DOCSLIB.ORG

VT Sheet3 DMU CMU Final

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
VT Sheet3 DMU CMU Final U.S. DEPARTMENT OF THE INTERIOR Prepared in cooperation with the SCIENTIFIC INVESTIGATIONS MAP 3184 U.S. GEOLOGICAL SURVEY STATE OF VERMONT, VERMONT AGENCY OF NATURAL RESOURCES, BEDROCK GEOLOGIC MAP OF VERMONT MARCIA K. McNUTT, DIRECTOR VERMONT GEOLOGICAL SURVEY SHEET 3 OF 3 (FRONT) LAURENCE R. BECKER, STATE GEOLOGIST CORRELATION OF MAP UNITS (Some lesser units listed in the Description of Map Units may not be shown here. Asterisk indicates U-Pb zircon age.) NEW HAMPSHIRE PLUTONIC SUITE Zfc 2 OTHER DEVONIAN Carbonaceous albite schist member—Gray to medium-dark-gray, Y lga Ludlow Mountain aplitic gneiss (Middle Mesoproterozoic)—Light-gray to Owwu Sandy phyllite, granofels, and cherty phyllite (Upper Ordovician)—Gray and Belvidere Mountain Structural Complex (Cambrian and Neoproterozoic) Compton Formation (Lower Devonian) Oarq Coarsely porphyritic, greenish-gray, light-bluish-gray, or medium-bluish-gray GRANITES rusty-weathering, carbonaceous albite-chlorite-quartz-muscovite schist, contain- white, very fine grained microcline-plagioclase-quartz (±magnetite) aplitic gneiss; grayish-green rocks associated with Whipstock breccia on Whipstock Hill but of metarhyolite tuff, lapilli tuff, and tuff breccia. Quartz and plagioclase pheno- STAGE GRANITE BLACK FRENCH AND PLUTONS STAGE Brandon Lignite POND ing porphyroblasts of black albite. Unit resembles gray albitic granofels and contains sparing amounts of biotite, and secondary muscovite. Unit interpreted to uncertain correlation Zbu Ultramafic rocks—Brown to white-weathering, green, massive, moderately to Dco Metasandstone member—Light-gray to tan, micaceous, locally calcareous crysts commonly as large as 5 mm DIKES MOUNTAIN AGE UNCERTAIN 2 2 Tmb GRANITE GRANITE schist of the Hoosac Formation (Zhab) be border facies of Y lgg. Y ap is similar aplitic gneiss, but is not in contact with fully serpentinized dunite and peridotite and schistose serpentinite; metasandstone and slate or metamudstone in beds a few centimeters to tens of Lower 2 2 Miocene TERTIARY Dg Dfpg either Y lgg or Y phg. Exposed on Ludlow Mountain Owbl Graptoliferous slate (Upper Ordovician)—Black slate of Climacograptus rusty-weathering, medium-grained talc-carbonate rock and quartz-carbonate centimeters thick. Graded bedding common. Interpreted to be correlative with Oat Metamorphosed aphyric rhyolite tuff *364 Ma *365 Ma 365* Ma Zfqz 365 Ma 24 Ma 365 Ma Quartzite member—White quartzite and tan to light-gray, medium-grained bicornis Biozone on and west of Whipstock Hill, otherwise typical of slates of the (magnesite) rock the Gile Mountain Formation Dbmg BARRE EAST BETHEL 2 PLUTONS muscovite quartzite locally rich in magnetite. Resembles quartzite of the Tyson Y phg Proctor Hill granodiorite gneiss (Middle Mesoproterozoic)—Gray to pinkish- Walloomsac Formation shown as Ow Oam Medium-light-bluish-gray, medium-bluish-gray, medium-dark-gray, to medium- break in scale PLUTONS DERBY *368 Ma PLUTON Formation (Ztq) 2 gray, gneissoid magnetite-biotite-microcline-perthite granodiorite, and locally Zbc Coarse-grained amphibolite—Dark-gray, coarse-grained amphibolite and Dcoa Amphibolite member—Garnetiferous hornblende schist and minor dark-greenish-gray metasiltstone and phyllite, and medium-gray feldspathic Dbbg Dbqm Y pha WHITE MOUNTAIN IGNEOUS SUITE Ddbg microcline megacrystic gneissic granite, well-foliated and highly variable in compo- layered amphibolite composed of barroisite, epidote, garnet, actinolite, albite, hornblende amphibolite metawacke. Purple tinge common; coticule and magnetite locally abundant FAMENNIAN FAMENNIAN 2 (consisting of plutons and dike swarms Ddrz Zfs Schist member—Silvery-green to rusty-tan, fine-grained chlorite-quartz- sition, having aplitic and hornblende-rich reaction zones (Y pha) where in contact chlorite, sphene, sericite, biotite, and calcite VICTORY (Dbg) Rocks of the Giddings Brook, Sunset Lake, and Bird Mountain slices of Jurassic to Early Cretaceous age) sericite (±garnet±chloritoid±allanite) schist and phyllite. Resembles green with calc-silicate rocks. Crosscuts all paragneiss units; is a thoroughly gneissic Di Ironbound Mountain Formation (Lower Devonian)—Medium-dark-gray to Oac Siliceous and argillaceous dolomite and calcareous pelite Upper Devonian Upper Devonian PLUTON (Dqm) WILLOUGHBY PLUTON CUTTINGSVILLE STOCK (Ddg) Dwmz phyllites of the Pinney Hollow Formation (Zph) and Mount Abraham Forma- rock. Correlated with the Ludlow Mountain granodiorite gneiss Zbf Fine-grained amphibolite—Bluish-gray, fine- to medium-grained albite-horn- grayish-black lustrous slate, phyllite, and schist containing sparse to moderately DIKES 100 Ma Opaw Pawlet Formation (Upper Ordovician)—Light-gray, tan-weathering, Dvbg (Dg) Dwwz Oap 375 Ma Kqs 375 Ma tion (Za) and chloritic phyllite (Ztg) of the Tyson Formation blende-epidote-actinolite (±garnet) amphibolite and quartz-bearing amphibolite abundant 1-mm to- 5-cm-thick beds of light-gray, fine-grained metasandstone and Dark-gray to grayish-black, rusty-weathering sulfidic slate and phyllite interlay- (Debg) mica-speckled, massive to thin-bedded quartz-plagioclase wacke interbedded with Kns Dwhz Y2cp NIAN NIAN Cole Pond tonalite gneiss (Middle Mesoproterozoic)—Gray to medium-dark- ered with felsic tuffs and minor sandy rocks; locally forms the base of the FRAS- FRAS- Oag metasiltstone, commonly pyritiferous and calcareous. Some graded beds. Grada- Kes Kab (Dedg) dark-gray carbonaceous slate. Contains distinctive autoclastic chips of gray slate, (Degr) gray, biotite-rich metatonalite gneiss, having irregular screens, and xenoliths of Zbg Mafic schist—Green, fine-grained schist composed of chlorite, actinolite, albite, tional contact with Dco above and Dir below. Interpreted to be correlative with the Ammonoosuc Volcanics 382 Ma 382 Ma fragments of dacitic to andesitic volcanics, and subangular clasts of dark-gray Kpd Kmd (Dwdg) BARBER HILL ASCUTNEY MOUNTAIN IGNEOUS COMPLEX CONNECTICUT VALLEY TROUGH Pinney Hollow Formation (Cambrian and Neoproterozoic) more mafic hornblende-biotite tonalite or diorite gneiss. U-Pb zircon SHRIMP age quartz and oligoclase. Interbedded black slates contain graptolites of the C. and epidote with biotite, calcite, sericite, quartz, sphene, pyrite, and magnetite; Meetinghouse Slate Member of the Gile Mountain Formation TIAN TIAN GIVE- GIVE- STOCK Kag Kgd Lower CRETACEOUS Zph of 1,321±9 Ma, no. 7 (Ratcliffe and others, 1991; Aleinikoff and others, 2011) bicornis Biozone (see Webby and others, 2004, fig. 2.1) (lower to middle includes homogeneous schistose greenstone, albitic greenstone, and massive Kas Kahg 387 Ma Kbh 387 Ma Phyllite member—Light-greenish-gray to lustrous pale-green chlorite- Mohawkian). Interpreted as uncomformable on rocks as old as the Hatch Hill banded greenstone Dih Halls Stream Grit Member (of Myers, 1964)—Lenticular masses of coarse- Washburn Brook Formation (Upper and Middle Ordovician) Kfd 2 Khf Kav BRONSON HILL AREA Zphc muscovite-quartz (±chloritoid±garnet±magnetite) phyllite. Chloritoid-rich rocks Y bv Bondville metadacite and trondhjemite gneiss (Middle Mesoproterozoic)— Formation and possibly the West Castleton Formation of the allochthon. Unit is grained quartzose volcaniclastic grit and cobble metaconglomerate commonly Owc CHESTER (Zphc) appear gritty owing to distributed porphyroblasts of chloritoid. Unit is Light-gray to whitish-gray, fine-grained biotite trondhjemitic gneiss, locally contain- indistinguishable from beds in the Austin Glen Graywacke (after Potter, 1972) Zbs Spangly schist—Silvery-blue, medium-grained tectonic mélange composed of with abundant dark-gray metapelitic matrix (diamictite) interlayered with Metamorphosed gray siltstone, quartzite, volcanogenic chert, and ironstone, all DOME NULHEGAN locally albitic and contains minor beds of quartzite ing abundant magnetite. U-Pb zircon SHRIMP age of 1,342 Ma, no. 6B (Ratcliffe (Oag) interpreted as synorogenic autochthonous rocks muscovite schist with minor amounts of chlorite, epidote, albite, and tourmaline; metasandstone, metapelite, and porphyritic metarhyolite. Grit contains suban- typically containing coticule and magnetite GRANITE PLUTON Middle Devonian EIFELIAN EIFELIAN 144 Ma Middle Devonian Y1rta and others, 1991; Aleinikoff and others, 2011) contains fragments and discontinuous lenses of greenstone, coarse-grained gular clasts of plagioclase and potassic feldspar as large as 2.5 cm across and SOUTH- CENTRAL- NORTH- SAWYER Dg SHAW MOUNTAIN, NORTHFIELD, WAITS RIVER EASTERN EASTERN EASTERN MOUNTAIN Dnqm (See DMU for Zphq Feldspathic quartz schist member—Light-gray to grayish-green, laminated, Omm Mount Merino Formation (Upper Ordovician)—Light-gray, powdery-weather- amphibolite, and talc phyllite larger clasts of dark-gray slate. Conglomerate contains rounded clasts of meta- Ows Metamorphosed sedimentary breccia interlayered with dark-gray slate and Upper *392 Ma unlisted symbols) 1 MONADNOCK AND GILE MOUNTAIN FORMATIONS VERMONT VERMONT VERMONT BELT gritty feldspathic chlorite-muscovite-plagioclase-quartz schist Y rt Rawsonville trondhjemite gneiss (Early Mesoproterozoic)—Chalky-white to ing, and red, green, and dark-gray, thinly bedded siliceous argillite and mudstone rhyolite, fine-grained granitoid, and rare marble, and angular clasts of dark-gray micaceous siltstone. Clasts include light-colored, fine-grained metasandstone MOUNTAIN 159 Ma Littleton Formation light-gray-weathering, medium- to coarse-grained biotite metatrondhjemite and Zbagn Albite gneiss—White, light-gray- and green-banded, fine- to medium-grained,
Load more

Recommended publications
  • Taconic Physiography
    Bulletin No. 272 ' Series B, Descriptive Geology, 74 DEPARTMENT OF THE INTERIOR . UNITED STATES GEOLOGICAL SURVEY CHARLES D. WALCOTT, DIRECTOR 4 t TACONIC PHYSIOGRAPHY BY T. NELSON DALE WASHINGTON GOVERNMENT PRINTING OFFICE 1905 CONTENTS. Page. Letter of transinittal......................................._......--..... 7 Introduction..........I..................................................... 9 Literature...........:.......................... ........................... 9 Land form __._..___.._.___________..___._____......__..__...._..._--..-..... 18 Green Mountain Range ..................... .......................... 18 Taconic Range .............................'............:.............. 19 Transverse valleys._-_-_.-..._.-......-....___-..-___-_....--_.-.._-- 19 Longitudinal valleys ............................................. ^...... 20 Bensselaer Plateau .................................................... 20 Hudson-Champlain valley................ ..-,..-.-.--.----.-..-...... 21 The Taconic landscape..................................................... 21 The lakes............................................................ 22 Topographic types .............,.....:..............'.................... 23 Plateau type ...--....---....-.-.-.-.--....-...... --.---.-.-..-.--... 23 Taconic type ...-..........-........-----............--......----.-.-- 28 Hudson-Champlain type ......................"...............--....... 23 Rock material..........................'.......'..---..-.....-...-.--.-.-. 23 Harder rocks ....---...............-.-.....-.-...--.-.........
    [Show full text]
  • Preliminary Bedrock Geologic Map of the Chittenden Quadrangle Rutland County, Vermont
    U.S. DEPARTMENT OF THE INTERIOR U. S. GEOLOGICAL SURVEY Preliminary Bedrock Geologic Map of the Chittenden Quadrangle Rutland County, Vermont By Nicholas M. Ratcliffe U.S. Geological Survey Open File Report 97-703 1997 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards nor with the North American Stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. INTRODUCTION The bedrock of the Chittenden quadrangle consists of Middle Proterozoic through Cambrian metasedimentary and metaigneous rocks that lie along the western flank of the Green Mountain massif in south-central Vermont. The Green Mountain massif is cored by highly deformed and extensively retrograded schists and schistose gneisses derived from once high-grade gneisses that were intruded and originally metamorphosed during the Grenville orogeny prior to about 950 Ma. Upper Proterozoic through Cambrian metaclastic rocks, referred to as the western cover sequence, form a cover sequence that was deposited unconformably on the older schists and gneisses. The upper part of the cover sequence consists of marine-shelf carbonate rocks of the Vermont Valley sequence that developed on the stable Atlantic-type continental margin prior to the deformation in the Taconian orogeny during the Middle to Upper Ordovician. In the Taconian orogeny, rocks of this area were thrust faulted and metamorphosed to biotite grade. The basement rocks were altered by low-grade remetamorphism and hydration to such an extent that the Grenvillian mineral assemblages, schistosity, and gneissosity are presently barely recognizable.
    [Show full text]
  • Dorset Village Plan
    Revitalizing Southern Vermont’s Villages Dorset, Vermont August 2013 Dorset Revitalization Planning Dorset VT Dorset is a town in Bennington County, Vermont, United States. Dorset is famous for being the location of Cephas Kent's Inn, where four meetings of the Convention that signed the Dorset Accords led to the independent Vermont Republic, and future statehood. Dorset is home to America's oldest marble quarry and is the birthplace of Alcoholics Anonymous co-founder Bill W. East Dorset is the setting of the Bill Wilson House and the Griffith Library. The East Dorset marble quarry was established by Bill W's great grandfather and stayed in the family for 3 generations. Marble from these quarries provided stone for the New York Public Library Main Branch building in New York City The Town of Dorset has an area of 29,463 acres, or 46.04 square miles, made up of many types of land and waterways: flat valley land, swamps, rolling hills, steep mountains, streams and rivers. 14,228 acres contain slopes in excess of 20%, and 2,880 acres have elevations above 2500 feet. The physiography of the Town may be described as two roughly north-south valleys, which contain most of Dorset's development, together with parts of three north-south mountainous areas, which define the valleys. The eastern edge of the Town runs along the western slope of the Green Mountains. The southwestern corner of the Town occupies the northeastern slope of Mother Myrick Mountain, in the Taconic Mountain Range. Thrusting into Dorset from the north is a mountainous area, also part of the Taconic Range, extending south from Dorset Mountain, whose summit, close to the northern town line, is over 3800 feet above sea level.
    [Show full text]
  • Green Mountain National Forest Supervisor’S Office 1-802-747-6700 TTY 1-802-747-6765
    Green Mountain United States Department of Agriculture National Forest Forest Service Eastern Region Record of Decision R9-GM-FEIS- Final Environmental Impact Statement ROD February 2006 To Accompany the Land and Resource Management Plan This document is available in large print. Contact the Green Mountain National Forest Supervisor’s Office 1-802-747-6700 TTY 1-802-747-6765 The U.S. Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, gender, religion, age, disability, political beliefs, sexual orientation, or marital or family status. (Not all prohibited bases apply to all programs.) Persons with disabilities who require alternative means for communication of program information (Braille, large print, audiotape, etc.) should contact USDA’s TARGET Center at (202) 720-2600 (voice and TDD). To file a complaint of discrimination, write USDA, Director, Office of Civil Rights, Room 326-W, Whitten Building, 14th and Independence Avenue, SW, Washington, DC 20250- 9410 or call (202) 720-5964 (voice and TDD). USDA is an equal opportunity provider and employer. Record of Decision Final Environmental Impact Statement to accompany the Land and Resource Management Plan Green Mountain National Forest Eastern Region Milwaukee, Wisconsin February 2006 Responsible Agency USDA Forest Service Responsible Official Randy Moore, Regional Forester Gaslight Building, Suite 800 626 E. Wisconsin Avenue Milwaukee, WI 53203 414-297-3765 For further information contact Melissa
    [Show full text]
  • The Vermont Stone Trail 2016
    The Vermont Stone Trail A Visitor’s Guide to Granite, Marble and Slate in the Green Mountain State Lake Willoughby Photo courtesy Annalie Babson Table of Contents The 2 The Story of Stone in Vermont Vermont 6 Southern Region Stone Trail 14 Central Region 32 Northern Region A Visitor’s Guide to Granite, Marble and Slate in the Green Mountain State Using this Guide The information in this guide is arranged into southern, central and northern regions of Vermont. Each section begins with a map Serendipity and the dynamic nature of the earth’s showing the number and location of landmarks and points of interest crust gave Vermont rare and excellent deposits of described in the guide pages. The guide pages include a landmark granite, marble and slate. With hard work, description and graphic icons creativity and the efforts of many, each of these indicating the type of stone, features and activities for each resources has been developed into a highly location. successful industry that continues to offer products Landmark Legend that are sought after throughout the world. Type of stone The Vermont Stone Trail is a guide to geological Marble regions of Vermont where granite, marble and slate Slate Granite were quarried, manufactured and utilized. Combination Vermont’s diverse geologic resources have been Other Dimensional used to create some of the finest buildings, Stone provocative memorials and stunning works of art Landmark features and activities found around the world. The Vermont Stone Trail Geology Above: A historical photo of a Boutwell, Milne & Varnum Company Quarry, Barre. invites visitors and residents alike to find a wealth Quarries/ On the cover: An artist uses the pointing machine method to reproduce a marble sculpture in the early 20th century.
    [Show full text]
  • The Surficial Geology and Hydrogeology of Dorset, Vermont
    THE SURFICIAL GEOLOGY AND HYDROGEOLOGY OF DORSET, VERMONT By David J. De Simone and Marjorie Gale June 2009 Vermont Geological Survey 103 South Main Street Logue Cottage Waterbury, VT 05671-2420 Laurence R. Becker Vermont State Geologist Introduction Field work for this project was carried out during the 2006 and 2007 field seasons. Data analysis and map revisions were done in 2008 and completed in 2009. Maps discussed in this report are: 1. Surficial Geology 2. Stratigraphic Cross Sections 3. Field Data Sites 4. Springs, Seeps & Water Well Locations 5. Deglacial History 6. Depth to Bedrock 7. Bedrock Topography 8. Discharge Areas and Possible Shallow Overburden Aquifers 9. Hydrogeologic Units 10.Recharge Potential to Bedrock Aquifer 11.Potentiometric Surface Map and Groundwater Flow Lines Location and Geologic Setting The town of Dorset encompasses portions of the West Rupert, Manchester, Peru, Dorset and Danby 1:24000 topographic quadrangles and covers approximately one quadrangle of area. Two major valleys separate three upland regions. The Dorset Valley trends northwest and contains the West Branch Batten Kill that flows southeast into Manchester. In the vicinity of Dorset Village, there is a broad drainage divide consisting of wetlands. North of this divide, the Mettawee River enters the valley from head waters in the central upland region and flows northwest into New York. The upper Mettawee River represents a notable east-west tributary valley referred to as Mettawee Hollow. In the east, the East Dorset Valley trends north-northeast and is a continuation of the Vermont Valley. The Batten Kill flows southward from a divide just north of the village of East Dorset.
    [Show full text]
  • MINERAL COLLECTING in VERMONT by Raymond W. Crant
    MINERAL COLLECTING IN VERMONT by Raymond W. Crant Vermont Geological Survey, Charles C. Doll, State Geologist Department of Water Resources, Montpelier, Vermont SPECIAL PUBLICATION NO, 2 1968 LIST OF ILLUSTRATIONS Figures Page 1. Index Map of Vermont Mineral L()cIities . 3 38. Slate Quarry, Poultney ............................................. 31 2. Metaiimrphic Map of Vermont ................................. 4 .39. NI ap showing the location of the mineral area, Rouiid 3. Geo logic NI ap of Vernio i it ....................................... 7 Hill, Shrewshorv................................. ..................... 32 4. Topograpl ii NI a!) S y 0)1)0 Is ....................................... 10 40. Map showing the location of the Molybdenite Prospect 5. Map showing the location of the Vermont Kaolin Coin- (1) and Copperas Hill Mines (2), Cuttingsville .............32 paiiy Quarry (1) and Monkton Iron Ore Beds (2) ......... 14 41. Map showing the location of the Marble Quarry, Dorset 6. Map showing the location of the Huntley Quarry, Leices- Nit., South Danhv ..................................................... 33 terJunction ............................................................. 15 42. Map showing the location of the Devil's Den, Nit. Tahor 34 7. Calcite crystals from the Huntley Quarry, Leicester 43. Smoky Quartz crystal from Devil's Den, Mt. Tabor ...... .34 Junction (times 1.6) .................................................. 15 44. Map showing the location of the Roacicuts on Route 155, 8. Map showing the location of
    [Show full text]
  • 5. PART-2.Pdf
    Part Two Biophysical Regions of Vermont Biophysical Regions of Vermont ne of the most rewarding parts of studying a landscape and its natural communities is appreciating all the factors that work together to cause Ovariation within that landscape. When we study the landscape of the world, we look to climate to explain most of the broad patterns of geographic variation. As we look more closely, say at the North American continent, climate is still the overrid- ing feature that causes variation, but we begin to see influences from other factors such as geological history. As we look even more closely, for example at the state of Vermont, we begin to see that landforms and soils, along with human history, influence variations as well. The biophysical regions of Vermont presented in Figure 2 help organize the landscape into smaller units that share features of climate, geology, topography, soils, natural communities, and human history. Although each region has variation within it, all are widely recognized as units that are more similar than they are different. Figure 2 was developed by analyzing existing land classification maps and by assessing biological and physical data with new analytical techniques (Girton 1997). The map was created so that land managers from all state and federal land managing agencies, as well as private land managers, could have a single map of biophysical regions to work with as a way of organizing their planning and thinking about natural communities in Vermont. Although our map shows Vermont only, the regions have no political boundaries, and they do not end at Vermont’s border.
    [Show full text]
  • Report Geology of Vermont
    REPORT ON THE GEOLOGY OF VERMONT: DESCRIPTIVE, THEORETICAL, ECONOMICAL, AND SCENOGRAPHICAL; BY EDWARD HITCHCOCK, LL.D., ALBERT D. HAGER, A.M., EDWARD HITCHCOCK, JR., M.D., CHARLES H. HITCHCOCK, A.M., PROFESSOR OF HYGIENE AND PHYSICAL CULTURE IN AMHERST COLLEGE. GEOLOGIST TO THE STATE OF MAINE. IN TWO VOLUMES. PUBLISHED UNDER VE AUTHORITY OF THE STATE LEGISLATURE, BY ALBERT D. HAGER, PROOTORSVILLE, VT. VOL. I. PRINTED BY THE CLAREMONT MANUFACTURING COMPANY, CLAREMONT, N. 11. 1861. NQTE. The Principal of the Survey desires to state, that the publication of this Report has been entirely under the direction of Mr. A. D. HAGER. In consequence of the great increase of the matter above the original estimate, the work has been a difficult one, and demanded not only much labor, but rigid economy, and great pecuniary responsibility and sacrifice. Yet, as the public will see, it has been carried through in excellent taste, and compares most favorably with the style of analogous Reports in other States. The citizens of Vermont are certainly much indebted to Mr. Hager for his faithful, judicious and persevering efforts - without which, these volumes never could have seen the light in a form so satisfactory. It is but justice, also, to say, that Mr. Hager was fortunate in securing the services of the Messrs. Goddard, of Claremont, for the printing. Had they not possessed unusual skill in deciphering illegible manuscripts and correcting proofs, in some cases where from distance or other causes they had not passed under the eye of the authors, errors would S have abounded where now we trust they are rare.
    [Show full text]
  • The Lay of the Land the CENTER
    CENTER E FO Dedicated to the increase H R T L and diffusion of knowledge A N N O I D about how the nation’s T U A S T lands are apportioned, E RE The Lay of the Land INTERP utilized, and perceived. The Center for Land Use Interpretation winter 2011 “Interpretation is a seed, not a tree.” - from the Interpretive Development Program, National Park Service THROUGH THE GRAPEVINE DIGGING VERMONT SOUTHERN CALIFORNIA’S GREAT MOUNTAIN PASS WHAT LIES BENEATH THE GREEN MOUNTAIN STATE Streams of transit through the Grapevine. CLUI photo CALIFORNIA’S RIDGE ROUTE WAS THE subject of an exhibit at the Center’s Los Angeles space in the latter half of 2010. The ex- hibit, Through the Grapevine: Streams of Transit in Southern Califor- nia’s Great Pass featured digital display panels describing different The grey rock that lies beneath the Green Mountains. CLUI photo aspects of this landscape of transition. Also on view was a landscan VERMONT MAY BE THE MOST uniformly scenic and pastorally of the region, a continuous shot of the landscape between the edge idyllic state in the union. Perhaps many imagine Vermont as roll- of Los Angeles’ sprawl and the beginning of the rural valley at ing hills with rushing brooks and snowy glens, peppered with the base of the Grapevine, shot by the CLUI and Ron Chapple whitewashed villages populated by DIY Yankees, back-to-the-land of Aerial Filmworks from a helicopter with a gyrostabilized high localists, and red barns full of fat happy cows making Ben and definition camera.
    [Show full text]
  • Chapter 2 Alternatives
    Chapter 2 Alternatives Chapter 2 Alternatives Introduction 2-2 Alternative Development 2-2 Changes between the Draft and Final Environmental Impact Statements 2-3 Elements Common to All Alternatives 2-10 Alternatives Considered in Detail 2-13 Alternatives Eliminated from Detailed Study 2-23 Comparison of Alternatives 2-25 Green Mountain National Forest Page 2-1 Alternatives Chapter 2 2.1 ALTERNATIVES response to the issues and need for change. 2.1.1 Introduction The following parameters were used in this process: This chapter describes and compares the five • Congressionally designated areas and management alternatives considered for the special areas will not get smaller Revised Forest Plan for the GMNF. The main • Ski areas and expansion areas will stay focus of this chapter is to sharply define the the same differences between alternatives. Alternatives • Habitats required for species viability provide a framework for analyzing different can’t be eliminated but amounts and ways of meeting the purpose and need and for locations could shift addressing the issues discussed in Chapter 1. These alternatives show a range of options for • The current management (no action) guiding natural resource management activities alternative will not have additional on the GMNF over the next 10 to 15 years. Wilderness Study Areas or Special Areas, and will not use new MAs Alternatives express different desired future • All newly acquired lands (existing MA conditions through different Management Area 9.2) will be assigned a MA designation (MA) allocation. The alternative that is selected except in the current management in the Record of Decision (ROD) will be a alternative management strategy that will guide all natural • There will be more Wilderness Study resource management activities and establish Areas considered and included in at management direction for the GMNF.
    [Show full text]
  • Green Mountain National Forest Comprehensive Trail Strategy
    Green Mountain United States Department of National Forest Agriculture Forest Service Eastern Comprehensive Region July 2015 Trail Strategy Photo Courtesy of Dwight Geis Comprehensive Trail Strategy Team: Manchester Ranger District: William Jackson, District Ranger Roger Boyer, Acting District Ranger Carol Knight, District Recreation Program Manager Joan McCloud, Recreation Specialist (ret.) Danna Strout, Recreation Technician William Garrison, Recreation Technician Rochester/Middlebury Ranger Districts: Christopher Mattrick, District Ranger Holly Knox, District Recreation Program Manager Dundonald Cochrane, III, Recreation Technician Seth Coffey, Recreation Technician David Nulsen, Recreation Technician Kenneth Norden, Forestry Technician Supervisors Office: Donna Grosz, Public Services Staff Officer Melissa Reichert, Recreation Program Manager Carol Burd, Recreation Planner Patricia D’Andrea, Realty Specialist Thomas Tenyah, GIS Specialist _/s/ John A. Sinclair________________ ___7/27/15____ John A. Sinclair Date FOREST SUPERVISOR Green Mountain National Forest The U.S. Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, age, disability, and where applicable, sex, marital status, familial status, parental status, religion, sexual orientation, genetic information, political beliefs, reprisal, or because all or part of an individual’s income is derived from any public assistance program. (Not all prohibited bases apply to all programs.) Persons with disabilities who require alternative means for communication of program information (Braille, large print, audiotape, etc.) should contact USDA’s TARGET Center at (202) 720-2600 (voice and TDD). To file a complaint of discrimination, write USDA, Director, Office of Civil Rights, 1400 Independence Avenue, S.W., Washington, D.C. 20250-9410, or call (800) 795-3272 (voice) or (202) 720-6382 (TDD).
    [Show full text]