New Jersey Local Names 1986
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Voided Certificate of Employee Information Reports
Public Contracts Equal Employment Opportunity Compliance Monitoring Program Voided Certificate of Employee Information Report Report run on: June 6, 2017 3:22 PM Name of Company Cert Street City State Zip (PC) 2 HD 37407 245 EAST 30TH NEW YORK CITY NY 10016 1515 BOARDWALK, INC 18317 121 WASHINGTON ST TOMS RIVER NJ 08753 174 NEWARK AVENUE ASSOCIATES, LP 34742 103 EISENHOWER PARKWAY ROSELAND NJ 07068 1993-N2 PROPERTIES, NO. 3 LIMITED PARTNERSHI 19621 12100 WILSHIRE BLVD LOS ANGELES CA 90025 1ST CALL PAINTING CONTRACTORS, LLC 37000 980-B DEHART PLACE ELIZABETH NJ 07202 3-2-1 QUALITY PRINTING 21779 100 JERSEY AVENUE NEW BRUNSWICK NJ 08901 3-D MFG.-DBA- AMERICAN LA-FRANCE 2831 500 S. AIRPORT ROAD SHAWANO WI 54166 4 FRONT VIDEO DESIGN INC. 22299 1500 BROADWAY #509 NEW YORK NY 10036 55 WASHINGTON STREET LLC 28132 P.O. BOX 66 CLOSTER NJ 07624 9-15 SOUTH MAIN STREET CORP. 20587 1125 ATLANTIC AVE., SUITE 617 ATLANTIC CITY NJ 08401 A & A ENGINEERING 9780 300 CORPORATE CENTER DRIVE MANALAPAN NJ 07726 A & B WIPER SUPPLY, INC. 6848 116 FOUNTAIN ST. PHILADELPHIA PA 19127 A & E CARPENTRY, INC. 8048 584 STUDIO RD. RIDGEFIELD NJ 07657 A & L UNIFORMS, L L C 37818 2605 SOUTH BROAD STREET TRENTON NJ 08610 A & P TUTORING, LLC 34701 4201 CHURCH ROAD #242 MT. LAUREL NJ 08054 A & R AUTO SUPPLY, INC. 7169 300 ATLANTIC CITY BLVD. TOMS RIVER NJ 08757 A & S FUEL OIL CO. INC. 25667 95 CALAIS ROAD PO BOX 22 IRONIA NJ 07845 A & W TECHNICAL SALES, INC. 33404 420 COMMERCE LANE, SUITE 3 WEST BERLIN NJ 08091 A AND C LABORATORIES, INC 17387 168 W. -
Saw Mill Creek in the Meadowlands Canoe Guide
Experience it all... Saw Mill Creek in the Meadowlands canoe guide The New Jersey Meadowlands Commission t Pontoon boat cruises and t Environmental remediation guided canoe tours and enhancement projects t Children’s programs, t Films, book talks, concerts and including our annual Halloween other public events Party and Spooky Walk t Grants, professional help and t School science programs other direct municipal assistance that meet NJ core curriculum to help offset property taxes standards t t Guided birding walks, Scientific research through talks and bird-banding MERI, the Meadowlands demonstrations Environmental Research Institute t The Flyway Gallery, featuring t MERI Science Library, open to the public local environmental artists The Meadowlands Experience t Meadowlands Environment t Free trail guides, birding books Center’s interactive educational and other pamphlets displays t Green building guides, t Thousands of acres preserved, assistance and existing examples eight miles of trails, 21 area parks t Public viewing nights and t Millions invested in major astronomy classes at the William flood plain management D. McDowell Observatory projects About the NJMC: The New Jersey Meadowlands Commission is the zoning and regulatory agency for the 30.4-square-mile Meadowlands District, composed of parts of 14 municipalities in Bergen and Hudson counties. Created in 1969, the NJMC has fought to end illegal dumping, encourage appropriate development, and protect the remaining open space and wetlands. The NJMC has helped preserve New Jersey thousands of acres and helped create eight miles of trails and 21 parks in the District, and also conducts Meadowlands Commission bird walks, canoe tours and popular pontoon boat One DeKorte Park Plaza • Lyndhurst, New Jersey • 07071 cruises on the Hackensack River. -
TRIP E: TACONIAN ISLANDS and the SHORES of APPALACHIA By
117 TRIP E: TACONIAN ISLANDS AND THE SHORES OF APPALACHIA By Robert M. Finks, Queens College of the City University of New York INTRODUCTION Within the Precambrian Highlands of northern New Jersey and adjacent New York are several infolded and infaulted belts of Paleozoic sediments. The easternmost of tnese belts, e the Green Pond - Schunemunk outlier; preserves Silurian and Devonian rocks as well as Cambrian and Ordovician. The mid-Paleozoic sediments lie some 25 miles farther southeast than the main outcrop belt of the miogeosyncline, and represent a sampling of material deposited approximately that much nearer the source. They provide a record of those tectonic events and geographic conditions in the source area whose influence did not spread far enough to become manifest farther west. TACONIAN ISLANDS AND RELATED MATTERS A gJance at the map (Figures 1 and 2) will show that the Silurian is in contact with the Precambrian in some places and with the Cambro-Ordovician in others. Some contacts with the Precambrian lie along the traces of high-angle faults that cut across the strike of the beds. The remaining Silurian-Precambrian contacts are parallel to the strike of the Silurian. It is possible that they are also faults, for the actual contacts are nowhere observable in the field, although outcrops are continuously exposed within a few feet of them (STOP 3). In certain places, as at the north end of Bowling Green Mountain (see Figure 1) the contact wraps around the nose of a fold and is parallel to Silurian beds of n.ther gentle dip (less than 45°). -
County Legislator Candidates Discuss Differences on Sales Tax
The Paper’s songwriters series, A Song is Born, this Saturday at 8 p.m. | Page 9 FRIDAY, OCT. 19, 2012 69 MAIN ST., COLD SPRING, N.Y. | www.philipstown.info Dunkin’ Donuts Decision Could Be Soon Planning Board schedules November meeting anticipating but not promising a decision By Kevin E. Foley onday, Nov. 5, now looms as a po- tential decision date for the Cold MSpring Planning Board’s ongo- ing consideration of the Elmesco applica- tion for the establishment of a Dunkin’ The Haldane School music room was the setting for The Paper’s forum featuring candidates Barbara Scuccimarra and Steve Donuts franchise and a convenience store Rosario. Both seek to represent the Town of Philipstown and Putnam Valley in the Putnam County Legislature. Photo by M. Turton at its Chestnut Street service station. The tentative date for the board’s next workshop was made after Joseph Bar- County Legislator Candidates Discuss Differences baro, board chair, was pressed by the Elmesco attorney Jennifer L. Van Tuyl to set a date even though the board has on Sales Tax, Butterfield, and Snake Hill Road outstanding issues with the application. Van Tuyl argued insistently that her cli- ‘Fracking’ and tree cutting also prompt questions ents deserved a sign of good faith that By Liz Schevtchuk Armstrong and entrepreneur. Sales-tax sharing the board was moving toward a deci- Rosario, an attorney and senior north- Contrasts between the candidates sion. She reminded the board that state ften agreeing about the serious- east regional director for the American quickly appeared in regard to Putnam law required a decision 62 days after the ness of the issues but not neces- Chemistry Council, a trade association, County’s refusal to share revenue from public hearing (held on Sept. -
Hackensack Meadowlands, New Jersey, Biodiversity: a Review and Synthesis
Kiviat & MacDonald, Hackensack Meadowlands Hackensack Meadowlands, New Jersey, Biodiversity: A Review and Synthesis Erik Kiviat and Kristi MacDonald Hudsonia Ltd. P.O. Box 5000, Annandale, New York 12504-5000 USA Prepared for the Hackensack Meadowlands Partnership 8 August 2002 © Hudsonia Ltd., Annandale, New York, 2002 Corrections and Updates to: Hackensack Meadowlands, New Jersey, Biodiversity: A Review and Synthesis By Erik Kiviat and Kristi MacDonald, Hudsonia Ltd. We will occasionally add information to this section of the report instead of frequently changing the report itself. This section last changed 23 June 2003 by EK. Corrections : P. 40: The laboratory work of J. Weis comparing reed and cordgrass detritus did not use mummichogs, only fiddler crabs and grass shrimp. P. 93: The correct year of publication for Labriola is 2000. Labriola should precede Langan. P. 97: The Yuhas 2001 thesis was prepared at New Jersey Institute of Technology, not Rutgers University. Table 4: American coot should be indicated (*) as water or wetland-associated; barn-owl should not be. Updates : P. 32: In July 2002, an apparent family group of northern harrier (Endangered) was observed on multiple days at the Carlstadt-Moonachie marshes (Empire tract), indicating breeding at that location. Thus the Empire tract and the Berry’s Creek marshes are the two known breeding localities for this species in the Meadowlands. P. 65: To the best of our knowledge, this clam-shrimp species is known from only about 10 localities in its global range. If this species were reviewed by the State Natural Heritage Program it would be ranked G1 S1. The Meadowlands population therefore may have considerable significance for conservation. -
Geomorphic Provinces and Sections of the New York Bight Watershed
GEOMORPHIC PROVINCES AND SECTIONS OF THE NEW YORK BIGHT WATERSHED 1. Atlantic Coastal Plain Province Sections Embayed Section New Jersey Outer Coastal Plain New Jersey Inner Coastal Plain Long Island Coastal Lowlands Barrier Beach System 2. Piedmont Province Sections Piedmont Lowlands (Northern Triassic Lowlands) 3. New England Province Sections New England Uplands New York/New Jersey Highlands (Reading Prong) Manhattan Hills (Manhattan Prong) Staten Island Sepentinite Taconic Mountains Taconic Highlands Rensselaer Plateau Stissing Mountain 4. Ridge and Valley Province Sections Great Valley Kittatinny Valley Wallkill Valley Hudson Valley Shawangunk/Kittatinny Ridge 5. Appalachian Plateaus Province Sections Glaciated Allegheny Plateau Catskill Mountains Heidelberg Mountains PHYSIOGRAPHIC SETTING Regional Geomorphology The inextricable and vital linkage between living organisms and their physical environment, or habitat, is generally well known to scientists and the public. In this report we have looked at species populations and their habitats from a broad regional perspective, focusing on large-scale physical landscape features as the basic habitat units for protection and conservation. The following general information is provided to help understand the regional physical classification units that were used as the basis for grouping and delineating regional habitat complexes. Geomorphology, or physiography, is a distinct branch of geology that deals with the nature and origin of landlords, the topographic features such as hills, plains, glacial terraces, ridges, or valleys that occur on the earth's surface. Regional geomorphology deals with the geology and associated landlords over a large regional landscape, with an emphasis on classifying and describing uniform areas of topography, relief, geology, altitude, and landlord patterns. These regions are generally referred to as GEOMORPHIC or physiographic provinces or regions and have been classified and described in various texts for the northeastern region and for the United States as a whole. -
New York and New Jersey Localities an Addendum to Moore’S Compendium of Mineral Discoveries
NEW YORK AND NEW JERSEY LOCALITIES AN ADDENDUM TO MOORE’S COMPENDIUM OF MINERAL DISCOVERIES By Hershel Friedman Founder, Minerals.net Published: January 2018 Prehnite, Lower New St., Paterson, NJ Hershel Friedman collection & photo 1 NEW YORK AND NEW JERSEY LOCALITIES An Addendum to Moore’s Compendium of Mineral Discoveries Moore’s Compendium of Mineral Discoveries is an exhaustive guide to documented mineral discoveries of minerals with crystals over one centimeter found since 1960. Completed in 2015 by Tom Moore, an editor for the Mineralogical Record and a prolific writer on mineral subjects, this is arguably the most detailed mineral book compiled in recent times. It contains two volumes, with a combined page count of 1,644 pages, describing each mineral locality in detail. There was only one publishing of this set, with only 500 copies, and there are no more plans for any additional editions to be published. Moore has stated that since the publishing, he has received much feedback and information on localities that were not included in the compendium. He stated his intention to produce a new compendium volume with the new localities of minerals not mentioned in the original compendium. Having an extensive background in the minerals of my native region of New York and New Jersey, I took the opportunity to fill in some missing gaps from my regional area. While the compendium was certainly very thorough in this region, there were still many important localities for mineral discoveries that were left out. There were also mineral discoveries in this region that were poorly documented, and require insider information from a local collector for a more thorough picture. -
The National Gazetteer of the United States of America
THE NATIONAL GAZETTEER OF THE UNITED STATES OF AMERICA NEW JERSEY 1983 THE NATIONAL GAZETTEER OF THE UNITED STATES OF AMERICA NEW JERSEY 1983 Barnegat Lighthouse took its name from adjacent Barnegat Inlet which connects Barnegat Bay with the Atlantic Ocean. The name, first appearing on a 1656 map as "Barndegat," reflects the early Dutch heritage of New Jersey. It is derived from "barende gat" meaning "foaming entrance (passage)," a descriptive reference to the break in the barrier islands with its foamy or breaking surf. The National Gazetteer of the United States of America New Jersey 1983 GEOLOGICAL SURVEY PROFESSIONAL PAPER 1200-NJ Prepared in cooperation with the U.S. Board on Geographic Names UNITED STATES GOVERNMENT PRINTING OFFICE:1983 UNITED STATES DEPARTMENT OF THE INTERIOR JAMES G. WATT, Secretary GEOLOGICAL SURVEY DALLAS L. PECK, Director UNITED STATES BOARD ON GEOGRAPHIC NAMES JOHN A. WOLTER, Chairman MEMBERS AS OF JULY 1982 Department of State ___________________________ Sandra Shaw, member Robert Smith, deputy Postal Service ________________________________ Robert G. Krause, member Paul S. Bakshi, deputy Lawrence L. Lum, deputy Department of Interior _________________________ Rupert B. Southard, member Solomon M. Lang, deputy Dwight F. Rettie, deputy David E. Meier, deputy Department of Agriculture _______________________ Myles R. Hewlett, member Lewis G. Glover, deputy Donald D. Loff, deputy Department of Commerce ______________----___- Charles E. Harrington, member Richard L. Forstall, deputy Roy G. Saltman, deputy Government Printing Office _____________________ Robert C. McArtor, member Roy W. Morton, deputy Library of Congress ____________________________ John A. Wolter, member Myrl D. Powell, deputy Department of Defense _________________________ Thomas P. Morris, member Carl Nelius, deputy Staff assistance for domestic geographic names provided by the U.S. -
9Th NYSGA Annual Meeting 1933 (6.510Mb)
,. EXCURSION OF THE NEW YORK STATE GEOLOGICAL ASSOCIATION IN THE NEW YORK C ITY REG I ON May 12th - 13th, 1933 G. MARSHALL KAY COLUMBIA UNIVERSITY (Note: Much of the region is described in Guidebqok 9, New York City and Vicinity, by c. P. Berkey, G. I. Finlay, R. J. Colony and others, to be issued by the International Geological Congress, Xvith sessiont Washington, 1933. The following guide has made use of the material in that guidebook.J INTRODUCTION Stop 1. Snake Hill is just southwest of Newburgh along State Highway 32. The locali The region to be visited in this excur ty has an outlier of resistant Pochuck gneiss sion is one including parts of several geolo that is an isolated remnant of a once-conti gical and physiographic provinces {see Figure nuous crystalline mass that was overthrust 1). The first stops are to be made adjacent northward from the Highlands upDn the Hudson to the Highlands of the Hudson, where the re River beds (see Figure 3). This overthrust sistant crystalline rocks of the Reading prong was cut later by a normal fault that tran of the New ·England Upland have been dissected sects the eastern side of the Hill and brings by the superimposed Hudson River. Northwest the Hudson River beds in contact with the of the Highlands, these crystalline rocks are older Wappinger limestone on the east. in faulted contact with the folded Paleozoic sediments of the Hudson Valley extension of the Folded Appalachians. The Catskill Moun tains farther northwest are the northern end of the Appalachian Plateau. -
GEOLOGICAL SURVEY Xf^Jlofilc/I /=B'3
DEPARTMENT OF THE INTEKIOR BULLETIN OF THE UNITED STATES GEOLOGICAL SURVEY Xf^jLOfilC/i /=b'3 67 THE RELATIONS OF THE TRAPS OF THE NEWARK SYSTEM IN THE NEW JERSEY REGION WASHINGTON GOVERNMENT PRINTING OFFICE 1890 203(222) 326 LIBRARY CATALOGUE SLIPS. - r t United States. Department of the interior. ( U. S. geological survey). Department of the interior } | Bulletin | of the | United States | geological survey | no. 67 | [Seal of the department] | Washington | government printing office | 1890 Second title: United States geological survey | J. W. Powell, director | | The relations | of the | traps of the Newark system | in the | New Jersey region | by | Nelson Horatio Darton | [Vig nette] | Washington | government printing office | 1890 8°. 82pp. 6 pi. Darton (Nelson Horatio). United States geological survey | J. W. Powell, director | | The relations | of the | traps of the Newark system | in the | New Jersey region | by | Nelson Horatio Darton | [Vignette] | Washington | government printing office | 1890 8°. 82 pp. 6 pi. [UNITED STATES. Department of the interior. (V. S. geological survey). Bulletin 67]. United States geological survey | J. W. Powell, director | | The relations | of the | traps of the Newark system | in the | New Jersey region | by | Nelson Horatio Darton | [Vignette] j Washington | government printing office | 1890 6°. 82 pp. 6 pi. (UNITED STATES. Department of the interior. (TJ. S. geological survey). Bulletin 67]. [Bulletin No. 67.] The publications of the United States Geological Survey are issued in accordance with the statute approved March 3,1879, which declares that 1 ' Thepuhlicationsof the Geological Survey shall consist of the annual report of operations, geological and economic maps illustrating the resources and classification of the lands, and reports upon general and economic geology and paleontology. -
FROM TAPPAN ZEE BRIDGE (HIGH SCHOOL): South on NY Thruway to Rte 287, Exit Elmsford, Rte 119, Turn Left at Light Onto Tarrytown Rd
Section One Directions School Directions School Office of Athletics Adam Lodewick Maureen Bassmann Updated October 2008 2 ALBERTUS MAGNUS HS ..................................................................................................................... 4 ALEXANDER HAMILTON HS ................................................................................................................ 4 ARDSLEY HS ........................................................................................................................................ 4 ARLINGTON HIGH SCHOOL ................................................................................................................ 5 BEACON HIGH ...................................................................................................................................... 5 BREWSTER HS ..................................................................................................................................... 6 BLIND BROOK HS ................................................................................................................................. 6 BRIARCLIFF HIGH/MIDDLE SCHOOL ................................................................................................. 6 BRONXVILLE SCHOOL ........................................................................................................................ 7 BYRAM HILLS HIGH SCHOOL ............................................................................................................. 9 CARMEL HS ......................................................................................................................................... -
Description of the Passaic Quadrangle
DESCRIPTION OF THE PASSAIC QUADRANGLE By N. H. Darton, W. S. Bayley, R. D. Salisbury, and H. B. Kummel. GEOGRAPHY. ing from 500 to 800 feet. This escarpment number of large tributaries which rise in the High and the north-central portion of Staten Island By N. H. DARTON. extends in a nearly straight line from Pompton to lands, of which the principal ones are Pompton exhibit metamorphic schists, of Ordovician age, Morris Plains, following a fault which lifts pre- and Rockaway rivers. The main stream enters and serpentine, and the southeastern part of the LOCATION. Cambrian rocks high above the Newark rocks. the quadrangle northwest of Plainfield, flows area is underlain by clays and sands of the Creta The Passaic quadrangle is bounded by parallels The Piedmont Plateau is very much lower and northeastward and northward for 20 miles, then ceous. Over all but the southwestern corner of 40° 30' and 41° north latitude and meridians 74° smoother than the Highlands. It consists largely eastward for 12 miles, crossing the Watchung the quadrangle is spread a mantle of drift com and 74° 30' west longitude, covering one-fourth of of wide areas of gently undulating lands having an Mountains in wide depressions, and thence flows posed of sand, clay, and bowlder deposits brought a square degree. It is approximately 35 miles in altitude of 200 to 400 feet along its western mar southward into Newark Bay, thus following a by the ice of the continental glaciers. In many length and 26 miles in width and has an area of gin and sloping down below sea level on Hudson remarkably tortuous course.