Description of Franklin Furnace Quadrangle
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Stated Meeting
1893.1 SEW YORK ACADEMY OF SCIENCES. 75 single day-might, in his long experience, with every possibility be depended on. SECTIONOF ASTROXOMYAND PHYSICS. Professor REESin the chair. The secretary read a paper by Mr. Herman S. naris, Fellow in Astronomy at Col‘umbia Col- lege, entitled “ Sote on Bessel’s determination of thc relative parallaxes of p and fl Cassiopei:e.” Mr. naris had re-reduced the observations of right ascension difference of the two stars made by Bessel in the years 1814 to 1816, and printed in Engel- inanii’s “Abhandlnngen ron F. W. Ijesscl,” vol. 2, p. 215. Em- ploying the duwers, proper motions of the two stnrs and introducing into the Besselian equations a term to allow for dif- ferential proper motion, Mr. Davis arrives at the value : Parallax of p relative to t) Cassiopeiz =+0. ”02 5 Off 24. Where Bessel had obtained -- 0 “.12 5 Off .29. It will be seen that the new reduction diminishes materially the probable error of the result, in spite of the fact that the in- troduction of the proper motion term into the parallax equa- tions has lessened the weight of the determination of the parallax itself. Mr. Davis’ result is in very close though perhaps acci- dental accord with that derived from Mr. Rutherfiird’s photo- graphic measures, which was + 0” .04 (Annals N. Y. Academy, rol. viii., 11. 11). Professor William Hallock read a paper on ‘’ The Theory of Geysers,” in which he described his researches upon the geysers of the Yellowstone Park, and explained their action. -
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............................................................................................................ -
A Century of Forest Stewardship in New Jersey 1905-2005
A Century of Forest Stewardship in New Jersey 1905-2005 Researched and written by Kevin Wright © Kevin Wright 2005 An Introduction to New Jersey’s Natural Parks and Forest Reservations Tucked between blue-hazed mountains and the ocean shore, the State of New Jersey occupies a full cross section of the Atlantic slope with terrains and habitats that vary remarkably mile by mile. The cultural landscape is equally picturesque; what began as the most ethnically and religiously diverse colony has become the most densely populated State in the Union. Consequently a wonderful variety of plant and animal life competes on a daily basis with a spreading suburban population for space and resources. New Jersey’s virgin forests vanished by 1860, having been repeatedly cut over. With such widespread deforestation, even the Highlands “presented a perfectly bare appearance.” By 1900, about 46% of New Jersey’s land area, amounting to two million acres, remained woodland, though its condition was generally poor. Though this forest area was close to lumber markets, its overall value was insignificant, due mainly to repeated and uncontrolled destruction by forest fires. The first generation of professional American foresters, trained mainly in the carefully managed forest reserves of Germany, recommended the practice of scientific forestry to restore the exhausted condition of New Jersey’s remnant woodlands after centuries of exploitation. They believed that even the poor sandy soils of the Pine Barrens might yield crops of “commercially valuable trees … at a more rapid rate than is the rule on the average forest soil in the East, due to a favorable climate.”1 They not only advocated the creation of an organized firefighting force, but also a system of state-owned demonstration forests to promote reforestation. -
Sussex County Open Space and Recreation Plan.”
OPEN SPACE AND RECREATION PLAN for the County of Sussex “People and Nature Together” Compiled by Morris Land Conservancy with the Sussex County Open Space Committee September 30, 2003 County of Sussex Open Space and Recreation Plan produced by Morris Land Conservancy’s Partners for Greener Communities team: David Epstein, Executive Director Laura Szwak, Assistant Director Barbara Heskins Davis, Director of Municipal Programs Robert Sheffield, Planning Manager Tanya Nolte, Mapping Manager Sandy Urgo, Land Preservation Specialist Anne Bowman, Land Acquisition Administrator Holly Szoke, Communications Manager Letty Lisk, Office Manager Student Interns: Melissa Haupt Brian Henderson Brian Licinski Ken Sicknick Erin Siek Andrew Szwak Dolce Vieira OPEN SPACE AND RECREATION PLAN for County of Sussex “People and Nature Together” Compiled by: Morris Land Conservancy a nonprofit land trust with the County of Sussex Open Space Advisory Committee September 2003 County of Sussex Board of Chosen Freeholders Harold J. Wirths, Director Joann D’Angeli, Deputy Director Gary R. Chiusano, Member Glen Vetrano, Member Susan M. Zellman, Member County of Sussex Open Space Advisory Committee Austin Carew, Chairperson Glen Vetrano, Freeholder Liaison Ray Bonker Louis Cherepy Libby Herland William Hookway Tom Meyer Barbara Rosko Eric Snyder Donna Traylor Acknowledgements Morris Land Conservancy would like to acknowledge the following individuals and organizations for their help in providing information, guidance, research and mapping materials for the County of -
Wallkill River National Wildlife Refuge Comprehensive Conservation Plan February 2009 This Blue Goose, Designed by J.N
U.S. Fish & Wildlife Service Wallkill River National Wildlife Refuge Comprehensive Conservation Plan February 2009 This blue goose, designed by J.N. “Ding” Darling, has become the symbol of the National Wildlife Refuge System. The U.S. Fish and Wildlife Service is the principal federal agency responsible for conserving, protecting, and enhancing fi sh, wildlife, plants, and their habitats for the continuing benefi t of the American people. The Service manages the 97-million acre National Wildlife Refuge System comprised of more than 548 national wildlife refuges and thousands of waterfowl production areas. It also operates 69 national fi sh hatcheries and 81 ecological services fi eld stations. The agency enforces federal wildlife laws, manages migratory bird populations, restores nationally signifi cant fi sheries, conserves and restores wildlife habitat such as wetlands, administers the Endangered Species Act, and helps foreign governments with their conservation efforts. It also oversees the Federal Assistance Program which distributes hundreds of millions of dollars in excise taxes on fi shing and hunting equipment to state wildlife agencies. Comprehensive Conservation Plans provide long term guidance for management decisions and set forth goals, objectives, and strategies needed to accomplish refuge purposes and identify the Service’s best estimate of future needs. These plans detail program planning levels that are sometimes substantially above current budget allocations and, as such, are primarily for Service strategic planning and program prioritization purposes. The plans do not constitute a commitment for staffi ng increases, operational and maintenance increases, or funding for future land acquisition. U.S. Fish & Wildlife Service Wallkill River National Wildlife Refuge Comprehensive Conservation Plan February 2009 Submitted by: Edward Henry Date Refuge Manager Wallkill River National Wildlife Refuge Concurrence by: Janet M. -
Inrnorucrron the Mineral Roeblingite Has Been Reported from Two
MINERALOGICAL NOTES THE AMERICAN MINERALOGIST, VOL. 51, MARCH_APRIL' 1966 NEW DATA ON ROEBLINGITE1 FnaxrrrN F. Forr, !n., Department of Geology and Mineralogy, The IJniaersity of Michigan, Ann Arbor, Michigan- INrnorucrroN The mineral roeblingite has been reported from two Iocalities: Franklin was Furnace,New Jersey,and Langban, Sweden.The Franklin material frrst describedby Penfield and Foote (1897) as dense,white, compact massesof minute prismatic crystals associatedwith axinite, willemite, datolite, barite, arsenopyrite,sphalerite, titanite, rhodonite and rhodo- chrosite,in or near the limestone-granitecontact. During an extensive mineralogical investigation of the Langban mineralsinitiated in the late 1920'sby G. Aminoff of the Natural History Museum, Stockholm, Sweden, a mineral similar in composition to roeblingite was discovered. A complete investigation of this new dis- covery demanded more reliable chemical data than was offered by Penfieldand Foote.Therefore, R. Blix (1931)performed several chemical analyseson the Franklin roeblingite in an effort to remedy the difficulty encounteredby Penfield and Foote in assigninga chemical formula. The chemical analyses from both sources are tabulated in Table I. Strunz (1957) reports the Langban roeblingite as possibly being orthorhombic with o:8.3, b:13.1, and c:12'65 A. Ho*evet' some difficulty is en- countered in obtaining a reasonable formula from the application of theseparameters to the available chemical analyses. X-nav ANar-vsrs A specimenfrom each of the localities was investigated by both powder diffraction and single crystal methods. This investigation confirmed that roeblingite found at Langban is structurally identical to the Franklin material. A list of indexed d-values for roeblingite is presented in Table II. -
HEDYPHANE from FRANKLIN FURNACE, NEW JERSEY Wu. F
JOURNAL MINERALOGICALSOCIETY OF AMERICA 351 Missouri, of the U. S. Geological Survev. Starting out from Ilarrison, the main road running southwestward (in 1925 not completed, but ultimately to extend to Fort Smith) is followed' About 25 kilometers (16 miles) frorn Harrison the tiny settlement of Compton is passed,recognized by the right-angled turn of the road from south to west;and 6.5 km. (4 m.) further west,where the road swingssouthward, one's auto must be parked and the journey continued on foot. An indistinct road, used to haul out timber, extendseast from the main road down into the gorge of Sneed'sCreek (which rises somewhat further west than shown on the map) and this is to be followed about 200 meters, to a point where the slope becomes very steep. Then, on scrambling down the hillside perhaps 100 meters,a group of small prospectpits will be more or lessplainly seen. These have long since fallen shut, and good sized trees are growing on the dumps, but the light color of many of the frag- ments renders them rather conspicuous against the brown forest soil. On digging into the mass of decomposedshale-a pickaxe and spade will be found useful-occasional small lumps of a soft, white, chalky material, more or less stained by iron oxides, are encountered;and this is the newtonite. Under the microscopeit is seen to be made up of minute grains of nearly,squareoutline, which have been variously interpreted as rhombs or as tetragonal bipyramids, but which, it is hoped, can now be further studied. -
The Picking Table Volume 50, No. 2 – Fall 2009
2009FallPT:Layout 1 8/27/2009 10:21 AM Page 1 JOURNAL OF THE FRANKLIN-OGDENSBURG MINERALOGICAL SOCIETY Volume 50, No. 2 – Fall 2009 $20.00 U.S. SPECIAL EDITION TH 50 ANNIVERSARY The contents of The Picking Table are licensed under a Creative Commons Attribution-NonCommercial 4.0 International License. 2009FallPT:Layout 1 8/27/2009 10:21 AM Page 2 The Franklin-Ogdensburg Mineralogical Society, Inc. OFFICERS and STAFF 2009 PRESIDENT SLIDE COLLECTION CUSTODIAN Bill Truran Edward H. Wilk 2 Little Tarn Court, Hamburg, NJ 07419 202 Boiling Springs Avenue (973) 827-7804 E. Rutherford, NJ 07073 [email protected] (201) 438-8471 VICE-PRESIDENT TRUSTEES Richard Keller C. Richard Bieling (2009-2010) 13 Green Street, Franklin, NJ 07416 Richard C. Bostwick (2009-2010) (973) 209-4178 George Elling (2008-2009) [email protected] Steven M. Kuitems (2009-2010) Chester S. Lemanski, Jr. (2008-2009) SECOND VICE-PRESIDENT Lee Lowell (2008-2009) Joe Kaiser Earl Verbeek (2008-2009) 40 Castlewood Trail, Sparta, NJ 07871 Edward H. Wilk (2008-2009) (973) 729-0215 Fred Young (2008-2009) [email protected] LIAISON WITH THE EASTERN FEDERATION SECRETARY OF MINERALOGICAL AND LAPIDARY Tema J. Hecht SOCIETIES (EFMLS) 600 West 111TH Street, Apt. 11B Delegate Joe Kaiser New York, NY 10025 Alternate Richard C. Bostwick (212) 749-5817 (Home) (917) 903-4687 (Cell) COMMITTEE CHAIRPERSONS [email protected] Auditing William J. Trost Field Trip Warren Cummings TREASURER Historical John L. Baum Denise Kroth Mineral Exchange Richard C. Bostwick 240 Union Avenue Nominating William Kroth Wood-Ridge, NJ 07075 Program Fred Young (201) 933-3029 Swap & Sell Chester S. -
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. -
Environmentally Sensitive Areas Guidance Document
New Jersey Department of Environmental Protection Bureau of Release Prevention ENVIRONMENTALLY SENSITIVE AREAS GUIDANCE DOCUMENT Revised September 2014 Introduction This guidance on environmentally sensitive areas is intended for use as a reference and a guide when gathering information to be used in preparing the topographical maps for Discharge Prevention, Containment and Countermeasure (DPCC), and Discharge Cleanup and Removal (DCR) Plans. It gathers in one place all the citations listed in N.J.A.C. 7:1E-1.8, which establishes the definition of environmentally sensitive areas (ESA) for the purpose of developing the DPCC/DCR plan. The areas described in this document are by no means the only ESA in New Jersey, but represent those most likely to be adversely affected by a discharge of a hazardous substance. When used in conjunction with the requirements of N.J.A.C. 7:1E-4.10, Mapping criteria, it will prove useful in preparing the topographical maps and the offsite response measures that are required as part of the DCR plan. Additional information concerning the certification of ESA information is available in A Guide to the Preparation of Discharge Prevention, Containment and Countermeasure (DPCC) and Discharge Cleanup and Removal (DCR) Plans and Plan Renewals, available on the Bureau of Release Prevention website at http://www.nj.gov/dep/rpp/brp/dp/index.htm. N.J.A.C. 7:1E-4.2(b)9 requires that topographical maps be included in the DPCC plan, while N.J.A.C. 7:1E-4.10(d) requires that these maps cover all surrounding areas which could be affected by a discharge from the facility, including ESA. -
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.