Physiographic Map of Maryland 422308 !

Total Page:16

File Type:pdf, Size:1020Kb

Physiographic Map of Maryland 422308 ! 79°00'W ! ! 78°30'W ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! 78°00'W ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! 76°00'W ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! 76°30'W ! ! ! ! 77°30'W 77°00'W ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! 112700 ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! 218000 ! 422303 ! ! ! 216000 ! ! ! 112100 ! 217000 ! ! ! ! ! ! 218001 ! ! ! 215000 ! 312002 ! ! ! ! 422100 ! ! ! ! ! 222100 ! 424001 ! 112500 ! ! ! ! ! ! 424000 ! 422301 212000 ! ! ! 223100 ! ! ! ! 222200 ! ! ! ! ! 112701 A l l e g a n y ! 422300 ! ! ! ! ! ! ! ! ! 112600 422302 ! ! ! ! ! ! 112301 ! ! ! ! ! 214000 ! 211100 ! 312000 ! 412100 ! ! ! ! ! 423100 ! ! ! ! C e c i l ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! W a s h i n g t o n ! G a r r e t t ! ! ! ! ! ! ! ! 421200 213000 ! 112200 ! ! ! 426100 Appalachian Plateaus 511101 ! Blue Ridge ! ! ! ! ! Ridge and Valley Piedmont Plateau ! ! ! ! ! ! ! 422101 ! ! ! 422305 ! ! ! ! ! ! ! ! ! Province ! ! C a r r o l l ! Province ! Province Province ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! 224100 211100 ! ! ! 422300 ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! 221100 ! ! ! ! ! ! ! ! H a r f o r d ! ! ! ! ! ! Allegheny Mountain ! ! ! ! ! ! ! ! ! ! ! ! Section ! ! ! 511100 ! ! ! ! ! 112501 ! 112300 ! 313100 ! B a l t i m o r e ! ! Great Valley ! ! ! ! ! 224200 F r e d e r i c k ! ! ! ! ! Folded Appalachian ! 422100 Section 78°00'W ! Upland Section ! ! ! ! ! ! 512100 ! ! ! 425102 ! ! ! Mountain Section Western Shore ! 423200 ! ! ! ! ! ! ! ! ! ! ! ! Lowlands Region ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! Northern Blue ! ! ! ! ! ! ! 112702 ! ! ! ! 422403 ! ! ! ! Ridge Section ! 425100 ! ! ! ! ! 223100 ! ! ! ! ! ! ! ! ! ! N ! ! ! ! 425101 ' ! ! ! ! ! ! ! ! ! ! ! ! 0 ! ! ! ! ! ! ! Lowland 3 ! ! 3 ! ° ! ! ! n ! 112201 ! ! Section 9 o 9 i ! ! ° Major Physiographic ! g 3 ! ! ! 3 e ! ! ! 426100 ! ! ! 0 ! R ! ! 422304 ! ! 514100 ! ! ! ! ! ! ! y ' ! 224201 Subdivisions ! 78°30'W 422305 ! ! N ! r ! ! ! ! ! Western Shore ! ! ! a ! ! ! ! ! ! ! ! u ! ! t Delmarva Peninsula ! ! ! Uplands Region ! ! ! in Maryland s ! ! ! ! 4 112700 ! ! E Region ! ! ! ! ! ! ! e ! ! 112401 ! ! k ! ! 313200 ! ! ! a ! 111100 ! ! ! ! ! ! e ! ! ! 312001 p ! ¯ ! ! a ! ! 112400 ! ! 422305 s ! ! ! ! e ! ! ! 422306 512100 h ! ! ! C ! ! ! 79°00'W 0 10 20 40 Miles ! ! ! ! ! ! ! ! ! ! ! 423300 ! ! ! 426101 ! ! ! ! ! 511200 ! ! ! ! 0 12.5 25 50 Kilometers ! 425200 ! ! ! ! ! 413100 ! DRAFT ! ! 425102 ! ! 112400 ! ! ! ! ! 422307 ! ! 314100 Coastal Plain ! ! ! ! ! ! ! 511201 Province ! ! 221100 425100 Legend ! ! ! ! ! Embayed Section ! ! 313201 ! ! ! 112200 ! ! ! ! Province Boundary ! ! ! 314000 ! ! ! ! 422501 ! ! ! ! ! ! ! ! 412200 ! 112402 ! ! ! 426100 ! ! ! ! ! ! Physiographic Map of Maryland 422308 ! ! 422200 ! ! ! ! ! ! ! ! 511200 ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! 422500 ! ! ! ! ! ! B a l t i m o r e K e n t ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! C i t y ! ! ! By James P. Reger and Emery T. Cleaves ! 311100 ! ! ! ! ! H o w a r d ! ! ! ! 514100 ! ! ! ! 422400 ! ! STATE OF MARYLAND ! ! ! 422401 422309 ! ! ! Martin O’ Malley 512100 ! ! ! ! ! ! ! ! ! ! Governor ! ! 2008 ! ! ! ! ! 422402 ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! ! 0 2 4 8 12 16 ! ! ! 511301 ! ! ! Miles 426102 ! ! 77°30'W ! ! ! ! ! ! 422300 ! 0 3.5 7 14 21 28 ! ! ! ! ! Kilometers ! ! 514400 ! 422500 ! ! ! ! ! ! ! 511300 ! ! ! ! ! ! ! ! 412200 M o n t g o m e r y ! ! ! ! 100000. 200000. 300000. 400000. 500000. A n n e A r u n d e l ! ! ! 426100 ! ! 513000 ! ! A PP A LA C HI AN P L AT E AU S P RO V IN C E R I D G E A N D V A L L E Y P R O V I N C E B L U E R I D G E P R O V I N C E PIEDMONT PLATEAU PROVINCE A T L A N T I C C O A S T A L P L A I N P R O V IN C E ! ! Plateau of moderately to thoroughly dissected roughly horizontal sedimentary An "accordion-like" topography composed of alternating, subparallel ridges and In Maryland, the Province consists of two prominent ridges separated in the Mostly a broadly undulating to rolling topography underlain by metamorphic A seaward sloping plain extending from Cape Cod to the southern tip of Florida. 422310 ! ! ! rock; elevations rise from west to east; landscape varies with Section. valleys resulting from differential erosion of various folded and faulted southern half by the rolling to hilly Middletown Valley. rocks and whose relief is increased locally by low knobs or ridges and valleys. In Maryland, consists of a fairly flat to moderately rolling upland and an even ! ! DEPARTMENT OF NATURAL RESOURCES ! ! 110000. Allegheny Mountain Section. Wide ridges separated by lithologies. On the west are lowlands developed either on Mesozoic clastics or early flatter lowland. ! ! John R. Griffin 310000. Northern Blue Ridge Section. Consists of two prominent ridges ! 411100 Q u e e n A n n e ' s ! ! Paleozoic carbonates. ! ! broad valleys; plunge direction on broad folds produces topographic ! ! ! 210000. Folded Appalachian Mountains Section. Alternating, 510000. Embayed Section. Characterized by estuaries and embayments ! (South and Catoctin Mountains) that merge northeastward into a single ! ! ! ! ! ! ! Secretary ! basins (“canoe” -shaped valleys). 410000. Piedmont Lowland Section. A valley consisting of both a ! subparallel ridges and valleys; generally increase in elevation east to west; attributed to the drowning of river mouths and formation of barrier ! hilly to mountainous area. In the southern part of the Section in ! 511302 ! ! relative spacing and width of ridges and valleys relate to fold limestone valley and parts of two Mesozoic rift basins. 422 310. Hunting Hill Area. T he largest of islands associated with post-glacial sea-level rise. Terrain is fairly 512 100. Aberdee n Estuaries a nd Lowlands ! 511400 514100 Maryland, a central valley (Middletown Valley) occurs along the fold ! ! 111000. Chesapeake Gorges Region. Generally steep-sided ! wavelength and amplitude and to attitude, thickness and erosional several mafic and ultramafic bodies in the southern flat to moderately rolling; upland bounded by flat lowlands. D i s t r i c t . A relatively featureless lowland (mostly <50 ft ! axis. 411000. Chesapeake Gorges Region. Two major gorges ! gorge coinciding with the Potomac River valley; in some places ! ! ! resistance of the rocks. part of the Hampstead Upland; the Area stands out elevation) along the NW shore of Chesapeake Bay. The ! parallel to regional geologic structure, in other places transverse to comprise the Region, those of the Potomac and Susquehanna Rivers, 511000. Western Shore Uplands Region. A flat to rolling upland ! ! 311000. Chesapeake Gorges Region. Generally a steep-sided ! 512200 because it is less dissected and has broader, gentler District has a very irregular coastline indented by the 3 structure. both originating in the Appalachian Plateaus Province. In the surface underlain by Cretaceous to Pliocene sediments. Markedly ! 211000. Chesapeake Gorges Region. Varies between a steep- 9 ! gorge with very limited flood plain development. ! ! Piedmont Lowland the Potomac occupies a well-defined flood plain. slopes than the surrounding upland. higher elevations and greater relief than the Eastern Shore. flooded mouths of the Bush, Bird, Middle, Back and ° 0 sided gorge and broader, shallower, but still steep-sided, valley N ' 111100. Upper Potomac Gorge District. ! ! Patapsco Rivers. 0 311100. Middle Potomac Gorge District. Steep- 0 Fluvial and estuarine terraces flank the major drainages, most ! ! with some flood plain development. 422400. Mt. Airy Upland District. Rolling 511401 ' 411100. Middle Potomac Floodplain District. N 0 Generally steep-sided gorge of the Potomac River; tends to ! ! sided gorge in quartzite at Elk Ridge and South Mtn; riffles ! ° ! notably the Patuxent River. ! upland; herringbone texture due to interaction of thin ! 511300 512200. Annapolis Estuaries and Lowlands The Potomac River occupies a narrow flood plain, but has 9 ! ! parallel the regional strike of bedrock geologic structure; in 211100. Upper Potomac Gorge District. Steep- where Potomac flows over steeply dipping resistant beds; ! 3 ! ! ! siltstones and quartzites with stream reaches controlled by District. ! ! A relatively featureless lowland (mostly <50 ft not developed a meandering stream habit. Several cobble- ! ! its lower reach, transverse to strike. ! 511100. Elk Neck Peninsula District. With sided gorge, most slopes >15 degrees, some >20 degrees; river incised >100 ft with narrow, discontinuous flood plain ! ! ! ! ! joints oblique to bedrock strike; streams often incised (e.g., elevation) along the west-central shore of Chesapeake Bay; ! ! veneered bedrock islands occupy much of the channel. ! ! ! ! ! elevations exceeding 200 feet, the peninsula is a prominent ! ! ! 112000. Allegheny High Plateau Region. Erosion of the folds cliffs common; limited flood plain; incised meanders; across granitic Middletown and Pleasant (Rohrersville) ! ! ! Bennett, Little Bennett, Bush, Linganore, and Israel it has a less irregular coastline than
Recommended publications
  • Upper Cenozoic Deposits of the Central Delmarva Peninsula, Maryland and Delaware
    Upper Ceoozoic Deposits GEOLOGICAL SXJEVilY FRQfEBSIONAL lAPEE Upper Cenozoic Deposits of the Central Delmarva Peninsula, Maryland and Delaware By JAMES P. OWENS and CHARLES S. DENNY SURFACE AND SHALLOW SUBSURFACE GEOLOGIC STUDIES IN THE EMERGED COASTAL PLAIN OF THE MIDDLE ATLANTIC STATES GEOLOGICAL SURVEY PROFESSIONAL PAPER 1067-A Upper Tertiary deltaic and shallow-water marine deposits form the backbone of the peninsula. The oldest marine deposits of Pleistocene age reach a maximum altitude of 15 meters (50 feet) and have been dated radiometrically at about 100,000 years UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1979 UNITED STATES DEPARTMENT OF THE INTERIOR CECIL D. ANDRUS, Secretary GEOLOGICAL SURVEY H. William Menard, Director Library of Congress Cataloging in Publication Data Owens, James Patrick, 1924- Upper Cenozoic deposits of the central Delmarva Peninsula, Maryland and Delaware. (Surface and shallow subsurface geologic studies in the emerged coastal plain of the Middle Atlantic States) (Geological Survey professional paper ; 1067-A) Bibliography: p. Includes index. Supt. of Docs, no.: I 19.16:1067-A 1. Geology, Stratigraphic Cenozoic. 2. Geology Delmarva Peninsula. I. Denny, Charles Storrow, 1911- joint author. II. Title. III. Series. IV. Series: United States. Geological Survey. Professional paper ; 1067-A. QE690.093 551.7'8 77-608325 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 024-001-03191-4 CONTENTS Abstract._____________________________________________________________
    [Show full text]
  • A Taxonomic Revision of Rhododendron L. Section Pentanthera G
    A TAXONOMIC REVISION OF RHODODENDRON L. SECTION PENTANTHERA G. DON (ERICACEAE) BY KATHLEEN ANNE KRON A DISSERTATION PRESENTED TO THE GRADUATE SCHOOL OF THE UNIVERSITY OF FLORIDA IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY UNIVERSITY OF FLORIDA 1987 , ACKNOWLEDGMENTS I gratefully acknowledge the supervision and encouragement given to me by Dr. Walter S. Judd. I thoroughly enjoyed my work under his direction. I would also like to thank the members of my advisory committee, Dr. Bijan Dehgan, Dr. Dana G. Griffin, III, Dr. James W. Kimbrough, Dr. Jonathon Reiskind, Dr. William Louis Stern, and Dr. Norris H. Williams for their critical comments and suggestions. The National Science Foundation generously supported this project in the form of a Doctoral Dissertation Improvement Grant;* field work in 1985 was supported by a grant from the Highlands Biological Station, Highlands, North Carolina. I thank the curators of the following herbaria for the loan of their material: A, AUA, BHA, DUKE, E, FSU, GA, GH, ISTE, JEPS , KW, KY, LAF, LE NCSC, NCU, NLU NO, OSC, PE, PH, LSU , M, MAK, MOAR, NA, , RSA/POM, SMU, SZ, TENN, TEX, TI, UARK, UC, UNA, USF, VDB, VPI, W, WA, WVA. My appreciation also is offered to the illustrators, Gerald Masters, Elizabeth Hall, Rosa Lee, Lisa Modola, and Virginia Tomat. I thank Dr. R. Howard * BSR-8601236 ii Berg for the scanning electron micrographs. Mr. Bart Schutzman graciously made available his computer program to plot the results of the principal components analyses. The herbarium staff, especially Mr. Kent D. Perkins, was always helpful and their service is greatly appreciated.
    [Show full text]
  • News Release Address: Email and Homepage: U.S
    News Release Address: Email and Homepage: U.S. Department of the Interior Maryland-Delaware-D.C. District [email protected] U.S. Geological Survey 8987 Yellow Brick Road http://md.water.usgs.gov/ Baltimore, MD 21237 Release: Contact: Phone: Fax: January 4, 2002 Wendy S. McPherson (410) 238-4255 (410) 238-4210 Below Normal Rainfall and Warm Temperatures Lead to Record Low Water Levels in December Three months of above normal temperatures and four months of below normal rainfall have led to record low monthly streamflow and ground-water levels, according to hydrologists at the U.S. Geological Survey (USGS) in Baltimore, Maryland. Streamflow was below normal at 94 percent of the real-time USGS gaging stations and 83 percent of the USGS observation wells across Maryland and Delaware in December. Record low streamflow levels for December were set at Winters Run and Pocomoke River. Streamflow levels at Deer Creek and Winters Run in Harford County have frequently set new record daily lows for the last four months (see real-time graphs at http://md.water.usgs.gov/realtime/). Streamflow was also significantly below normal at Antietam Creek, Choptank River, Conococheague Creek, Nassawango Creek, Patapsco River, Gunpowder River, Patuxent River, Piscataway Creek, Monocacy River, and Potomac River in Maryland, and Christina River, St. Jones River, and White Clay Creek in Delaware. The monthly streamflow in the Potomac River near Washington, D.C. was 82 percent below normal in December and 54 percent below normal for 2001. Streamflow entering the Chesapeake Bay averaged 23.7 bgd (billion gallons per day), which is 54 percent below the long-term average for December.
    [Show full text]
  • Eastern Shore, VA
    Community Info Sheet Eastern Shore, VA Total Population (2010): 45,553 Accomack County: 33,164 North Hampton County: 12,389 Parksley, VA: 842 (Northampton and Accomack Counties comprise the Eastern Shore of Virginia.) Things Eastern Shore is known for: Chincoteague Island & Chincoteague National Wildlife Refuge, The Chesapeake Bay, The Annual Wild Pony Round Up, NASA Wallops Flight Facility of the Eastern Shore, Tyson & Purdue Chicken Processing Plants, The Crabbing and Fishing Industry Eastern Shore Overview: The Eastern Shore of Virginia offers a historic setting, serene lifestyle, and abundant outdoor recreation. It is a 70-mile-long stretch of shoreline at the southern end of the Delmarva Peninsula. It is comprised of two counties – Accomack and North Hampton – and is bordered by the Chesapeake Bay to the West, the Atlantic Ocean to the East, and Maryland to the North. It is accessible to mainland Virginia by the 23-mile-long Chesapeake Bay Bridge-Tunnel. Prior to its completion in 1964, mainland Virginia was only accessible by ferry, or by lengthy commute through Maryland and Washington D.C. Despite being largely isolated from mainland Virginia, the Eastern Shore has a robust agricultural The Delmarva Peninsula The Eastern Shore of Virginia economy. Crabbing and fishing industries share the coastline, while large-scale produce and chicken farms utilize much of the peninsula itself. Tyson and Accomack County Census 2010 Stats* Perdue both maintain poultry processing plants on the shore and are two of the largest employers in Population: 33,164 the area. The agricultural community has drawn Race: many Hispanic or Latino immigrants and migrant 68% White workers to the area; these workers spend all or 29% African American parts of their year working in farms or factories.
    [Show full text]
  • MARCH 29 2007 Frederick County Mills ACCOMMODATION FACTORY
    MARCH 29 2007 Frederick County Mills ACCOMMODATION FACTORY ( ) David Foute advertised wool carding at Accommodation Factory, Dumb Quarter extended, Frederick-Town Herald, June 23, 1827. ADAMS FULLING MILL (9) Frederick Brown advertised wool carding at 6-1/4 cents per pound at the old establishment of Mr. Adams, about 2 miles south of New Market, Frederick-Town Herald, May 11, 1831, p. 4. He had offered fulling and dyeing there (Mrs. Adams’), Ibid., August 20, 1825. This was presumably the fulling mill shown on the 1808 Charles Varlé map on Bush Creek, 0.33 mile north of the present Weller Road, SE of Monrovia. The 1860 Bond map showed the Mrs. H. Norris wool factory, while the 1878 atlas showed Mrs. Norris with a grist and sawmill. ADLER ROPEWALK (F) A ropewalk operated by John Adler in 1819 was on South Market Street, Frederick. The building was occupied in 1976 by Federated Charities (See, Ralph F. Martz, “Richard Potts,” Frederick Post, May 11, 1976, p. A-7). ADELSPERGER MILL CO (5) This steam foundry and machine shop was listed in the 1860 census of manufactures with $14,000 capital investment and 25 employees; annual output was $5000 in castings and $25,000 in machinery. ADLUM STILL ( ) John Adlum advertised to sell two stills, 106-gallon and 49-gallon, Frederick-Town Herald, August 14, 1802. AETNA GLASS WORKS (7) Thomas Johnson purchased some of Amelung’s machinery and built a new Aetna Glass Works on Bush Creek, hauling sand from Ellicott City in empty wheat wagons. He later built another works on Tuscarora Creek, The Potomac, p.
    [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]
  • Maryland Stream Waders 10 Year Report
    MARYLAND STREAM WADERS TEN YEAR (2000-2009) REPORT October 2012 Maryland Stream Waders Ten Year (2000-2009) Report Prepared for: Maryland Department of Natural Resources Monitoring and Non-tidal Assessment Division 580 Taylor Avenue; C-2 Annapolis, Maryland 21401 1-877-620-8DNR (x8623) [email protected] Prepared by: Daniel Boward1 Sara Weglein1 Erik W. Leppo2 1 Maryland Department of Natural Resources Monitoring and Non-tidal Assessment Division 580 Taylor Avenue; C-2 Annapolis, Maryland 21401 2 Tetra Tech, Inc. Center for Ecological Studies 400 Red Brook Boulevard, Suite 200 Owings Mills, Maryland 21117 October 2012 This page intentionally blank. Foreword This document reports on the firstt en years (2000-2009) of sampling and results for the Maryland Stream Waders (MSW) statewide volunteer stream monitoring program managed by the Maryland Department of Natural Resources’ (DNR) Monitoring and Non-tidal Assessment Division (MANTA). Stream Waders data are intended to supplementt hose collected for the Maryland Biological Stream Survey (MBSS) by DNR and University of Maryland biologists. This report provides an overview oft he Program and summarizes results from the firstt en years of sampling. Acknowledgments We wish to acknowledge, first and foremost, the dedicated volunteers who collected data for this report (Appendix A): Thanks also to the following individuals for helping to make the Program a success. • The DNR Benthic Macroinvertebrate Lab staffof Neal Dziepak, Ellen Friedman, and Kerry Tebbs, for their countless hours in
    [Show full text]
  • View of Valley and Ridge Structures from ?:R Stop IX
    GIJIDEBOOJ< TECTONICS AND. CAMBRIAN·ORDO'IICIAN STRATIGRAPHY CENTRAL APPALACHIANS OF PENNSYLVANIA. Pifftbutgh Geological Society with the Appalachian Geological Society Septembet, 1963 TECTONICS AND CAMBRIAN -ORDOVICIAN STRATIGRAPHY in the CENTRAL APPALACHIANS OF PENNSYLVANIA FIELD CONFERENCE SPONSORS Pittsburgh Geological Society Appalachian Geological Society September 19, 20, 21, 1963 CONTENTS Page Introduction 1 Acknowledgments 2 Cambro-Ordovician Stratigraphy of Central and South-Central 3 Pennsylvania by W. R. Wagner Fold Patterns and Continuous Deformation Mechanisms of the 13 Central Pennsylvania Folded Appalachians by R. P. Nickelsen Road Log 1st day: Bedford to State College 31 2nd day: State College to Hagerstown 65 3rd day: Hagerstown to Bedford 11.5 ILLUSTRATIONS Page Wagner paper: Figure 1. Stratigraphic cross-section of Upper-Cambrian 4 in central and south-central Pennsylvania Figure 2. Stratigraphic section of St.Paul-Beekmantown 6 rocks in central Pennsylvania and nearby Maryland Nickelsen paper: Figure 1. Geologic map of Pennsylvania 15 Figure 2. Structural lithic units and Size-Orders of folds 18 in central Pennsylvania Figure 3. Camera lucida sketches of cleavage and folds 23 Figure 4. Schematic drawing of rotational movements in 27 flexure folds Road Log: Figure 1. Route of Field Trip 30 Figure 2. Stratigraphic column for route of Field Trip 34 Figure 3. Cross-section of Martin, Miller and Rankey wells- 41 Stops I and II Figure 4. Map and cross-sections in sinking Valley area- 55 Stop III Figure 5. Panorama view of Valley and Ridge structures from ?:r Stop IX Figure 6. Camera lucida sketch of sedimentary features in ?6 contorted shale - Stop X Figure 7- Cleavage and bedding relationship at Stop XI ?9 Figure 8.
    [Show full text]
  • The Recreation the Delmarva Peninsula by David
    THE RECREATION POTENTIAL OF THE DELMARVA PENINSULA BY DAVID LEE RUBIN S.B., Massachusetts Institute of Technology (1965) SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOT THE DEGREE OF MASTER IN CITY PLANNING at the MASSACHUSETTS INSTITUTE OF TECHNOLOGY June, 1966 Signature of Author.,.-.-,.*....... .. .*.0 .. .. ...... .. ...... ... Department of City and Regional Planning May 23, 1966 Certified by.... ....... .- -*s.e- Super....... Thesis Supervisor Accepted by... ... ...tire r'*n.-..0 *10iy.- .. 0....................0 Chairman, Departmental Committee on Graduate Students 038 The Recreation Potential of the Delmarva Peninsula By David Lee Rubin Submitted to the Department of City and Regional Planning on 23 May, 1966 in partial fulfillment of the requirements for the degree of Master in City Planning. rhis thesis is a plan for the development of Lne recreation potential of the Delmarva Peninsyla, the lower counties of Delaware and the Eastern Shore of Maryland and Virginia, to meet the needs of the Megalopolitan population. Before 1952, the Delmarva Peninsula was isolated, and no development of any kind occurred. The population was stable, with no in migration, and the attitudes were rural. The economy was sagging. Then a bridge was built across the Chesapeake Bay, and the peninsula became a recreation resource for the Baltimore and Washington areas. Ocean City and Rehoboth, the major resorts, have grown rapidly since then. In 1964, the opening of the Chesapeake Bay Bridge-Tunnel further accellerated growth. There are presently plans for the development of a National Seashore on Assateague Island, home of the Chincoteague ponies, as well as state parks along the Chesapeake Bay, and such facilities as a causeway through the ocean and a residential complex in the Indian River Bay.
    [Show full text]
  • Report of Investigations 71 (Pdf, 4.8
    Department of Natural Resources Resource Assessment Service MARYLAND GEOLOGICAL SURVEY Emery T. Cleaves, Director REPORT OF INVESTIGATIONS NO. 71 A STRATEGY FOR A STREAM-GAGING NETWORK IN MARYLAND by Emery T. Cleaves, State Geologist and Director, Maryland Geological Survey and Edward J. Doheny, Hydrologist, U.S. Geological Survey Prepared for the Maryland Water Monitoring Council in cooperation with the Stream-Gage Committee 2000 Parris N. Glendening Governor Kathleen Kennedy Townsend Lieutenant Governor Sarah Taylor-Rogers Secretary Stanley K. Arthur Deputy Secretary MARYLAND DEPARTMENT OF NATURAL RESOURCES 580 Taylor Avenue Annapolis, Maryland 21401 General DNR Public Information Number: 1-877-620-8DNR http://www.dnr.state.md.us MARYLAND GEOLOGICAL SURVEY 2300 St. Paul Street Baltimore, Maryland 21218 (410) 554-5500 http://mgs.dnr.md.gov The facilities and services of the Maryland Department of Natural Resources are available to all without regard to race, color, religion, sex, age, national origin, or physical or mental disability. COMMISSION OF THE MARYLAND GEOLOGICAL SURVEY M. GORDON WOLMAN, CHAIRMAN F. PIERCE LINAWEAVER ROBERT W. RIDKY JAMES B. STRIBLING CONTENTS Page Executive summary.........................................................................................................................................................1 Why stream gages?.........................................................................................................................................................4 Introduction............................................................................................................................................................4
    [Show full text]
  • Savage River State Forest Is a Natural Area with Hunting Is Permitted Throughout the Forest
    DIRECTIONS Take Exit 22 off I-68, turn left and go south on Chestnut Ridge WELCOME Please Play Safe! HUNTING Savage River Reservoir Road. At the stop sign, turn left onto New Germany Road. Savage River State Forest is a natural area with Hunting is permitted throughout the forest. The Savage River Reservoir provides fishing and Continue for two miles. Turn right onto Headquarters Lane certain hazards such as overhanging branches, Boundaries are marked with yellow paint. No paddling opportunities. Boat launches are located and continue to the forest office on the right. rocky and slippery trails, and venomous hunting allowed where there are safety zone signs or at Big Run State Park, Dry Run Road and near the snakes. Bottles of water and sturdy shoes are where posted by private landowners. Hunters should breast of the dam. No gasoline motors are permitted. Approximately 3 hours from Washington, D.C./Baltimore, 2 hours from Pittsburgh. recommended while exploring, as well as blaze consult the Maryland Hunting Guide — available at Anglers can catch Catfish, Trout, Bass and Tiger orange clothing during hunting seasons. Some of dnr.maryland.gov/huntersguide — for exact season Muskie. Depending on the season, visitors may More information is available at dnr.maryland.gov/ the forest trails are gravel roads, which are open dates and bag limits. see grouse, great blue herons, king fishers, minks publiclands/western/savageriverforest.asp or by contacting to motor vehicles at various times. Remember, and eagles as well. Swimming in the Reservoir is the forest office. you are responsible for having the necessary Several access roads are available to hunters with prohibited.
    [Show full text]
  • Maryland Department of Natural Resources
    MARYLAND DEPARTMENT OF NATURAL RESOURCES WILDLIFE AND HERITAGE SERVICE WILDLIFE MANAGEMENT PLAN For INDIAN SPRINGS WILDLIFE MANAGEMENT AREA 15 YEAR VISION PLAN Location 14038 Blairs Valley Road Clear Spring, MD 21722 In Washington County Maryland On Approximately 6,635 acres Prepared by: Maryland Department of Natural Resources Wildlife & Heritage Service Indian Springs Wildlife Management Area 14038 Blairs Valley Rd Clear Spring, Maryland 21722 301-842-2702 March 2014 Introduction The Maryland Department of Natural Resources, Wildlife & Heritage Service (WHS) is responsible for the management of approximately 106,000 acres of State property. These areas, entitled “Wildlife Management Areas” (WMA), encompass 44 separate tracts of land and are located in 18 of the 23 counties that make up the State. WMA’s range in size from as small as 20 acres to well over 29,000 acres, and represent most, if not all, of the major habitat types found throughout the State of Maryland. These properties make up a significant portion of the Department’s land holdings of approximately 440,000 acres. In 1940 the former Maryland Game and Inland Fish Commission made their initial purchase of 1,225.57 acres, with the property designed as a Wildlife Management Area and named after the small adjacent community of Indian Springs. At the time, this land was purchased using Pittman-Robertson Federal Aid in Wildlife Restoration (PR) funds. This 1937 federally enacted legislation provided reliable funding to state wildlife departments by placing a federal excise tax on sporting arms and ammunition, which are earmarked solely for wildlife conservation. WHS has the principal responsibility to lead in the management of Indian Springs WMA.
    [Show full text]