broad River to over 6,600 feet at the summit of Mount Mitchell, this segment is quite rugged. Indeed, the Segment 3 | 2 section just west of Asheville hosts the infamous Shut-In Ridge Trail Run, an 18-mile trail run that annually humbles racers from around the country. Complementing the natural beauty of the Blue Ridge Mountains in this area is the vibrancy of Asheville, a city of 80,000 nestled in the French Broad River valley, which regularly makes lists of the top 10 cities in the United States. Crammed with restaurants, shops, art galleries, and brew- eries, Asheville offers something for nearly everyone and is well worth a layover in your hiking schedule. HIGHLIGHTS INCLUDE • The views atop 6,684-foot Mount Mitchell, the highest point east of the Mississippi River • The Shut-In Trail, which follows the old carriage road from the Biltmore House to George Vanderbilt’s hunting lodge on Mount Pisgah (which no longer stands, but a few remnants of which are still visible) • The cultural and scientific displays at the Blue Ridge Parkway Visitor Center & Headquarters near Asheville • The fine collection of southern art and crafts at the Folk Art Center also near Asheville.