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Restoration Plan and Environmental Assessment for the Industri-Plex Superfund Site Town of W Oburn, Middlesex County, Massachusetts
Rest oration Plan and Environmental Asses sment for the Industri-Plex Superfund Site Draft for Public Review February 19, 2020 Prepared by: Industri-Plex NRDAR Trustee Council Commonwealth of Massachusetts U.S. Fish and Wildlife Service National Oceanic and Atmospheric Administration With support from: Abt Associates 6130 Executive Boulevard Rockville, MD 20852 Abt Associates Report Title Insert Date ▌1-1 This page intentionally left blank Industri-Plex RP/EA February 19, 2020 ▌i CONTENTS CONTENTS List of Acronyms ...................................................................................................................... iv Executive Summary ................................................................................................................. vi 1. Introduction to the Restoration Plan and Environmental Assessment ..................... 1 1.1. Trustee Responsibilities and Authorities ................................................................. 1 1.2. Summary of Industri-Plex NRDAR Settlement ........................................................ 2 1.3. Summary of Natural Resource Injuries ................................................................... 2 1.4. Purpose and Need for Restoration .......................................................................... 4 1.5. Restoration Goals ...................................................................................................4 1.6. Coordination and Scoping ....................................................................................... 4 -
Glacial Change on Baranof Island: Quantifying Local-Level Impact of Climate Change
Glacial Change on Baranof Island: Quantifying Local-level Impact of Climate Change Jonathan Kreiss-Tomkins, Chandler Kemp, Eli Bildner Overview The glaciers of Baranof Island – the only glaciated island in Southeast Alaska – are small, disparate, and sensitive to climatic change due to the temperate climate in which they are situated. We propose to quantify the change in area of a selection of Baranof Island glaciers over recent history by gathering geospatial data, calculating the perimeter and surface area of the glaciers, using a model to estimate glacial volume, and then comparing our findings against the historical record – historical USGS field measurements, historical aerial photographs, tree core data, and geomorphological indicators such as terminal moraines and trim lines. We will then quantify historical change of surface area and perimeter, and if sufficient historical data points are available, we will also calculate a rate of change (both for surface area and extent of the terminus) and predict future glacial advance or retreat. Methodology Targeted Glaciers We will gather data for two subsets of glaciers, one subset from mid-Baranof Island, one subset from the South Baranof Wilderness Area. The first subset of glaciers will consist of two glaciers from mid-Baranof Island, both on or near the Cross-Baranof Island Trail and well known by users of the Sitka Community Use Area. These glaciers are indicated in map attachment 1 – a small valley glacier north of Glacier Lake and a modest icefield north of the Baranof River valley. The second subset of glaciers will consist of three smaller hanging and cirque glaciers from the South Baranof Wilderness Area (see map attachment 2). -
Mohawk River Watershed – HUC-12
ID Number Name of Mohawk Watershed 1 Switz Kill 2 Flat Creek 3 Headwaters West Creek 4 Kayaderosseras Creek 5 Little Schoharie Creek 6 Headwaters Mohawk River 7 Headwaters Cayadutta Creek 8 Lansing Kill 9 North Creek 10 Little West Kill 11 Irish Creek 12 Auries Creek 13 Panther Creek 14 Hinckley Reservoir 15 Nowadaga Creek 16 Wheelers Creek 17 Middle Canajoharie Creek 18 Honnedaga 19 Roberts Creek 20 Headwaters Otsquago Creek 21 Mill Creek 22 Lewis Creek 23 Upper East Canada Creek 24 Shakers Creek 25 King Creek 26 Crane Creek 27 South Chuctanunda Creek 28 Middle Sprite Creek 29 Crum Creek 30 Upper Canajoharie Creek 31 Manor Kill 32 Vly Brook 33 West Kill 34 Headwaters Batavia Kill 35 Headwaters Flat Creek 36 Sterling Creek 37 Lower Ninemile Creek 38 Moyer Creek 39 Sixmile Creek 40 Cincinnati Creek 41 Reall Creek 42 Fourmile Brook 43 Poentic Kill 44 Wilsey Creek 45 Lower East Canada Creek 46 Middle Ninemile Creek 47 Gooseberry Creek 48 Mother Creek 49 Mud Creek 50 North Chuctanunda Creek 51 Wharton Hollow Creek 52 Wells Creek 53 Sandsea Kill 54 Middle East Canada Creek 55 Beaver Brook 56 Ferguson Creek 57 West Creek 58 Fort Plain 59 Ox Kill 60 Huntersfield Creek 61 Platter Kill 62 Headwaters Oriskany Creek 63 West Kill 64 Headwaters South Branch West Canada Creek 65 Fly Creek 66 Headwaters Alplaus Kill 67 Punch Kill 68 Schenevus Creek 69 Deans Creek 70 Evas Kill 71 Cripplebush Creek 72 Zimmerman Creek 73 Big Brook 74 North Creek 75 Upper Ninemile Creek 76 Yatesville Creek 77 Concklin Brook 78 Peck Lake-Caroga Creek 79 Metcalf Brook 80 Indian -
Alexander the Great's Tombolos at Tyre and Alexandria, Eastern Mediterranean ⁎ N
Available online at www.sciencedirect.com Geomorphology 100 (2008) 377–400 www.elsevier.com/locate/geomorph Alexander the Great's tombolos at Tyre and Alexandria, eastern Mediterranean ⁎ N. Marriner a, , J.P. Goiran b, C. Morhange a a CNRS CEREGE UMR 6635, Université Aix-Marseille, Europôle de l'Arbois, BP 80, 13545 Aix-en-Provence cedex 04, France b CNRS MOM Archéorient UMR 5133, 5/7 rue Raulin, 69365 Lyon cedex 07, France Received 25 July 2007; received in revised form 10 January 2008; accepted 11 January 2008 Available online 2 February 2008 Abstract Tyre and Alexandria's coastlines are today characterised by wave-dominated tombolos, peculiar sand isthmuses that link former islands to the adjacent continent. Paradoxically, despite a long history of inquiry into spit and barrier formation, understanding of the dynamics and sedimentary history of tombolos over the Holocene timescale is poor. At Tyre and Alexandria we demonstrate that these rare coastal features are the heritage of a long history of natural morphodynamic forcing and human impacts. In 332 BC, following a protracted seven-month siege of the city, Alexander the Great's engineers cleverly exploited a shallow sublittoral sand bank to seize the island fortress; Tyre's causeway served as a prototype for Alexandria's Heptastadium built a few months later. We report stratigraphic and geomorphological data from the two sand spits, proposing a chronostratigraphic model of tombolo evolution. © 2008 Elsevier B.V. All rights reserved. Keywords: Tombolo; Spit; Tyre; Alexandria; Mediterranean; Holocene 1. Introduction Courtaud, 2000; Browder and McNinch, 2006); (2) establishing a typology of shoreline salients and tombolos (Zenkovich, 1967; The term tombolo is used to define a spit of sand or shingle Sanderson and Eliot, 1996); and (3) modelling the geometrical linking an island to the adjacent coast. -
Bibliography of Alaskan Geology
BIBLIOGRAPHY OF ALASKAN GEOLOGY , ,. SPECIAL REPORT 22 ..... Compiled by: CRAWFORD E. FRITTS and MILDRED E. BROWN State of Alaska Department of Hat ural Resources OIVISIOH OF GEOLOGICAL SURVEY College, Alaska 187 1 STATE OF ALASKA William A. Egan - Governor DEPARTMENT OF NATURAL RESOURCES Charles F. Herbert - Commissioner DIVISION OF GEOLOGICAL SURVEY William C. Fackler - Assistant Commissioner for Minerals BIBLIOGWHY OF ALASKAN GEOLOGY, 1919-1949 Compiled by Crawford E. Fritrs and Mildred E. Brown College, Alaska 1971 CONTENTS Page Introduction ................................ 1 Purpose. source and format .......,............... 1 Serial publications ........................... 2 Other publishing media .........................ll Miscellaneous abbreviations ....................... 13 Bibliography ................................ 15 Index .................. Arealgeology ............. Earthquakes .............. Economic geology ........... Engineering geology .......... General subjects ........... Geomorphology [or physiography] .... Geophysical surveys .......... Glacial geology ............ Historical geology .......... Maps. geologic ............ Mineralogy .............. Paleoclimatology ........... Paleontology ............. Petrology ............... Physical geology ........... Sedimentation or sedimentary petrology Stratigraphy ............. Structural geology .......... Volcanism and volcanology ....... ILLUSTRATIONS Figure 1 . Quadrangles and major geographic divisions of Alaska referred to in this report ....................... -
Agroforestry: Enhancing Resiliency in U.S
Southeast and Caribbean Sarah Workman, Becky Barlow, and John Fike Sarah Workman is the associate director of the Highlands Biological Station, University of North Carolina; Becky Barlow is an associate professor, School of Forestry and Wildlife Sciences, Auburn University; John Fike is an associate professor, College of Agriculture and Life Sciences, Virginia Tech. Description of the Region (fig. A.15). All of these land uses provide significant produc- tivity and income. The Southeast encompasses physiographic Cropland and pastureland occupy significant portions of land provinces, or ecoregions (Wear and Greis 2012), that have area in the Southeastern United States. Forests occupy from 50 unique climate, fire history, and composition of vegetation. to 69 percent of the land within each State in the region From the physiographic province of the Appalachian Mountains Figure A.15. Acres of landuse categories of the 11 Southeastern States. (Map and table prepared by William M. Christie, Eastern Forest Environmental Threat Assessment Center, USDA Forest Service, Southern Research Station, Asheville, NC). Agroforestry: Enhancing Resiliency in U.S. Agricultural Landscapes Under Changing Conditions 189 to the alluvial plains of the Mis sissippi River Basin, within land use outside developed zones is perhaps best viewed in deciduous forests of Kentucky and Tennessee and the Interior terms of the nature of woody plant cover and whether animals Highlands of the Ozarks, to the Piedmont, Flatwoods, and are excluded or allowed access. Both Puerto Rico and the U.S. Coastal Plains, a large portion of the land area is appropriate Virgin Islands are experiencing a trend toward an increase in for implementing several types of agroforestry, integrating woody cover with the loss of agricultural land and pastureland either crops or livestock, or both, with trees and woody (Brandeis and Turner 2013a, 2013b; Brandeis et al. -
Ecoregions of Nevada Ecoregion 5 Is a Mountainous, Deeply Dissected, and Westerly Tilting Fault Block
5 . S i e r r a N e v a d a Ecoregions of Nevada Ecoregion 5 is a mountainous, deeply dissected, and westerly tilting fault block. It is largely composed of granitic rocks that are lithologically distinct from the sedimentary rocks of the Klamath Mountains (78) and the volcanic rocks of the Cascades (4). A Ecoregions denote areas of general similarity in ecosystems and in the type, quality, Vegas, Reno, and Carson City areas. Most of the state is internally drained and lies Literature Cited: high fault scarp divides the Sierra Nevada (5) from the Northern Basin and Range (80) and Central Basin and Range (13) to the 2 2 . A r i z o n a / N e w M e x i c o P l a t e a u east. Near this eastern fault scarp, the Sierra Nevada (5) reaches its highest elevations. Here, moraines, cirques, and small lakes and quantity of environmental resources. They are designed to serve as a spatial within the Great Basin; rivers in the southeast are part of the Colorado River system Bailey, R.G., Avers, P.E., King, T., and McNab, W.H., eds., 1994, Ecoregions and subregions of the Ecoregion 22 is a high dissected plateau underlain by horizontal beds of limestone, sandstone, and shale, cut by canyons, and United States (map): Washington, D.C., USFS, scale 1:7,500,000. are especially common and are products of Pleistocene alpine glaciation. Large areas are above timberline, including Mt. Whitney framework for the research, assessment, management, and monitoring of ecosystems and those in the northeast drain to the Snake River. -
Wetland Jurisdictional Determination Report
Case 10-T-0139 Hearing Exhibit 17 Page 1 of 38 WETLAND DELINEATION REPORT Champlain Hudson Power Express Project Albany, Saratoga, Schenectady, New York, Washington, and Westchester Counties, New York Prepared for: Champlain Hudson Power Express, Inc. Toronto, Ontario Prepared by: TRC ENVIRONMENTAL CORPORATION Wannalancit Mills 650 Suffolk St Lowell, MA 01854 March 2010 Case 10-T-0139 Hearing Exhibit 17 Page 2 of 38 TABLE OF CONTENTS 1.0 INTRODUCTION..............................................................................................................1 2.0 PROJECT OVERVIEW ...................................................................................................1 3.0 WETLAND DELINEATION METHODOLOGY .........................................................2 4.0 WETLAND DELINEATION RESULTS ........................................................................4 4.1 Vegetation..............................................................................................................17 4.2 Hydrology ..............................................................................................................19 4.3 Soils........................................................................................................................20 4.4 Natural Resource Conservation Service Soil Series Descriptions.........................20 5.0 REFERENCES.................................................................................................................32 TABLES Table 4-1 Summary of Wetlands Within the Study Area ........................................................5 -
Central Coast and Hawkesbury River Recreational Fishing Guide
Central Coast and Hawkesbury River Recreational Fishing Guide Fisheries Compliance Unit • fish aggregating devices (FADs) to enhance fishing for dolphinfish and even tuna and August 2020 marlin; Fishing is a fun, outdoor activity for the whole • creation of recreational fishing havens; family. Fishing rules help ensure healthy and sustainable fisheries for future generations. • angler facilities such as fish cleaning tables and fishing platforms; The Central Coast’s waterways provide excellent beach, rock, and boat fishing opportunities. This • stocking of freshwater fish in dams and rivers; guide provides essential information on fishing, • essential research on popular recreational fish including any closures and restrictions, which apply species; within the Central Coast district, extending from Munmorah State Recreation Park in the north, to • restoring important fish habitat; the southern bank of the Hawkesbury River. • marine stocking of prawns in estuaries; DPI fisheries officers routinely patrol waterways, • angler education and advisory programs such boat ramps and foreshores to advise anglers about as the Fishcare Volunteer program, fishing responsible fishing practices and to ensure workshops, Get Hooked…it's fun to fish compliance with NSW fishing regulations. primary schools education and fishing guides. Information on bag and size limits and legal fishing Much more information is available at gear can be obtained at www.dpi.nsw.gov.au/fisheries. www.dpi.nsw.gov.au/fisheries or by visiting your local DPI fisheries office. You can pay the NSW recreational fishing fee at www.onegov.nsw.gov.au or by calling 1300 369 To report suspected illegal fishing activity, call the 365 or at many outlets throughout NSW, such as Fishers Watch phone line on 1800 043 536 (free fishing tackle stores, caravan parks, local shops, call) or report on-line at service stations and many Kmart stores. -
Metro Boston Regional Climate Change Adaptation Strategy - WORKING DRAFT
Metro Boston Regional Climate Change Adaptation Strategy - WORKING DRAFT - Funding provided by the Federal Sustainable Communities Program and the Barr Foundation Revised June 2015 By: Metropolitan Area Planning Council 60 Temple Place Boston, MA 02111 617.933.0700 www.mapc.org With assistance from: Tellus Institute 11 Arlington St. Boston, MA 02116 Acknowledgements This report was originally produced in June 2014 by the Metropolitan Area Planning Council, and revised on June 1 , 2015 after discussion and approval by the MAPC Executive Committee. Technical assistance was provided by Martin Pillsbury, Environmental Director (Project Manager); Julie Conroy, Senior Environmental Planner (Primary Author); Sam Cleaves, Senior Regional Planner (Author); Bill Wang, GIS Analyst; and Barry Keppard, Public Health Division Manager; James Goldstein, Senior Fellow, Tellus Institute; and William Dougherty, President, Climate Change Research Group. Editing and continued guidance was provided by Marc Draisen, MAPC Executive Director. The Metro-Boston Regional Climate Change Adaptation Strategy (RCCAS) was undertaken with funds from the U.S. Department of Housing and Urban Development, the U.S. Environmental Protection Agency, and the U.S. Department of Transportation’s Sustainable Communities Program and the Barr Foundation. We would also like to thank the MAPC Officers for their continued support: Lynn Duncan, President; Keith Bergman, Vice President; Shirronda Almeida, Secretary; and Taber Keally, Treasurer. Special appreciation goes to the members of the RCCAS Advisory Committee for their continuous assistance and leadership: John Bolduc Environmental Planner Cambridge Community Development Dept. Wayne Castonguay Executive Director Ipswich River Watershed Assoc. Hunt Durey Acting Director MA Dept. of Ecological Restoration Kwabena Kyei-Aboagye MA Urban Program Manager U.S. -
Tatshenshini and Alsek Rivers of Alaska
ASSESSING THE RISKOF BEAR-HUMANINTERACTION AT RIVERCAMPSITES A. GRANTMacHUTCHON, 237 CurtisRoad, Comox,BC V9M3W1, Canada, email: [email protected] DEBBIEW. WELLWOOD, P.O. Box 3217, Smithers,BC VOJ2N0, Canada,email: [email protected] Abstract: The Alsek and Tatshenshinirivers of Yukon, British Columbia, and Alaska, and the Babine River, British Columbia, are seasonally importantfor grizzly bears(Ursus arctos) and Americanblack bears(Ursus americanus). Recreationaltravelers on these rivers use riparianhabitats for camping, which could lead to bear-humaninteraction and conflict. During visits in late summer 1998-99, we used 4 qualitativeindicators to assess risk of bear-humaninteraction at river campsites: (1) seasonal habitatpotential, (2) travel concerns, (3) sensory concerns, and (4) bear sign. We then rated each campsite on a 5-class scale, relative to other campsites, for the potential to displace bears and the potential for bear-human encounters. We used these ratingsto recommendhuman use of campsites with relatively low risk. Ursus 13:293-298 (2002) Key words: Alaska,American black bear, bear-human conflict, British Columbia, grizzly bear, habitat assessment, river recreation, Ursus americanus, Ursus arctos, Yukon Riparianhabitats in manyriver valleys in westernNorth 1997). The Tatshenshiniand Alsek river valleys com- America are seasonally important for grizzly bears prise a large proportionof available bear habitatwithin (Hamilton and Archibald 1986, Reinhart and Mattson the parksthrough which they flow, and the importanceof 1990, MacHutchon et al. 1993, Schoen et al. 1994, riparianhabitats to bearsis high (Simpson 1992, Herrero McCann 1998, Titusand Beier 1999) andAmerican black et al. 1993, McCann 1998). The main period of human bears (Reinhartand Mattson 1990, MacHutchonet al. use coincides with seasonalmovement of grizzly bearsto 1998, Chi and Gilbert 1999). -
Mount Mazama: Explosion Versus Collapse
Mount Mazama: Explosion versus Collapse WARREN D. SMITH, Ph.D. Professor of Geology University of Oregon CARL R. SWAR TZLOW, Ph.D. Park N aturalist Lassen National Park [Reprint from Bulletin of Geological Society of America. Vol. XLVII , December 1936. ] .. (. I I University of O regon EUGENE BULLETIN OF THE GEOLOGICAL SOCIETY OF AMERICA VOL. 47, PP. 1809-taso. 6 PLS., s FIGS. DECEMBER 31, 1936 MOUNT MAZAMA: EXPLOSION VERSUS COLLAPSE ~y WARREN D. SMITH AND CARL R. SWARTZLOW CONTENTS -Page Introduction ..................................................... •.:..... • 1809 Distribution, character, and amount of erupted material ..•.......• ·• . • . • . • . • 1812 Dillcr's "bn.ckflow" in Clcctwood Cove. • • . • . • • . • .. • . • • • . • • . .. • 1816 Shape nnd character of the crater. • . • . • . • • . • . • . • • • • . • . 1817 Absence of extruded lava of recent date. • . • • • . • . • • • • . • • . 1821 UNIVERSITY OF OREGON MONOGRAPHS· I\1nterinls of the rim . • . • • . • . • . • . • • • • • . 1822 · l\1cchanics of coJiapse. • • . • • • • . • . • • • • . 1824 Studies in Geology and Geography Records of some Pacific rim volcanoes .......•••••••... ·. • • • . • • . • • . • 1827 No; 1. February 1937 Summary and conclusions ........•.......•..•..••••.•.....•....•.•..•..•.• 1820 Published by' the University of Oregon Oregon State System of Higher ·· ILLUSTRATIONS Education, Eugene, Oregon Figure Pago I. Cross section of Crater Lake ............•••...•••••.....•••...••.••. : .. 1810 2. Pumice areas. • • • • . • . • . • . 1813 3. Section in Wheeler