Oliverian Domes, Related Plutonic Rocks, and Mantling Ammonoosu;C Volcanics of the Bronson Hill Anticlinorium, New England Appalachians

Total Page:16

File Type:pdf, Size:1020Kb

Oliverian Domes, Related Plutonic Rocks, and Mantling Ammonoosu;C Volcanics of the Bronson Hill Anticlinorium, New England Appalachians Oliverian Domes, Related Plutonic Rocks, and Mantling AmmonoosU;c Volcanics of the Bronson Hill Anticlinorium, New England Appalachians U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1516 Oliverian Domes, Related Plutonic Rocks, and Mantling Ammonoosuc Volcanics of the Bronson Hill Anticlinorium, New England Appalachians By GERHARD W. LEO U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1516 Major- and trace-element geochemistry of the Oliverian Plutonic Suite (Middle Ordovician to Early Silurian?), associated volcanogenic gneisses, and mantling but chemically distinct Ammonoosuc Volcanics and related trondhjemite is interpreted to indicate a transitional oceanic-continental volcanic arc in west-central New England UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1991 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 Library of Congress Cataloging in Publication Data Leo, Gerhard W. Oliverian domes, related plutonic rocks, and mantling Ammonoosuc Volcanics of the Bronson Hill Anticlinorium, New England Appalachians I by Gerhard W. Leo p. em. - (U.S. Geological Survey professional paper; 1516) Includes bibliographical references. Supt. of Docs. no.: I 19.19:1516 1. Intrusions (Geology)-New England Region. 2. Geology, Stratigraphic-Ordovician. 3. Geology, Stratigraphic-Silurian. 4. Geology-New England Region. I. Title. II. Series. QE611.5.N49L46 1991 551. 7'3'0974-dc20 90-4951 CIP For sale by the Books and Open-File Reports Section, U.S. Geological Survey, Federal Center, Box 25425, Denver, CO 80225 CONTENTS Page Abstract ........................................................................... 1 Oliverian Plutonic Suite and Other Rocks in Cores of Introduction....................................................................... 1 Domes -Continued Acknowledgments........................................................... 3 Descriptions of Individual Domes and Plutons-Continued Regional Relationships . 3 Southern New Hampshire and Northern Massachu­ Ordovician Formations . .. .. .. .. .. 3 setts Plutons-Continued Dead River Formation (Former Albee Formation) . 3 Mascoma Dome and Pluton................................ 43 Orfordville Formation (Abandoned) . 4 Holts Ledge Volcanic Sequence.................... 43' Partridge Formation . 4 "Stratified Core Gneiss".............................. 46 ~ Quimby Formation.................................................. 5 Lebanon Dome and Pluton .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. 46 Silurian Formations . 5 Croydon Dome and Pluton .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. 47 Clough Quartzite and Fitch Formation . 5 Unity Dome and Gneiss.................................... 47 Devonian Formations . 5 Alstead Dome and Gneiss.................................. 47 Littleton Formation . 5 Vernon Dome and Pluton.................................. 48 Erving, Gile Mountain, and Waits River Formations.... 5 Warwick Dome and Pauchaug Gneiss .. .. .. .. .. .. .. .. .. .. .. .. 48 Ammonoosuc Volcanics and Related Rocks . 5 Monson Gneiss and Swanzey Gneis~ of the Keene Holts Ledge Volcanic Sequence....................................... 12 Dome.......................................................... 49 Ammonoosuc Trondhjemite . 22 Monson Gneiss . 51 Dikes and Sills . .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. 22 Swanzey Gneiss............................................... 52 Larger Trondhjemite Masses . 27 Highland croft Plutonic Suite................................................ 52 Contact Relationships of the Ammonoosuc Volcanics . 27 Geochemistry . 52 Isotopic Age(s) of the Ammonoosuc Volcanics and Related Methods...................................................................... 52 Rocks................................................................ 27 Gneisses of the Oliverian Plutonic Suite and Related Oliverian Plutonic Suite and Other Rocks in Cores of Domes . 32 Rocks................................................................ 53 Tectonic Development . 33 Major Elements..................................................... 53 Descriptions of Individual Domes and Plutons . 33 Trace Elements Other Than Rare Earths . 53 Jefferson Dome and Batholith.................................. 33 Rare-Earth Elements .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. 58 Berlin Area of New Hampshire.......................... 33 Ammonoosuc Volcanics and Associated Trondhjemite . 61 Gneiss of the Oliverian Plutonic Suite .. .. .. .. .. 33 Major Elements..................................................... 61 Structural Relationship to the Ammonoosuc Trace Elements Other Than Rare Earths . 63 Volcanics......................................... 35 Rare-Earth Elements............................................. 64 Whitefield Area of New Hampshire . 35 Mafic Ammonoosuc Volcanics............................. 65 Owls Head Group of Plutons.................................... 36 Felsic Ammonoosuc Volcanics and Related Sugar Hill Pluton............................................. 36 Rocks................................................... 66 Landaff Pluton . 38 Discussion .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. 68 Moody Ledge Plutons....................................... 38 Ammonoosuc Volcanics . 68 Owls Head Dome and Pluton .. .. .. .. .. .. .. .. .. .. .. .. .. .. 39 Partial Melting Versus Fractional Crystallization............... 70 Metasomatism versus Primary Potassic Ammonoosuc Volcanics . 70 Composition........................................... 41 Oliverian Plutonic Suite . 76 Southern New Hampshire and Northern Massachu- Plate Tectonic Models......................................................... 78 setts Plutons............................................. 41 Conclusions....................................................................... 79 Baker Pond Pluton and Associated Rocks . 41 References Cited . 80 Smarts Mountain Dome and Gneiss..................... 43 Appendix: Descriptions and Locations of Analyzed Samples...... 87 ILLUSTRATIONS Page PLATE 1. Geologic setting of the Bronson Hill anticlinorium, emphasizing the Oliverian domes and the Ammonoosuc Volcanics ..... In pocket Ill IV CONTENTS Page FIGURE 1. Schematic correlation diagram showing the stratigraphy and structure of the Bronson Hill anticlinorium, New Hampshire and northern Massachusetts . 4 2. Geologic sketch map of the Berlin area of New Hampshire . 28 3-6. Photographs showing: 3. Trondhjemite associated with Ammonoosuc Volcanics, Berlin area of New Hampshire.......................................... 29 4, 5. Trondhjemite-amphibolite relationships near West Lebanon, N.H., and White River Junction; Vt., and elsewhere in western New Hampshire . 30 6. Oliverian gneiss and Ammonoosuc Volcanics in the Berlin area of New Hampshire .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. 34 7, 8. Geologic sketch maps of: 7. Sugar Hill and Landaff plutons..................................................................................................................... 37 8. Part of the Owls Head dome area . 40 9. Photographs showing contact features in the Owls Head and Lebanon plutons................................................................ 42 10. Geologic sketch map of the Smarts Mountain, Mascoma, Lebanon, and Croydon domes, west-central New Hampshire.......... 44 11. Diagram showing a hypothetical relationship involving the Ammonoosuc Volcanics, the stratified core gneiss of Naylor (1969), and the Oliverian Plutonic Suite in the Smarts Mountain and Mascoma domes .. .. .. .. .... .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. 45 12, 13. Photographs showing: 12. Aspects of the Monson Gneiss .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. 49 13. Contact relationships in the Alstead and Keene domes . 50 14-17. Harker diagrams for: 14. Jefferson batholith..................................................................................................................................... 54 15. Owls Head group of plutons......................................................................................................................... 55 16. Smarts Mountain, Mascoma, Lebanon, Croydon, and Warwick plutons .............................................................. 56 17. Monson and Swanzey Gneisses..................................................................................................................... 57 18. Peacock plots for the Smarts Mountain, Mascoma, Lebanon, Croydon, and Warwick plutons and for the Owls Head group of plutons . 58 19-22. Q-Ab-Or plots for: 19. Jefferson batholith..................................................................................................................................... 59 20. Owls Head group of plutons......................................................................................................................... 59 21. Smarts Mountain, Mascoma, Lebanon, Croydon, and Warwick plutons............................................................... 60 22. Monson and Swanzey Gneisses . .. .. 61 23. An-Ab-Or plot for all gneissic core rocks except the Unity, Alstead, and Vernon gneisses................................................ 62 24. AFM plot for all gneissic core
Recommended publications
  • Ecoregions of New England Forested Land Cover, Nutrient-Poor Frigid and Cryic Soils (Mostly Spodosols), and Numerous High-Gradient Streams and Glacial Lakes
    58. Northeastern Highlands The Northeastern Highlands ecoregion covers most of the northern and mountainous parts of New England as well as the Adirondacks in New York. It is a relatively sparsely populated region compared to adjacent regions, and is characterized by hills and mountains, a mostly Ecoregions of New England forested land cover, nutrient-poor frigid and cryic soils (mostly Spodosols), and numerous high-gradient streams and glacial lakes. Forest vegetation is somewhat transitional between the boreal regions to the north in Canada and the broadleaf deciduous forests to the south. Typical forest types include northern hardwoods (maple-beech-birch), northern hardwoods/spruce, and northeastern spruce-fir forests. Recreation, tourism, and forestry are primary land uses. Farm-to-forest conversion began in the 19th century and continues today. In spite of this trend, Ecoregions denote areas of general similarity in ecosystems and in the type, quality, and 5 level III ecoregions and 40 level IV ecoregions in the New England states and many Commission for Environmental Cooperation Working Group, 1997, Ecological regions of North America – toward a common perspective: Montreal, Commission for Environmental Cooperation, 71 p. alluvial valleys, glacial lake basins, and areas of limestone-derived soils are still farmed for dairy products, forage crops, apples, and potatoes. In addition to the timber industry, recreational homes and associated lodging and services sustain the forested regions economically, but quantity of environmental resources; they are designed to serve as a spatial framework for continue into ecologically similar parts of adjacent states or provinces. they also create development pressure that threatens to change the pastoral character of the region.
    [Show full text]
  • Official List of Public Waters
    Official List of Public Waters New Hampshire Department of Environmental Services Water Division Dam Bureau 29 Hazen Drive PO Box 95 Concord, NH 03302-0095 (603) 271-3406 https://www.des.nh.gov NH Official List of Public Waters Revision Date October 9, 2020 Robert R. Scott, Commissioner Thomas E. O’Donovan, Division Director OFFICIAL LIST OF PUBLIC WATERS Published Pursuant to RSA 271:20 II (effective June 26, 1990) IMPORTANT NOTE: Do not use this list for determining water bodies that are subject to the Comprehensive Shoreland Protection Act (CSPA). The CSPA list is available on the NHDES website. Public waters in New Hampshire are prescribed by common law as great ponds (natural waterbodies of 10 acres or more in size), public rivers and streams, and tidal waters. These common law public waters are held by the State in trust for the people of New Hampshire. The State holds the land underlying great ponds and tidal waters (including tidal rivers) in trust for the people of New Hampshire. Generally, but with some exceptions, private property owners hold title to the land underlying freshwater rivers and streams, and the State has an easement over this land for public purposes. Several New Hampshire statutes further define public waters as including artificial impoundments 10 acres or more in size, solely for the purpose of applying specific statutes. Most artificial impoundments were created by the construction of a dam, but some were created by actions such as dredging or as a result of urbanization (usually due to the effect of road crossings obstructing flow and increased runoff from the surrounding area).
    [Show full text]
  • New Hampshire River Protection and Energy Development Project Final
    ..... ~ • ••. "'-" .... - , ... =-· : ·: .• .,,./.. ,.• •.... · .. ~=·: ·~ ·:·r:. · · :_ J · :- .. · .... - • N:·E·. ·w··. .· H: ·AM·.-·. "p• . ·s;. ~:H·1· ··RE.;·.· . ·,;<::)::_) •, ·~•.'.'."'~._;...... · ..., ' ...· . , ·....... ' · .. , -. ' .., .- .. ·.~ ···•: ':.,.." ·~,.· 1:·:,//:,:: ,::, ·: :;,:. .:. /~-':. ·,_. •-': }·; >: .. :. ' ::,· ;(:·:· '5: ,:: ·>"·.:'. :- .·.. :.. ·.·.···.•. '.1.. ·.•·.·. ·.··.:.:._.._ ·..:· _, .... · -RIVER~-PR.OT-E,CT.10-N--AND . ·,,:·_.. ·•.,·• -~-.-.. :. ·. .. :: :·: .. _.. .· ·<··~-,: :-:··•:;·: ::··· ._ _;· , . ·ENER(3Y~EVELOP~.ENT.PROJ~~T. 1 .. .. .. .. i 1·· . ·. _:_. ~- FINAL REPORT··. .. : .. \j . :.> ·;' .'·' ··.·.· ·/··,. /-. '.'_\:: ..:· ..:"i•;. ·.. :-·: :···0:. ·;, - ·:··•,. ·/\·· :" ::;:·.-:'. J .. ;, . · · .. · · . ·: . Prepared by ~ . · . .-~- '·· )/i<·.(:'. '.·}, •.. --··.<. :{ .--. :o_:··.:"' .\.• .-:;: ,· :;:· ·_.:; ·< ·.<. (i'·. ;.: \ i:) ·::' .::··::i.:•.>\ I ··· ·. ··: · ..:_ · · New England ·Rtvers Center · ·. ··· r "., .f.·. ~ ..... .. ' . ~ "' .. ,:·1· ,; : ._.i ..... ... ; . .. ~- .. ·· .. -,• ~- • . .. r·· . , . : . L L 'I L t. ': ... r ........ ·.· . ---- - ,, ·· ·.·NE New England Rivers Center · !RC 3Jo,Shet ·Boston.Massachusetts 02108 - 117. 742-4134 NEW HAMPSHIRE RIVER PRO'l'ECTION J\ND ENERGY !)EVELOPMENT PBOJECT . -· . .. .. .. .. ., ,· . ' ··- .. ... : . •• ••• \ ·* ... ' ,· FINAL. REPORT February 22, 1983 New·England.Rivers Center Staff: 'l'bomas B. Arnold Drew o·. Parkin f . ..... - - . • I -1- . TABLE OF CONTENTS. ADVISORY COMMITTEE MEMBERS . ~ . • • . .. • .ii EXECUTIVE
    [Show full text]
  • PROVENANCE and TECTONIC HISTORY of METAMORPHIC ROCKS of CENTRAL PARK and NEW YORK CITY Steven J
    PROVENANCE AND TECTONIC HISTORY OF METAMORPHIC ROCKS OF CENTRAL PARK AND NEW YORK CITY Steven J. Jaret1,2, Nicholas D. Tailby1, Keiji Hammond1, E. Troy Rasbury2, Kathleen Wooton2, E. DiPadova1,3, Lisa Smith1,3, Riley Smith1,3, Victoria Yuan1,3, and Noa Jaffe1,3 1Department of Earth and Planetary Sciences, American Museum of Natural History, New York, NY. 2Department of Geosciences, Stony Brook University. 3Department of Education, New York City. The rocks underlying much of New York City, frequently referred to as the “Manhattan Prong”, predominately consist of a series of metasedimentary units, which were originally deposited into the Iapetus Ocean and subsequently deformed and metamorphosed during the Taconic, Acadian, and Alleghenian Orogenies (Merguerian and Merguerian , 2014, 2016; van Staal and Barr, 2012). Despite extensive field mapping in parks around Manhattan and subsurface mapping in major infrastructure sites (i.e., building foundations and tunnels), these rocks have not been studied geochemically and isotopically and interpretation within the larger tectonic framework has largely been based on correlation with presumed equivalent units in Connecticut and New England. Here we present new detrital zircon and Nd isotope provenance analyses in the broader geologic context of Northern Appalachia. General Background The Manhattan Schist was originally defined by Hall, 1976 and has been the subject of great debate for nearly 50 years. Merguerian 2004; 2016 has subdivided the original “Manhattan Schist” of Hall into 3 subunits of schistose rocks. He correlated the third unit with the Hartland Schist in Connecticut and thus interpreted these to be fault-bounded schists which were juxtaposed during a middle Ordovician collision between the eastern margin of Laurentia and volcanic arcs (the so-called “Taconic Arc”).
    [Show full text]
  • Partnership Opportunities for Lake-Friendly Living Service Providers NH LAKES Lakesmart Program
    Partnership Opportunities for Lake-Friendly Living Service Providers NH LAKES LakeSmart Program Only with YOUR help will New Hampshire’s lakes remain clean and healthy, now and in the future. The health of our lakes, and our enjoyment of these irreplaceable natural resources, is at risk. Polluted runoff water from the landscape is washing into our lakes, causing toxic algal blooms that make swimming in lakes unsafe. Failing septic systems and animal waste washed off the land are contributing bacteria to our lakes that can make people and pets who swim in the water sick. Toxic products used in the home, on lawns, and on roadways and driveways are also reaching our lakes, poisoning the water in some areas to the point where fish and other aquatic life cannot survive. NH LAKES has found that most property owners don’t know how their actions affect the health of lakes. We’ve also found that property owners want to do the right thing to help keep the lakes they enjoy clean and healthy and that they often need help of professional service providers like YOU! What is LakeSmart? The LakeSmart program is an education, evaluation, and recognition program that inspires property owners to live in a lake- friendly way, keeping our lakes clean and healthy. The program is free, voluntary, and non-regulatory. Through a confidential evaluation process, property owners receive tailored recommendations about how to implement lake-friendly living practices year-round in their home, on their property, and along and on the lake. Property owners have access to a directory of lake- friendly living service providers to help them adopt lake-friendly living practices.
    [Show full text]
  • Final Phase Iii Remedial Investigation Report Volume I Text and Appendices
    FINAL PHASE III REMEDIAL INVESTIGATION REPORT VOLUME I TEXT AND APPENDICES For REMEDIAL INVESTIGATION AND FEASIBILITY STUDY COLD REGIONS RESEARCH AND ENGINEERING LABORATORY (CRREL) HANOVER, NEW HAMPSHIRE Contract No.: W912WJ-11-D-0005 TASK ORDER 0004 Prepared for: New England District U.S. Army Corps of Engineers 696 Virginia Road Concord MA 01742-2751 June 29, 2018 U.S. Army Corps of Engineers - New England District Cold Regions Research and Engineering Laboratory Hanover, New Hampshire Final Phase III Remedial Investigation Report – Volume I TABLE OF CONTENTS EXECUTIVE SUMMARY ......................................................................................................................... ES-1 1.0 INTRODUCTION ............................................................................................................................ 1-1 1.1 REGULATORY STATUS ................................................................................................................... 1-1 1.2 ROLES AND RESPONSIBILITIES ....................................................................................................... 1-2 1.3 PURPOSE AND SCOPE OF THE RI REPORT ...................................................................................... 1-2 1.4 SITE BACKGROUND ....................................................................................................................... 1-3 1.4.1 Site Description (From FY 2013 CRREL Army Defense Environmental Restoration Program, Installation Action Plan, US Army Installation Command)
    [Show full text]
  • The Geology of the Saddleback Mountain Area, Northwood Quadrangle, Southeastern New Hampshire
    University of New Hampshire University of New Hampshire Scholars' Repository New England Intercollegiate Geological NEIGC Trips Excursion Collection 1-1-1984 The geology of the Saddleback Mountain Area, Northwood quadrangle, southeastern New Hampshire Whitaker, Laura R. Follow this and additional works at: https://scholars.unh.edu/neigc_trips Recommended Citation Whitaker, Laura R., "The geology of the Saddleback Mountain Area, Northwood quadrangle, southeastern New Hampshire" (1984). NEIGC Trips. 352. https://scholars.unh.edu/neigc_trips/352 This Text is brought to you for free and open access by the New England Intercollegiate Geological Excursion Collection at University of New Hampshire Scholars' Repository. It has been accepted for inclusion in NEIGC Trips by an authorized administrator of University of New Hampshire Scholars' Repository. For more information, please contact [email protected]. B6-1 207 THE GEOLOGY OF THE SADDLEBACK MOUNTAIN AREA, NORTHWOOD QUADRANGLE, SOUTHEASTERN NEW HAMPSHIRE Laura R. Whitaker Department of Geology The College of Charleston Charleston. SC 2942^ Introduction Saddleback Mountain is a four-peaked saddle-shapped mountain located 39 km west of Portsmouth, NH (Figure 1). The mountain lies along the boundary between the New England Uplands and the Seaboard Lowlands Sections of the New England Physiographic Province of Fenneman (1938). It also lies adjacent to the western boundary of the Massabesic Gneiss Complex as designated by Anderson (1978). Figure 2 of this text is a generalized Geologic Map of Southeastern New Hampshire compiled from Billings (1956) and later workers cited in the references from Figure 1. Portions of Figure 2 show that the Saddleback Mountain area is on strike with two convergent fault zones which are postulated to be of regional tectonic significance: the Nurambego of southern Maine (Hussey and Pankiwskyj, 1976; Hussey and Newberg, 1978), and the Pinnacle-Campbell-Hill-Hall Mountain Faults mapped by Camein (1976).
    [Show full text]
  • See the Wildlife Action Plan Habitat Profile
    Appendix B: Habitats Floodplain Habitats Photo by Ben Kimball Acres in NH: 23,201 Percent of NH Area: >1 Acres Protected: 7656 Percent Protected: 33 Habitat Distribution Map Habitat Description Floodplains occur in river valleys adjacent to river channels and are prone to periodic flooding. Floodplains are often comprised of forests, oxbows, meadows, and thickets. The habitats, vegetation, and hydrologic regime of floodplains are strongly influenced by watershed size, gradient, and channel morphometry. Most open or partially wooded floodplain communities occur on low floodplains. Sloughs, oxbows, vernal pools, and other depressions in the floodplain tend to be inundated for longer periods than low floodplains (Sperduto 2011). Floodplain soils range from well‐drained coarse sand on levees to poorly drained silts and mucks in depressions, and tend to be moderately to strongly minerotrophic (Sperduto 2011). Montane/near‐boreal floodplains are found primarily along rivers in the White Mountains or northern New Hampshire, and have relatively high gradients and flashy flood regimes compared to other floodplain systems. Sugar maple (Acer saccharum) and balsam fir (Abies balsamea) are dominant trees, and riparian wetlands such as oxbows and sloughs are uncommon in these high‐ gradient floodplains. Major river silver maple floodplains occur primarily along the Connecticut and Merrimack Rivers, and occasionally on lower reaches of major tributaries. These floodplains are often interspersed with oxbow marshes and shrub communities. The forested areas are characterized by a canopy of silver maple (Acer saccharinum) over a lush herbaceous layer, with a sparse shrub layer. Temperate minor river floodplains are found along large streams and small rivers in central and New Hampshire Wildlife Action Plan Appendix B-101 Appendix B: Habitats southern New Hampshire.
    [Show full text]
  • GRANIT 7.5' Quad Tile Index 1 2 3
    GRANIT 7.5' Quad Tile Index 1 2 3 1 GREELEY BROOK 108 DANBURY 4 5 6 7 2 PROSPECT HILL 109 BRISTOL PITTSBURG 3 MOOSE BOG 110 WINNISQUAM LAKE 4 METALLAK MOUNTAIN 111 LACONIA 5 COWEN HILL 112 WEST ALTON 6 SECOND CONNECTICUT LAKE 113 WOLFEBORO 8 9 10 11 7 RUMP MTN 114 SANBORNVILLE 8 PITTSBURG 115 GREAT EAST LAKE CLARKSVILLE ATKINSON & 9 LAKE FRANCIS 116 WINDSOR GILMANTON 10 MAGALLOWAY MOUNTAIN 117 CLAREMONT NORTH 11 BOSEBUCK MTN 118 GRANTHAM STEWARTSTOWN 12 13 14 15T SECOND 16 12 MONADNOCK MTN, VT-NH 119 SUNAPEE LAKE NORTH N A COLLEGE R G GRANT 13 LOVERING MOUNTAIN 120 NEW LONDON COLEBROOK S ' X DIXVILLE I 14 DIAMOND POND 121 ANDOVER D 15 MOUNT PISGAH 122 FRANKLIN 16 WILSONS MILLS 123 NORTHFIELD WENTWORTHS COLUMBIA LOCATION 17 BLOOMFIELD 124 BELMONT 17 18 1ER9VINGS 20 21 22 18 TINKERVILLE 125 GILMANTON IRON WORKS LOCATION 19 BLUE MOUNTAIN 126 ALTON MILLSFIELD ERROL 20 DIXVILLE NOTCH 127 FARMINGTON 21 ERROL 128 MILTON ODELL 22 UMBAGOG LAKE NORTH 129 SPRINGFIELD STRATFORD 23 MAIDSTONE LAKE 130 CLAREMONT SOUTH 23 24 25 26 27 28 DUMMER 24 STRATFORD 131 NEWPORT CAMBRIDGE 25 PERCY PEAKS 132 SUNAPEE LAKES D N A 26 DUMMER PONDS 133 BRADFORD L R E B 27 TEAKETTLE RIDGE 134 WARNER M STARK U H 28 UMBAGOG LAKE SOUTH 135 WEBSTER T MILAN R 29 O 30 31 32 33 29 GROVETON 136 PENACOOK N 30 STARK 137 LOUDON Y 31 WEST MILAN 138 PITTSFIELD N N E K BERLIN SUCCESS L 32 MILAN 139 PARKER MOUNTAIN I LANCASTER K 33 SUCCESS POND 140 BAXTER LAKE 34 MILES POND 141 ROCHESTER 34 35 36 37 38 39 40 35 LANCASTER W 142 SOMERSWORTH GORHAM RANDOLPH D A L T O N JEFFERSON 36 LANCASTER E 143 BELLOWS FALLS SHELBURNE 37 PLINY RANGE W 144 ALSTEAD WHITEFIELD 38 PLINY RANGE E 145 EAST LEMPSTER MARTINS 39 BERLIN 146 WASHINGTON LITTLETON CARROLL LOW & LOCATION & .
    [Show full text]
  • Preliminary Planimetric Bedrock Geologic Map of the Prescott Peninsula Equivalents
    arc- or back-arc-related tholeiitic basalts and rare andesites and metamorphosed hydrothermally altered Omo Oaf Preliminary Planimetric Bedrock Geologic Map of the Prescott Peninsula equivalents. Locally pillows, graded tuffs, agglomerates and other features are preserved even at Oaa Omos sillimanite grade. They are older than the overlying felsic member dated at 453 ±2 Ma, but the exact age Sf Omo Oaa is presently unknown. Similar rocks in northern New Hampshire (Moench and Aleinikoff, 2002; Rankin and Surroundings, Quabbin Reservoir Area, Massachusetts et al., 2007) are cut by the Joslin Turn pluton with an age of 469 ±2 Ma (late Arenig). More recent U–Pb Kempfield Oaa dating of felsic volcanics in the same area (Aleinikoff et al., 2015) suggests ages in the ranges 480–462 Omog and 458–445 Ma. U–Pb ages from 7 intrusions and 1 volcanic rock in west-central New Hampshire Anticline Geology by Peter Robinson (1959-2016) and his students, (Valley et al., 2015) were the following. The Plainfield and Lebanon tonalites, both cutting 202 Ammonoosuc Volcanics, gave 475 ±5 Ma and 466 ±8 respectively. The Sugar River granodiorite including the M.S. Thesis of Jordan Makower (1964), and intruded the Ammonoosuc at 460 ±3 Ma at the same time as extrusion of a felsic lapilli tuff at 460 ±2 Omos Ma. Wendell Bears results from his Advanced Mapping Classes, 1980-1985. Oaau: Uppermost part of the mafic lower member. Hornblende amphibolite and former coarse Syncline anthophyllite amphibolite extensively retrograded to chlorite. Some of these rocks, especially near the Den top of the unit, contain significant magnetite, and these were followed through a series of folds across Dea Oamc Dated samples (Tucker and Robinson, 1990) the channel west of Little Quabbin Island, based on a ground-magnetic survey on the ice in February Faults 1965.
    [Show full text]
  • Town of Auburn, New Hampshire Hazard Mitigation Plan Executive Summary
    TOWN OF AUBURN, NEW HAMPSHIRE Town of Auburn, New Hampshire, Town Offices HAZARD MITIGATION PLAN 2018 TOWN OF AUBURN NEW HAMPSHIRE HAZARD MITIGATION PLAN October 2018 Prepared for the Town of Auburn, NH, NH Homeland Security & Emergency Management (NHHSEM) and Federal Emergency Management Agency (FEMA) by The Southern New Hampshire Planning Commission with assistance from the Auburn Hazard Mitigation Committee October, 2018 October 22, 2018 Public Hearing Date October 22, 2018 Adoption Date Final Plan Acknowledgements Southern NH Planning Commission and the Town of Auburn wish to thank the following individuals for serving on the Town’s Hazard Mitigation Committee and for their assistance in the development of this Plan: Acknowledgements Appreciation is extended to the following people for contributing their time and effort to complete the Auburn Hazard Mitigation Plan: 2016-2018 Auburn Hazard Mitigation Committee Members Edward Gannon Fire Chief/Emergency Director, Town of Auburn, Chair Lori Collins Principal, Auburn Village School Lillian Deeb Police, Town of Auburn Mike Dross Road Agent, Town of Auburn Bill Herman Town Administrator, Town of Auburn Ray Pelton Police Chief, Town of Auburn Carrie Rouleau-Cote Building Inspector, Town of Auburn Denise Royce Planning/Land Use Administrator, Town of Auburn Jim Scalnier Fire Inspector, Town of Auburn Madeline DiIonno Southern New Hampshire Planning Commission Cameron Prolman Southern New Hampshire Planning Commission Derek Shooster Southern New Hampshire Planning Commission Zachary Swick
    [Show full text]
  • 2019 Emergency Operations Plan
    2019 Final August 14, 2019 Piermont Emergency Operations Plan 2019 THE OWNER OF THIS COPY OF THE PLAN IS: Name _____________________________________________________________________ Title ______________________________________________________________________ Plan Number_________________ Plans are worthless, but planning is everything. There is a very great distinction because when you are planning for an emergency you must start with this one thing: The very definition of "emergency" is that it is unexpected, therefore it is not going to happen the way you are planning. -Dwight D. Eisenhower Plan Prepared and Authored By June E. Garneau Mapping and Planning Solutions 105 Union Street, Suite 1 Whitefield, NH 03598 603-837-7122 [email protected] Cover Photos: Photos taken around the Town of Piermont Photos by Piermont Emergency Management Page 2 Piermont Emergency Operations Plan 2019 PIERMONT EMERGENCY OPERATIONS PLAN – 2019 General Table of Contents ACKNOWLEDGEMENTS .......................................................................................................................................... 5 CHAPTER 1 – INTRODUCTION ............................................................................................................................... 7 CHAPTER 2 – CRITICAL INFRASTRUCTURE & KEY RESOURCES AND HAZARD ANALYSIS ..................... 17 CHAPTER 3 – CONCEPT OF OPERATIONS ........................................................................................................ 27 CHAPTER 4 – ADMINISTRATIVE & FINANCE
    [Show full text]