DOCSLIB.ORG

West Rocl( to the Barndoor Hills No

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
West Rocl( to the Barndoor Hills No Conn Doc G292v West Rocl( to the Barndoor Hills no. 4 cop. 3 The Traprock Ridges of Cotmecticut ... \ j " Cara Lee ( APR ~f ~/jgg0 State Geological and Natural History Survey of Connecticut Department of Environmental Protection 1985 Vegetation of Connecticut Natural Areas .No.4 I j - - - -- STATE GEOLOGICAL AND NATURAL HISTORY SURVEY OF CONNECTICUT DEPARTMENT OF ENVIRONMENTAL PROTECTION West Rocl( to the Barndoor Hills THE TRAPROCK RIDGES OF CONNECTICUT TEXT AND ILLUSTRATIONS Cara Lee Co..,., )oc 6o1Y'o.:...., /1(), y 1985 ( Oj'J. ) VEGETATION OF CONNECTICUT NATURAL AREAS NO. 4 STATE GEOLOGICAL AND ATURAL HISTORY SURVEY OF CON ECTICUT DEPARTMENT OF ENVIRONMENTAL PROTECTION Honorable William O'Neill, Governor Stanley J. Pac, Commissioner of Environmental Protection Hugo Thomas, Director, Natural Resources Center in cooperation with School of Forestry and Environmental Studies Yale University support provided by the Sperry Fund and The ature Conservancy - Connecticut Chapter Acknowledgements Many people helped me to look at traprock ridges the way they do. Their capacities range from engineering to her­ petology to geology and their generously shared enthusi­ asm, talents and skills made this project a pleasure to pursue. Thanks in particular to Ned Childs and his trusty airplane, Lauren Brown, Sue Cooley, Mike Klemens, Ken Metzler, Les Mehrhoff, Barbara arendra, Sid Quar­ rier and Steve Stanne. Diane Mayerfeld was a gracious and thoughtful editor whose help was greatly appreci­ ated. Special thanks to Tom Siccama for never failing to show interest in every aspect of the project as it evolved. This publication is one of a series describing the ecology of natural areas in Connecticut. The previous publica­ tions in this series discussed the vegetation of specific sites that were legally protected as natural areas. This report takes a broader approach. Rather than focusing in great detail on a single area, this book describes the natural history of a habitat type-traprock ridges­ which includes some protected and some unprotected areas in the state. Critical habitats such as traprock ridges are important parts of Connecticut~ natural heritage. In their natural condition, these areas are valuable for education, research, and relaxation, and as refuges for rare species and unusual biological communities. For information on how to order this report or other publications of the Connecticut and Natural History Survey, contact the Natural Resources Center in the Department of Environmental Protection. Contents I Geology 9 The Setting 9 The Sequence 12 II Ecology 20 Traprock as Critical Habitat 20 Growing on a Ridge 22 Wildlife Corridors 28 A Wilder State 33 The Green Belts 36 III Land Use 38 Quarrying the Traprock 38 Hiking, Climbing, and Sometimes Flying 43 People in High Places 48 IV Managing for Diversity 52 Appendices 57 For Further Reading 57 Other Resources 59 Topographic Maps as a Resource 60 8 I 5 LA 9 I. GEOLOGY The Setting In June ofl889, six students from the Harvard University the softer, more gently rounded hills of the surrounding Geology Department arrived in Meriden, Connecticut to valley. spend the summer. Geologists-in-training, they would The prominence of the ridges as a landscape feature in venture into the field every day with Professor William the Central Valley drew the attention of others besides M. Davis, their backpacks bulging with rock hammers, geologists in the late 18008. By the turn of the century, notebooks, compasses, maps and sample bags. Meriden the Victorian vogue for natural history study, combined was a well chosen spot for their field camp, situated in with the persistent footwork of geologists and naturalists, sight of the spectacular traprock cliffs of the Hanging resulted in a wealth of knowledge about the unique Hills and Lamentation Mountain. Hiking to prominent outcrops that they would measure and map, the young Harvard geologists learned to inter­ pret the composition and form of the geologic features that they visited. By the end of a summer of adventurous climbing, prolific note-taking and friendly arguing, they were swept into the controversy over the formation of the ridges. They too became speculators on the order and timing of prehistoric events that had given rise to the landscape of the Central Valley of Connecticut and Mas­ sachusetts. These same traprock cliffs of Central Connecticut and Massachusetts still capture the attention of all who travel in the region. Interstate 91, which runs up the Central Valley, is graced with some of the best vistas of the ridges. They rise precipitously above the valley floor and West Rock-viewed from the west, circa 1890 are fringed by steep aprons of fallen rock, distinct from (The New Haven Colony Historical Society) lO qualities of the traprock ridges. Fascination with the Sound for over 100 miles to northern Massachusetts. It ridges has continued to be reflected in the work of ranges in width from eight miles near ew Haven to 20 geologists, ecologists and landscape artists to the pres­ miles at its broadest point. The elevation of the Valley ent day. rises from sea level to 300 feet, in contrast to the Up­ A relief map of Connecticut dramatically illustrates lands, which range from 300 to 1500 feet. The trap­ that the state is divided into three major regions. The rock ridges are sharp spines of rock running the length of Western Uplands are separated from the Eastern Uplands this otherwise modestly undulating Central Valley. The by the expanse of the Central Lowlands, or Central ridges protrude from the valley floor with elevations of Valley. The Valley trends northward from Long Island 500 to almost 1000 feet. Connecticut's major physiographic provinces. , These three major , 1 areas have distinctive ' geology, soil types Ea5ter~~.- and topography. Upla~d Lowlall.d ;' 11 The Eastern and Western Uplands are underlain pre­ dominantly by hard, erosion resistant rock such as schist and gneiss. In contrast, sandstones, shales and con­ glomerates found in the Central Lowlands are soft and susceptible to erosion. The exception are the ridges of the Central Valley, which are made of durable rock that geologists call basalt and most people know as traprock. Historically, the Central Valley has been the focus of intense land use and agricultural development because of the richer, deeper and more level soils found there. The traprock ridges stand out as a dominant feature running through the Valley. They punctuate the flat expanse, interrupting continuity ofland use patterns and lending visual drama to the otherwise gentle landscape. The ridges occur in the Valley in two major belts. The major central ridge is called the Metacomet Ridge and runs from Branford past Meriden, through Hartford and north to the Holyoke Range in Massachusetts. Near Meriden, the continuity of the Metacomet Ridge is bro­ ken up, with the Hanging Hills as a bridge between the northern and southern sections. At Bluff Head, in Durham, Connecticut, the southernmost part of this ridge system abuts the Eastern Uplands. A more frag­ mented but related series of ridges lies further to the west From the "chest" of Sleeping Giant and includes West Rock in New Haven, Sleeping Giant 12 The Sequence It is not easy to imagine the sequence of geological events that created the Connecticut landscape. Interpreting these events has stirred controversy among ew England geologists for over a century. New evidence has fre­ quently necessitated the revision of theories about the geologic origins of the region. Traprock ridges are a major and highly visible part of this geological story. The sequence of events that created the present land­ scape is solidly but cryptically recorded in the bedrock geology. It is there one must look to interpret the origin of the traprock ridges. Understanding of underlying bed­ rock structure is based on information gradually ac­ Looking north toward the Barndoor Hills cumulated from naturally exposed outcrops, blasted roadcuts and quarries, tunnels, well-borings and the explorations of prospectors, fossil hunters and natu­ m Hamden and the Barndoor Hills near the Massa­ ralists. The relationship between the surface forms and chusetts border. the underlying rock strata is an imaginative three dimen­ Despite differences in their formation, the ridges in sional projection pieced together from the interpretation both belts are similar in appearance. Most of the traprock of these features. Geologists constantly revise and en­ ridges in the Central Valley have similar aspects and large this picture with new insights and observations. slopes due to large scale processes that tilted the bedrock The now widely accepted theory of plate tectonics masses in common. Their steep cliffs generally face west describes the earth's crust as large plates of bedrock and dip gently eastward from their summits. Even to the floating on the underlying molten mantle. The plates casual observer, their uniform positioning links them as a move slowly, but with great force. Over hundreds of feature in the landscape of the Central Valley. millions of years, the plates have drifted, changing size 13 Late Paleozoic era: "New England Alps" created Early Triassic period: Beginning of sedimentation by lateral compression and position. Pile-ups have occurred as one plate ground crystalline rock. By the early Triassic period, some 75 into another, forming mountain ranges. The collision of million years later, this range had lost its youthful height plates and the resulting mountain-building is currently and ruggedness to erosion. The only evidence of these in progress in the Himalayas and Andes. After colliding, mountains left today is their roots, which constitute the some plates reverse direction and pull away from each bedrock of eastern and western Connecticut. other, trying the elastic strength of the earths crust. Such Over the next 90 million years, the motion of the plates a sequence of events marked the beginning of the forma­ changed and the North American and African plates tion of current landforms in Connecticut's Central Valley.
Load more

Recommended publications
  • Consolidated School District of New Britain
    CONSOLIDATED SCHOOL DISTRICT OF NEW BRITAIN FOR IMMEDIATE RELEASE Media Contact: Helen Yung District Communications Specialist (860) 832-4382, cell (860) 877-4552 [email protected] URBAN AND SUBURBAN TEENAGERS TAKE TEAM WORK AND DIVERSITYTO NEW HEIGHTS ATOP HUBLEIN TOWER (SIMSBURY, CT)—Climbing Hublein Tower at the Talcott Mountain State Park was the least of the challenges for a group of 35 middle and high school students conducting geological field studies along the Metacomet Ridge on July 15. The students, from six school districts dispersed from New Britain to the greater Hartford area are enrolled in the Metacomet Ridge Interdistrict Academy (MRIA). The MRIA program is funded through the State Department of Education Interdistrict Cooperative Grant and managed by CREC (Capital Region Education Council), have the task of studying the environment of the Metacomet Ridge, a rocky ridge that rises above the Connecticut Valley and stretches from Long Island Sound to far above the Massachusetts/Connecticut border. According to Dr. Nalini Munshi, lead teacher at Roosevelt Middle School’s S.T.E.M Academy, the students conducted a land cover testing that includes a site of 30 by 30 meters square squares at the bottom of Talcott Mountain State Park. The students with assistance from NBHS Teachers Joe Bosco, III and Robert Ramsey feed their data into an international website for scientists known as the Globe network, where in Scientists can access it and use it for their own research. The work that the students do is considered real time science. Referring to the land cover testing, Dr. Munshi said, “we calculate the canopy cover and ground cover and measure the height of the dominant and co dominant tree species.
    [Show full text]
  • Mount Holyoke Range Planning Unit
    Massachusetts Department of Conservation and Recreation Bureau of Planning and Resource Protection Resource Management Planning Program RESOURCE MANAGEMENT PLAN Mount Holyoke Range Planning Unit Including Mount Holyoke Range State Park, Joseph Allen Skinner State Park, Mount Tom State Reservation and Holyoke Heritage State Park July 2013 Mount Holyoke Range Planning Unit Including Mount Holyoke Range State Park, Joseph Allen Skinner State Park, Mount Tom State Reservation and Holyoke Heritage State Park RESOURCE MANAGEMENT PLAN 2013 Deval L. Patrick, Governor Richard K. Sullivan, Jr., Secretary John P. Murray, Commissioner Resource Management Plans provide guidance for managing properties under the stewardship of the Department of Conservation and Recreation (DCR). They are intended to be working documents for setting priorities, enabling the Department to adapt to changing fiscal, social and environmental conditions. The planning process provides a forum for communication and cooperation with park visitors and the surrounding communities to ensure transparency in the DCR’s stewardship efforts. As I travel the Commonwealth, I am reminded of the variety of high-quality experiences offered by DCR parks. Those within the Mount Holyoke Range Planning Unit are among the best that this state has to offer. They provide a variety of recreational opportunities, from challenging hikes along mountain ridgelines, to family picnics on a promontory overlooking the Connecticut River Valley, to taking in a summer concert in downtown Holyoke. Although they may all be visited in a single day, the true character of these parks is best revealed through repeat visits. In addition to providing outstanding recreational opportunities, these parks protect important natural and cultural resources.
    [Show full text]
  • A History of Connecticut's Long Island Sound Boundary
    The Catholic University of America, Columbus School of Law CUA Law Scholarship Repository Scholarly Articles and Other Contributions Faculty Scholarship 1972 A History of Connecticut's Long Island Sound Boundary Raymond B. Marcin The Catholic University of America, Columbus School of Law Follow this and additional works at: https://scholarship.law.edu/scholar Part of the Legal History Commons Recommended Citation Raymond B. Marcin, A History of Connecticut's Long Island Sound Boundary, 46 CONN. B.J. 506 (1972). This Article is brought to you for free and open access by the Faculty Scholarship at CUA Law Scholarship Repository. It has been accepted for inclusion in Scholarly Articles and Other Contributions by an authorized administrator of CUA Law Scholarship Repository. For more information, please contact [email protected]. 506 CONNECTICUT BAR JOURNAL [Vol. 46 A HISTORY OF CONNECTICUT'S LONG ISLAND SOUND BOUNDARY By RAYMOND B. MARciN* THE SCENEt Long before remembered time, ice fields blanketed central India, discharging floes into a sea covering the Plains of Punjab. The Argentine Pampas lay frozen and still beneath a crush of ice. Ice sheets were carving their presence into the highest mountains of Hawaii and New Guinea. On the western land mass, ice gutted what was, in pre-glacial time, a stream valley near the northeastern shore. In this alien epoch, when woolly mammoth and caribou roamed the North American tundra, the ice began to melt. Receding glaciers left an inland lake where the primeval stream valley had been. For a time the waters of the lake reposed in bo- real calm, until, with the melting of the polar cap, the level of the great salt ocean rose to the level of the lake.
    [Show full text]
  • 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]
  • Ridgelines Spring 2013
    Newsletter of the West Rock Ridge Park Association Spring 2013 Regicide Drive to summit view will open to motorists on Sat., May 25! FROM THE PRESIDENT I had the pleasure of attending Friends of Connecticut State Parks Day at the state capitol on March 20th, together with Bill Doheny, past WRRPA president and current board member, and my wife, Amy. This year is the 100-year anniversary of Connecticut state parks, and there is a wonderful centennial photo display in the Legislative Office Building concourse. We spoke with representatives from 21 other volunteer groups that support our state parks, with DEEP Commissioner Dan Esty, and with our State Senator, Joseph Crisco, who has long been a strong supporter of West Rock Ridge State Park. Senator Crisco was one of the first legislators to join a new initiative supporting state parks and has “adopted” West Rock Ridge State Park; we are hopeful that our state representatives will join him in this initiative. Legislators who adopt a park agree to work with the park’s volunteer organization and with the DEEP to publicize the park and help advocate for the needs of the state park system. State parks are one of Connecticut’s most valuable natural assets. According to a 2011 UConn Economic Study, Connecticut State Parks attract over $1 billion and support over 9,000 jobs each year. Only 74 field staff are currently available to manage the 107 State Parks, and 15 of those staff are eligible for retirement in July, 2013. Because of rescissions and continued attrition, several parks will either not be opened or will have services reduced in 2013.
    [Show full text]
  • (King Philip's War), 1675-1676 Dissertation Presented in Partial
    Connecticut Unscathed: Victory in The Great Narragansett War (King Philip’s War), 1675-1676 Dissertation Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University By Major Jason W. Warren, M.A. Graduate Program in History The Ohio State University 2011 Dissertation Committee: John F. Guilmartin Jr., Advisor Alan Gallay, Kristen Gremillion Peter Mansoor, Geoffrey Parker Copyright by Jason W. Warren 2011 Abstract King Philip’s War (1675-1676) was one of the bloodiest per capita in American history. Although hostile native groups damaged much of New England, Connecticut emerged unscathed from the conflict. Connecticut’s role has been obscured by historians’ focus on the disasters in the other colonies as well as a misplaced emphasis on “King Philip,” a chief sachem of the Wampanoag groups. Although Philip formed the initial hostile coalition and served as an important leader, he was later overshadowed by other sachems of stronger native groups such as the Narragansetts. Viewing the conflict through the lens of a ‘Great Narragansett War’ brings Connecticut’s role more clearly into focus, and indeed enables a more accurate narrative for the conflict. Connecticut achieved success where other colonies failed by establishing a policy of moderation towards the native groups living within its borders. This relationship set the stage for successful military operations. Local native groups, whether allied or neutral did not assist hostile Indians, denying them the critical intelligence necessary to coordinate attacks on Connecticut towns. The English colonists convinced allied Mohegan, Pequot, and Western Niantic warriors to support their military operations, giving Connecticut forces a decisive advantage in the field.
    [Show full text]
  • News Notes Conserving the Land, Trails and Natural Resources of Connecticut Since 1895
    NEWSLETTER OF THE CONNECTICUT FOREST PARK ASSOCIATION CFPANews Notes Conserving the land, trails and natural resources of Connecticut since 1895. Winter 2008 Volume 1 Issue #2 Annual Fund Easier than Trail Mix CFPA wants you! Ever to Support Many Hands on the (to volunteer for special CFPA kicks off our 2008 Trails, Annual Awards events). Eastern Annual Fund with to Trail Managers, and Mountain Sports easier donation options tally of Trail hours. provides CFPA Club Day than ever before. Page 4-5 benefits to members. From the Executive Wedding Bells & Happy Page 5 Director’s Desk Trails brings support to CFPA’s Image Problem. CFPA. Giving options WalkCT Gains Ground Staff updates - Awards abound. New program makes and new family. Page 3 strides to connect you Page 2 with good hikes. Page 6 Conservation Center. For several years influence Connecticut’s forest resources, Partnership at after the 1964 gift, CFPA was contracted either now or in the future. Forest by the state to operate the educational landowners, foresters and loggers, scout Goodwin Center center. In 2005, after 2+ years of and other youth groups, and municipal Renewed minimal activity at the Center, we were commissioners are some key examples. instrumental in forming the “Goodwin The foundation of the Center’s On October 1, CFPA opened a new Collaborative”: a 3-way partnership educational programs is demonstration: chapter in educational partnership when on-the-ground examples of good forest we officially began directing programs and wildlife stewardship put in place at the Goodwin Forest Conservation and documented. These demonstrations Education Center in Hampton, CT.
    [Show full text]
  • Bedrock Valleys of the New England Coast As Related to Fluctuations of Sea Level
    Bedrock Valleys of the New England Coast as Related to Fluctuations of Sea Level By JOSEPH E. UPSON and CHARLES W. SPENCER SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY PROFESSIONAL PAPER 454-M Depths to bedrock in coastal valleys of New England, and nature of sedimentary Jill resulting from sea-level fluctuations in Pleistocene and Recent time UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1964 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U.S. Geological Survey Library has cataloged this publication, as follows: Upson, Joseph Edwin, 1910- Bedrock valleys of the New England coast as related to fluctuations of sea level, by Joseph E. Upson and Charles W. Spencer. Washington, U.S. Govt. Print. Off., 1964. iv, 42 p. illus., maps, diagrs., tables. 29 cm. (U.S. Geological Survey. Professional paper 454-M) Shorter contributions to general geology. Bibliography: p. 39-41. (Continued on next card) Upson, Joseph Edwin, 1910- Bedrock valleys of the New England coast as related to fluctuations of sea level. 1964. (Card 2) l.Geology, Stratigraphic Pleistocene. 2.Geology, Stratigraphic Recent. S.Geology New England. I.Spencer, Charles Winthrop, 1930-joint author. ILTitle. (Series) For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Configuration and depth of bedrock valleys, etc. Con. Page Abstract.__________________________________________ Ml Buried valleys of the Boston area. _ _______________
    [Show full text]
  • Bedrock Geologic Map of the New Milford Quadrangle, Litchfield and Fairfield Counties, Connecticut
    U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Prepared in cooperation with the State of Connecticut, Geological and Natural History Survey BEDROCK GEOLOGIC MAP OF THE NEW MILFORD QUADRANGLE, LITCHFIELD AND FAIRFIELD COUNTIES, CONNECTICUT By Gregory J. Walsh1 Open-File Report 03-487 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards (or with the North American Stratigraphic Code). 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. ______________________________________________________________________________ 1U.S. Geological Survey P.O. Box 628 Montpelier, Vermont 05601 The map and database of this report are available online at: http://pubs.usgs.gov/of/2003/of03-487/ USGS Open File Report 03-487 On the cover: Photograph of Lake Candlewood from Hubbell Hill in Sherman. View is to the south. Green Island and Deer Island are visible in the center of the view. The Vaughns Neck peninsula is visible on the left side of the photograph. Bedrock Geologic Map of the New Milford Quadrangle, Litchfield and Fairfield Counties, Connecticut 2 USGS Open File Report 03-487 TABLE OF CONTENTS INTRODUCTION .......................................................................................................................... 4 STRATIGRAPHY .......................................................................................................................... 6 MESOPROTEROZOIC GNEISS..............................................................................................
    [Show full text]
  • Environmental Review Record
    FINAL Environmental Assessment (24 CFR Part 58) Project Identification: Meriden Mills Apartments Disposition and Related Parcel Assembly Meriden, CT Map/Lots: 0106-0029-0001-0003 0106-0029-0002-0000 0106-0029-001A-0000 Responsible Entity: City of Meriden, CT Month/Year: March 2017 Meriden Mills Apartments Disposition and Related Parcel Assembly, City of Meriden, CT Environmental Assessment Determinations and Compliance Findings for HUD-assisted Projects 24 CFR Part 58 Project Information Responsible Entity: City of Meriden, CT [24 CFR 58.2(a)(7)] Certifying Officer: City Manager, Meriden, CT [24 CFR 58.2(a)(2)] Project Name: Meriden Commons Project Location: 144 Mills Street, 161 State Street, 177 State Street, 62 Cedar Street; Meriden CT. Estimated total project cost: TBD Grant Recipient: Meriden Housing Authority, Meriden CT. [24 CFR 58.2(a)(5)] Recipient Address: 22 Church Street Meriden, CT 06451 Project Representative: Robert Cappelletti Telephone Number: 203-235-0157 Conditions for Approval: (List all mitigation measures adopted by the responsible entity to eliminate or minimize adverse environmental impacts. These conditions must be included in project contracts or other relevant documents as requirements). [24 CFR 58.40(d), 40 CFR 1505.2(c)] The proposed action requires no mitigation measures. 2 4/11/2017 4/11/2017 Meriden Mills Apartments Disposition and Related Parcel Assembly, City of Meriden, CT This page intentionally left blank. 4 Meriden Mills Apartments Disposition and Related Parcel Assembly, City of Meriden, CT Statement of Purpose and Need for the Proposal: [40 CFR 1508.9(b)] This Environmental Assessment (EA) is a revision of the Final EA for Meriden Mills Apartments Disposition and Related Parcel Assembly prepared for the City of Meriden (“the City”) in October 2013.
    [Show full text]
  • Telling Guilford's Story: Report on Interpretation and Signage
    December 31, 2013 Telling Guilford’s Story Report on Interpretation and Signage Prepared for the Heritage Tourism Initiative of the Guilford Preservation Alliance Nancy I. M. Morgan, Ph.D. Point Heritage Development Consulting Jeffrey Dawson Dawson Associates Carolyn Brackett National Trust for Historic Preservation This project was made possible through generous support from the Connecticut Humanities Council and the Guilford Foundation. Contents Project Background 1 Introduction 1 Telling Guilford’s Story: Project Scope 2 Summary of Meetings 2 Elisabeth C. Adams Middle School Meeting 2 Information Kiosk Meeting 3 Historical Experts Meeting 3 Guilford Community Meeting 5 Heritage Tourism Initiative Meeting 6 Telling Guilford’s Story 8 A Thematic Framework 9 Theme 1 9 Theme 2 11 Theme 3 13 Theme 4 16 A Selected Bibliography for Telling Guilford’s Stories 19 Identifying Target Audiences for Guilford’s Heritage Tourism Experience 21 Section Overview: Identifying Target Audiences 21 Current Traveler Profile 22 Potential Target Audiences for Guilford 27 Signing Guilford 29 Site Visit 29 Survey of Existing Conditions 31 Summary of Challenges and Opportunities 41 Examples from Other Communities 43 Maps 45 Telling Guilford’s Story A Report on Interpretation and Signage Project Background Introduction Guilford is a vibrant historic community that fronts the Long Island Sound and stretches into the rolling Connecticut farmland of New Haven County. The town is blessed with a history that stretches nearly four centuries into the past, the Guilford Green and architecture that define an incredible sense of place, and forward-looking citizens who appreciate the town’s legacy and are thoughtfully building upon it.
    [Show full text]
  • AQUIFERPROTECTIONAREA SP Lainville
    d n H L Bradley Brook Beaverdam Pond Williams Pond r r R u D H r D s D t d Taine and y ell S 4 d Mountain c 7 Upl nd xw rn e Rd a a e 6 n i m M F n SV k 1 t L l or t n R s r s n o l N a Morley Elementary School R H l y Fisher Meadows gg s E N ! e L w Pi u e r H b a o b r S m d r n ld D W R e l b k D O'Larrys Ice Pond No 1 t o el c T e e r r A r o e a w a R a Ratlum Mountain Fish & Game Club Pond i t x y a Edward W Morley School u r f S r d r M t h r A 162 a d v D r l h a i i n h l r d R o v s y Charles W House u n R L C l u A o n l P l a o r Av ry l ll n e t i e d a n M M D w r n R n i e m k H L c D S e d Farmington Woods 2 H e B 4 v t o n d R R o o l a r i S i d Fisher Meadows e n a C e n l B 167 p V o M S r i l e lton St D r A A 133 F l V l r r o D u i S e C V i M n v s l l R o S e r D u v B e H b u o D y T H y A 156 A A e o q l ob n l m S e o d S i e t i e t A 162 r S n S r i o s n r n o v r d H R e l i u t s ar Av Punch Brook n r l b a h t e n r v c rm l s e e r Trout Brook R h o o D S c b n i O e a d l e R e l r v m o k l e L t A r t s d W s r i n s d r r West Hartford Reservoir No 5 a o l a R f o C d o r R tm d r e r S f i d o h i W o o i y Taine Mountain W v D e a t s n l a u t d R n i l W L e k r f v l r y A V O N Dyke Pond D D L a b r t e d W B e L l n o a r R o y t A R a n y i S g r d a r Punch Brook Ponds J n g y e i o d M a d B S d r B n a d e t a a y A s i i n b o H E r P d t G L e c r r d L r t R w il n y v d n o e f l a il H A P x r e t u e i n m nc M t l i w h B P e t e l R e r e a i S R o Norw s ! o ood Rd t d Bayberry
    [Show full text]