Annotated Bibliography for the Kittatinny Ridge in Pennsylvania
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Kittatinny Valley Is the Name Given to That Part of the Great Appala Chian Valley
BULLETIN OF THE GEOLOGICAL SOCIETY OF AMERICA PALEOZOIC LIMESTONES OF KITTATINNY VALLEY, NEW J E R S E Y * BY HENRY B. KUMMEL AND STUART WELLER ( Read before the Society December 28, 1900) CONTENTS P a g e Kittatinny valley............................................................................................................... 147 Hardiston quartzite........................................................................................................... 149 Relations and character............................................................................................ 149 Previous views............................................................................................................. 151 Kittatinny limestone......................................................................................................... 151 Stratigraphic and macroscopic characters............................................................ 151 Chemical composition................................................................................................ 152 Fauna of the Kittatinny lim estone........................................................................ 152 Previous views............................................................................................................. 154 Trenton formation............................................................................................................. 154 Basal conglomerate............................................................................................................ -
Philanthropic Report Building Upon a Solid Foundation 2016
Philanthropic Report Building Upon a Solid Foundation 2016 1 www.lvcfoundation.org LVCF ANNUAL REPORT | 2016 The Lehigh Valley Community Foundation is a major philanthropic hub in the region– we know and navigate the landscape of community needs to connect people who care to causes that matter. Special thanks to LVEDC, Digital Feast, John Kish IV, Discover Lehigh Valley, and grantees for contributing photos to this report 2 LVCF ANNUAL REPORT | 2016 Table of Contents Fast Facts ............................................................ 4 Annual Letter........................................................ 5 Types of Funds..................................................... 6 George T. Walker Fund List of Funds......................................................... 7 Page 17 New Funds........................................................... 15 List of Gifts........................................................... 16 Rolland L. Adams Society..................................... 24 Joseph R. Gagnier Legacy Society...................................................... 31 Memorial Fund Page 23 List of Grants........................................................ 33 Program Highlights.............................................. 44 Financial Information........................................... 46 Kay and Marshall Wolff Board of Governors.............................................. 48 Page 30 Professional Advisors Council.............................. 49 LVCF Staff............................................................ -
A History of Lehigh County
\B7 L5H3 Class _^^ ^ 7 2- CoKiightN". ^A^ COFmiGHT DEPOSIT 1/ I \ HISTORY OF < Lehigh . County . Pennsylvania From The Earliest Settlements to The Present Time including much valuable information FOR THE USE OF THE ScDoolSt Families ana Cibrarics, BY James J. Hauser. "A! Emaus, Pknna., TIMES PURIJSHING CO. 1 901, b^V THF LIBRARY OF CONGRESS, Two Copies Recfived AUG. 31 1901 COPYBIOHT ENTRV ^LASS<^M<Xa No. COPY A/ Entered according to Die Act of Congress, in the year 1901, By JAMES J. HAUSER, In the Office of the Librarian of Congress, at Washington, D. C. All rights reserved. OMISSIONS AND ERRORS. /)n page 20, the Lehigh Valley R. R. omitted. rag6[29, Swamp not Swoiup. Page 28, Milford not Milfod. Page ol, Popnlatioii not Populatirn. Page 39, the Daily Leader of Ailentown, omitted. Page 88, Rev. .Solomon Neitz's E. name omitted. Page i)2,The second column of area of square miles should begin with Hanover township and not with Heidelberg. ^ INTRODUCTION i It is both interesting and instructive to study the history of our fathers, to ^ fully understand through what difficulties, obstacles, toils and trials they went to plant settlements wliich struggled up to a position of wealth and prosperity. y These accounts of our county have been written so as to bring before every youth and citizen of our county, on account of the growth of the population, its resources, the up building of the institution that give character and stability to the county. It has been made as concise as possible and everything which was thought to be of any value to the youth and citizen, has been presented as best as it could be under the circumstances and hope that by perusing its pages, many facts of interest can be gathered that will be of use in future years. -
To Middle Silurian) in Eastern Pennsylvania
The Shawangunk Formation (Upper OrdovicianC?) to Middle Silurian) in Eastern Pennsylvania GEOLOGICAL SURVEY PROFESSIONAL PAPER 744 Work done in cooperation with the Pennsylvania Depa rtm ent of Enviro nm ental Resources^ Bureau of Topographic and Geological Survey The Shawangunk Formation (Upper Ordovician (?) to Middle Silurian) in Eastern Pennsylvania By JACK B. EPSTEIN and ANITA G. EPSTEIN GEOLOGICAL SURVEY PROFESSIONAL PAPER 744 Work done in cooperation with the Pennsylvania Department of Environmental Resources, Bureau of Topographic and Geological Survey Statigraphy, petrography, sedimentology, and a discussion of the age of a lower Paleozoic fluvial and transitional marine clastic sequence in eastern Pennsylvania UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1972 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 74-189667 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price 65 cents (paper cover) Stock Number 2401-2098 CONTENTS Page Abstract _____________________________________________ 1 Introduction __________________________________________ 1 Shawangunk Formation ___________________________________ 1 Weiders Member __________ ________________________ 2 Minsi Member ___________________________________ 5 Lizard Creek Member _________________________________ 7 Tammany Member _______________________________-_ 12 Age of the Shawangunk Formation _______ __________-___ 14 Depositional environments and paleogeography _______________ 16 Measured sections ______________________________________ 23 References cited ________________________________________ 42 ILLUSTRATIONS Page FIGURE 1. Generalized geologic map showing outcrop belt of the Shawangunk Formation in eastern Pennsylvania and northwestern New Jersey ___________________-_ 3 2. Stratigraphic section of the Shawangunk Formation in the report area ___ 3 3-21. Photographs showing 3. Conglomerate and quartzite, Weiders Member, Lehigh Gap ____ 4 4. -
Pennsylvania
Elton 243 13A Road Ithaca Harford 36 54A 226 220 Dayton 390 14 79 11 41 80° 30’ 80° 15’ 80° 00’ 79° 45’ 79° 30’ Toll 79° 15’ 79° 00’ 78° 45’ 78° 30’Machias 78° 15’ 78° 00’ 77° 45’ 77° 30’ 77° 15’ 77° 00’ 76° 45’ 76° 30’ 76° 15’ 76° 00’ 75° 45’ 75° 30’ 75° 15’ 75° 00’ 74° 45’ 74° 30’ Houghton 53 414 5 38 21 Haskinville 327 26 A B C D E F G H J K 3 L M N 1 O P Q R S T U V W X Y Z To Buffalo East Otto Rushford Arkport Avoca 36 2 54 Hammondsport Caroline 219 Caneadea 3 96B Whitney 60 83 Hamlet South 62 243 Watkins 10 20 Cassadaga 240 98 Birdsall 10 415 37 13 79 Point 7 90 Dayton 16 2 86 35 7 Glen 3 Montour 228 THESE Bloomville Bear 322 5 Wesley Lake 41 12 TOURISM AND TRANSPORTATION28 MAP Lakes 353 242 17 79 Barcelona Lake Belfast 3 Falls Danby Center Lisle Triangle 206 Unadilla Franklin Cassadaga 6 34 329 Newfield Lisle 60 Howard Richford 11 357 Tom Wolf, Governor 1 1 2 19 Bath Townsend 224 QUICK RESPONSE 8 Greene CoventryPA Sidney PA 5 5 3 33 Hornell 38 Sonora 29 34 2 Whitney Point 41 10 Westfield Charlotte Cattaraugus Franklinville Odessa 206 Stockton 9 96 Yassmin Gramian, P.E., Secretary, Department of Transportation Center Cherry Ashford Almond 4 30 9 Creek Angelica 32 Speedsville Itaska visitPA.com41 Bainbridge visitPA.com STATE 17 7 226 Monterey 414 CODES N 394 Leon 8 42 39 5 8 88 9 Delhi Forsyth 21 86 Willseyville ROAD CLASSIFICATION AND ROUTE MARKERS KEY TO MAP SYMBOLS 61 6 New 36 3 Beaver Dams 7 20 PARKSAlbion 5 Nanticoke TRAFFIC INTERCHANGES 28 ? Hartfield 27 353 31 Alfred Savona 16 CAN BE USEDJenksville Glen 7 PASSENGER RAILROADS -
Delaware River Basin Wild and Scenic River Values
DELAWARE RIVER BASIN NATIONAL PARK SERVICE | NATIONAL WILD AND SCENIC RIVERS SYSTEM | US DEPARTMENT OF THE INTERIOR NATIONAL WILD AND SCENIC RIVER VALUES DELAWARE RIVER BASIN | NATIONAL WILD AND SCENIC RIVER VALUES DELAWARE RIVER BASIN DELAWARE | NATIONAL WILD AND SCENIC RIVER VALUES NATIONAL Photo: David B. Soete PENNSYLVANIA • NEW YORK • NEW JERSEY EXPERIENCE YOUR AMERICA NATIONAL PARK SERVICE | NATIONAL WILD AND SCENIC RIVERS SYSTEM | US DEPARTMENT OF THE INTERIOR DELAWARE RIVER BASIN CONTENTS WILD AND SCENIC RIVER VALUES PENNSYLVANIA, NEW YORK, AND NEW JERSEY Overview ....................................... 2 Lower Delaware National Wild and Scenic River ....... 48 Dear friends of the Delaware River Basin, The Wild and Scenic Rivers Act . 5 ° Cultural . 50 Outstandingly Remarkable Values . 8 ~ Lower Delaware River (including Tinicum Creek, What comes to mind when you think about the Delaware River and its tributaries? Tohickon Creek, and Paunacussing Creek) . 50 ° Cultural Values . 10 Do you think of a beautiful river valley where one can experience solitude in nature and Ecological Values . 12 ° Ecological . 51 enjoy the incredible scenery of the meandering river and forested hillsides? A family friendly ° ~ Lower Delaware River . 51 destination that provides great opportunities for boating, fi shing, and picnicking? A rare example ° Geological Values . 14 ~ Tinicum Creek . 52 of a large, undammed river that allows continual natural migration of native fi sh from the sea to ° Recreational Values . 16 the river headwaters and back? An intact network of aquatic and riparian habitat that supports Scenic Values . 17 ~ Tohickon Creek . 52 abundance and diversity of plants, fi sh, birds, and other animals? A waterway and valley with an ° ~ Paunacussing Creek . -
Delaware Water Gap
Delaware Water Gap NATIONAL RECREATION AREA PENNSYLVANIA . NEW JERSEY WHERE TO STAY Delaware Water Gap National Recreation Area, completed facilities are not yet in operation at terrace at the foot of Mount Minsi near the lower authorized by Congress in 1965, will preserve a a particular site, plan to return when you can end of the parking area, there is an unobstructed Food, lodging, gasoline, souvenirs, and other large and relatively unspoiled area astride the visit in safety and comfort. view across the river. Exhibits at the terrace ex items are available in towns and communities river boundary of Pennsylvania and New Jersey. plain how this mountain range was formed and from Port Jervis, N. Y., at the upper end of the Within easy driving range of several large metro- help you to understand rock formations visible national recreation area, to Portland, Pa., a few KITTATINNY POINT is on the New Jersey side politan areas, it will provide facilities and in the side of Mount Tammany. These million-year- miles below the proposed dam. No camping or of the Water Gap between Int. 80 and the Dela services for many types of recreational activities old rocks are constantly being changed by the picnicking facilities are available in the area ware River. A parking overlook is at the foot of and for interpretation of the area's scenic, forces of erosion. Alternate freezing and thawing this season, but they are available in nearby Mount Tammany on the opposite side of the scientific, and historical values. The forest cover of water in the crevices and plants forcing their State and private developments. -
The Nature of Boulder-Rich Deposits in the Upper Big Flat Brook Drainage, Sussex County, New Jersey
Middle States Geographer, 2009, 42: 33-43 THE NATURE OF BOULDER-RICH DEPOSITS IN THE UPPER BIG FLAT BROOK DRAINAGE, SUSSEX COUNTY, NEW JERSEY Gregory A. Pope, Andrew J. Temples, Sean I. McLearie, Joanne C. Kornoelje, and Thomas J. Glynn Department of Earth & Environmental Studies Montclair State University 1 Normal Avenue Montclair, New Jersey, 07043 ABSTRACT: The upper reaches of the Big Flat Brook drainage, northwest of Kittatinny Mountain, contain a variety of glacial, pro-glacial, and periglacial deposits from the Late Quaternary. The area is dominated by recessional moraines and ubiquitous ground moraine, along with meltwater deposits, drumlins, and possible post- glacial periglacial features. We have identified a curious boulder-rich deposit in the vicinity of Lake Ocquittunk and Lake Wapalanne on upper Big Flat Brook. The area where these boulder deposits occur is mapped (1:24,000 surficial geology) as till. As mapped and observed, larger cobbles and boulders within the till are quartz-pebble conglomerate, quartzite, sandstone, and shale. The boulder-rich deposits differ from the typical till, however. Unlike the local till, which is more mixed in lithology, the boulder deposits are nearly exclusively Shawangunk conglomerate. The deposits are discontinuous, but appear to occur at a topographic level above the meltwater stream terraces. The boulders in the deposits lie partially embedded in soil, but are very closely spaced. The boulders range in size from ~20cm to over 100cm, and present a subrounded to subangular shape. There appears to be a fabric orientation of the boulders, NE-SW, with subsidiary orientations. As the boulder deposits differ from other mapped features in the area, we attempt to ascertain the origin for the deposits. -
Nj-Tocks-Island-Nra.Pdf
TOC:K:S ISL .AN"D N ...A. TION ...A.I... R ECRE...A.TION ...A.RE...A. A Proposal I~~~~~.~~~~~i~i_i~i~~i~i~~!~~~area must come soon ~~~~(U;~.[t'~WI on-th.e dp.m ~ (ar a/ouR. for to aI/OIl' the nu:.r..e~ iJIt!f.Lilllt!rlJl::~(.ttion QHd planl1lng to IOff hchrnd tllP resen.;'rr 1j::frrJi m!lJftt.~sIi#-fn the IO::Js of this oll/slalic/lflR :W!H'tf'tmfi tat:ttit:r 8~to[!Wh8'. --:Eac7i7ifTlie biUff introduced in the COIlt;ress /0 authorize the rf!(rl!ation area states that the!lill!.!. i6' propOJM!..d...:..l.!l order 1(1 further the purpo::;es' of the 1961 Delau'ore· BlTsin ComlxlC't. They state further that the admu!.!.stratlOfL or/he Ft,!feral responsd7rhUes UH.~I! lcith tilt' p I shall be fn • ft1li ulellt"it Comrx1ci. "=T.I . , t 1(1 ecrca/UHl Rill.'! (l r(' IUO·°l'f'fcenl intUIt' -wid flu IlJNrr£:if Cimpacl as approl'ed by th-; Congrr '1 1961-' I'"m ~t"terr: nr- b) Ih'!aware HIV r B.. n l miSSion lJ('fiJrt, tht, . '01 on I Pari ~ubc mmlttee of the lIml It or nd In ular \fhllrB Sulxom nu~a States Department af thfi1 nterio T' IJ'I tt ,",unc M. %4 National Park S ervice 1965 • CONTENTS T ilE SPLEN DOR OF A 37-M1Ll:. LAKE recreation experience 1O an estimated 10 winding through the ext raordinaril y beautiful million visitors annua ll y ... and big enough Introduction to the Proposal 2 Delaware Ri ve r Valley just upstream from to preserve the natural scene for all time. -
The RPI Website 10
10 The RPI Website Jason Sodergren Abstract.—Hawkcount.org is an online database system that provides data submission, reporting, and storage services for hawk migration watchsites. Here, I outline current features of the online database system, implementation details, and plans for future system develop- ment. Hawkcount.org is an online database system that provides count and observation data entry, storage, and reporting services for migration watchsites. This system was implemented in 1999–2000 as a single-site data reporting system for the Holiday Beach Migration Observatory watchsite near Amherstburg, Ontario, Canada. This early version pro- vided functionality related to daily reporting of observed raptor counts at the site. Results were made available immediately on the Holiday Beach web site, and automated e-mail reports were submitted daily to various mailing lists, including the BIRDHAWK list maintained by the Hawk Migration Association of North America (HMANA), regional bird-related mailing lists, and others. One of the primary goals of the original system involved the simplifi - cation of the hawk counters’ daily reporting tasks, including eliminating the need to submit hard-copy daily paper forms. Each day, the counter (or other site representative) “reported” the day’s results to several places, including a hard-copy daily report form or HMANA “greensheet” to be submitted to HMANA, various e-mail lists, and the Autumn HawkWatch system, an internet-based database system that, as the result of collabora- tion among Hawk Mountain Sanctuary, the Cornell Lab of Ornithology, and the Hawk Migration Association of North America, provided a database of Hawk Migration Association of North America, P.O. -
Lower Paleozoic Carbonates: Great Valley
LOWER PALEOZOIC CARBONATES: GREAT VALLEY Frank J. Markewicz and Richard Dalton New Jersey Department of Environmental Protection, Division of Water Resources, Trenton, New Jersey INTRODUCTION The purpose of this field trip is to demonstrate the The Lower Cambrian Leithsville Formation named subdivision of the Cambro-Ordovician carbonate se by Wherry (1909) in Pennsylvania is the equivalent of quence as proposed by the field trip.leaders. In addition, the Tomstown Formation described by Miller and there will be discussions on environmental, others (1939) in eastern Pennsylvania and New Jersey, hydrogeologic, and engineering problems in these car bonates and how this subdivision has "opened the Avery Drake, (1961, 1967b) mapped the Leithsville doors" in understanding how everyday problems from Formation on the Frenchtown and Bloomsbury man's activities can affect or be affected by certain lit,hie Quadrangles and Markewicz (1967) used the term units within the carbonate sequence. This understanding Leithsville on the High Bridge Quadrangle. Wherry of the interaction between man's activities' and how it (1909) assigned a Lower-Middle Cambrian age to the lflight affect or be affected by critical aquifers, thin or Leithsville, whereas Willard (1961) infers that it is Mid thick soil horizons, and specific lithologies by septic dle Cambrian. No fossil evidence had been found to waste loads, ground water pollution, building founda establish its age until the discovery of the Lower Cam tion loading, landfills, etc'., has become extremely im-' brian fossil Hyolithellus micans in the early part of the portant in the land development process. 1960's, Markewicz (1964 unpublished), in rubbly dolomitic beds of the basal Leithsville at Califon, New We anticipate this field trip will not only relate the Jersey and also near Monroe in southern New York carbonate subdivision but will point out how important State. -
Geology of the New Tripoli Quadrangle, Lehigh, Berks, Schuylki II, and Carbon Counties, Pennsylvania
Geology of the New Tripoli Quadrangle, Lehigh, Berks, Schuylki II, and Carbon Counties, Pennsylvania U.S. GEOLOGICAL SURVEY BULLETIN 1994 Prepared in cooperation with the Pennsylvania Department of Environmental Resources, Bureau of Topographic and Geologic Survey Geology of the New Tripoli Quadrangle, Lehigh, Berks, Schuylkill, and Carbon Counties, Pennsylvania By JACK B. EPSTEIN and PETER T. LYTTLE Prepared in cooperation with the Pennsylvania Department of Environmental Resources, Bureau of Topographic and Geologic Survey Structure and stratigraphy of a complexly deformed Paleozoic sequence in the central Appalachians of Pennsylvania U.S. GEOLOGICAL SURVEY BULLETIN 1994 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, 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 UNITED STATES GOVERNMENT PRINTING OFFICE: 1993 For sale by U.S. Geological Survey, Map Distribution Box 25286, Bldg. 810, Federal Center Denver, CO 80225 Library of Congress Cataloging in Publication Data Epstein, Jack Burton, 1935- Geology of the New Tripoli quadrangle, Lehigh, Berks, Schuylkill, and Carbon counties, Pennsylvania I by Jack B. Epstein and Peter T. Lyttle. p. cm.-(U.S. Geological Survey bulletin ; 1994) "Prepared in cooperation with the Pennsylvania Department of Environmental Resources, Bureau of Topographic and Geologic Survey." Includes bibliographical references. Supt. of Docs. no.: I 19.3:1994 1. Geology-Pennsylvania.