Selected Bibliography of the Geology and Ore Deposits of the Shawangunk Mountain Region, New York, and Related Topics Compiled by Jules D
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Natural Cement Industry at Rosendale, Ulster County, New York
Journal of ASTM International, Vol. 4, No. 6 Paper ID JAI100672 Available online at www.astm.org Dietrich Werner1 and Kurtis C. Burmeister2 An Overview of the History and Economic Geology of the Natural Cement Industry at Rosendale, Ulster County, New York ABSTRACT: The Rosendale region of southeastern New York State is widely recognized as the source of the highest quality natural cement in North America. The North American natural cement industry was founded in 1819 by Canvass White in central New York, but soon shifted to Rosendale where it flourished for over 150 years. By the end of the 19th century, the superior quality of Rosen- dale cement was known worldwide and was actively used in the construction of some of America’s most enduring landmarks. Rosendale natural cement’s reputation stems from the unique composi- tion of the clay-rich layers of dolostone in the Upper Silurian Rondout Formation from which it is manufactured. Miners utilized room-and-pillar techniques to extract this dolostone from strongly deformed strata in the Rosendale region, creating unique bedrock exposures in mines that are something of an engineering marvel. The exposures resulting from these mining activities have long attracted the attention of geologists for research and education. Production of natural cement trans- formed extracted dolostone into barrels of cement through a labor-intensive process involving calci- nation in kilns, cracking, and grinding. Barrels of cement produced were quickly shipped at competi- tive prices via the Delaware and Hudson Canal, which directly connected the Rosendale natural cement region to major shipping avenues. KEYWORDS: natural cement, Canvass White, Delaware and Hudson canal, cement production, geology, education, Rosendale, Ulster County, New York Introduction The momentum of the North American Industrial Revolution in the opening years of the 19th century sparked a number of large-scale building projects, including the construction of regional canal net- works. -
A Long-Term Prehistoric Occupation in the Hudson Valley
City University of New York (CUNY) CUNY Academic Works School of Arts & Sciences Theses Hunter College Spring 4-23-2018 The Roscoe Perry House Site: A Long-Term Prehistoric Occupation in the Hudson Valley Dylan C. Lewis CUNY Hunter College How does access to this work benefit ou?y Let us know! More information about this work at: https://academicworks.cuny.edu/hc_sas_etds/339 Discover additional works at: https://academicworks.cuny.edu This work is made publicly available by the City University of New York (CUNY). Contact: [email protected] The Roscoe Perry House Site: A Long-Term Prehistoric Occupation in the Hudson Valley by Dylan C. F. Lewis Submitted in partial fulfillment of the requirements for the degree of Master of Arts in Anthropology, Hunter College The City University of New York 2018 Thesis Sponsor: April 23, 2018 Dr. William J Parry Date Signature April 23, 2018 Dr. Joseph Diamond Date Signature of Second Reader Acknowledgments: I would like to thank Dr. Joseph Diamond for providing me with a well excavated and informative archaeological collection from the SUNY New Paltz Collection. Without which I would have been unable to conduct research in the Hudson Valley. I would like to thank Dr. William Parry for so generously taking me on as a graduate student. His expertise in lithics has been invaluable. Thank you Glen Kolyer for centering me and helping me sort through the chaos of a large collection. Frank Spada generously gave his time to help sort through the debitage. Lastly, I would like to thank my wife to be for supporting me through the entire process. -
And Eastern Pennsylvania
GEOLOGY OF THE RIDGE AND VALLEY PROVINCE, NORTHWESTERN NEW JERSEY AND EASTERN PENNSYLVANIA JACK B. EPSTEIN U. S. Geological Survey, Reston, Va. 22092 INTRODUCTION The rocks seen in this segment of the field trip range A general transgressive-shelf sequence followed in age from Middle Ordovician to Middle Devonian and characterized mainly by tidal sediments and barrier bars constitute a.deep basin-continental-shallow shelf succes (Poxono Island, Bossardville, Decker, Rondout)~ suc sion. Within this succession, three lithotectonic units, or ceeded by generally subtidal and bar deposits (Helder sequences of rock that were deformed semi burg and Oriskany Groups), and then by deeper sub independently of each other, have somewhat different tidal deposits (Esopus, . Schoharie. and Buttermilk structural characteristics. Both the Alleghenian and Falls), finally giving way to another deep~water to Taconic orogenies have left their imprint on the rocks. shoaling sequence (Marcellus Shale through the Catskill Wind and water gaps are structurally controlled, thus Formation). Rocks of the Marcellus through Catskill placing doubt upon the hypothesis of regional super will not be seen on this trip. position. Wisconsinan deposits and erosion effects are common. We will examine these geologic features as This vertical stratigraphic sequence is complicated a well as some of the economic deposits in the area. bit because most Upper Silurian and Lower Devonian units are much thinner or are absent toward a paleo Figure 1 is an index map of the field-trip area, show positive area a few tens of miles southwest of the field ing the trip route and quadrangle coverage. Figure 2 is a trip area. -
How the Gap Formed
Delaware Water Gap National Recreation Area How the Gap formed What is a water gap? Several words in the English language The Delaware Water Gap is justly famous for denote a “break” or “cleft” in the moun- its depth, width, and scenic beauty. The Gap tains. Chasm and notch are popular in New is a mile wide from New Jersey’s Mount England; pass and gorge in the South and Tammany (1,527 feet) to Pennsylvania’s West of the United States. Gap is especially Mount Minsi (1,463 feet.) The Gap is about common in this part of the country. 1,200 feet deep from the tops of these mountains to the surface of the river, which A gap or wind gap is a break or pass through at this point is 290 feet above sea level. The the mountains, in this case the Appalachian maximum depth of the river at the Gap is Mountains. A water gap is a pass that a river about 55 feet. runs through. How does a gap form? Geology is the study of the earth’s forma- Starting with Native American legend, there tion. Though the geologist’s time frame may have been many ideas about how the seem vast and remote, the results of Delaware Water Gap formed. One current geological processes are the mountains we theory explains the Gap through a series of hike on, the river we swim in, and the processes: continental shift (involving plate scenery we admire. tectonics), mountain building (orogeny), erosion, and the “capturing” of rivers and streams. -
Changes in Stratigraphic Nomenclature by the U.S. Geological Survey, 1972
Changes in Stratigraphic Nomenclature by the U.S. Geological Survey, 1972 GEOLOGICAL SURVEY BULLETIN 1394-A I*3P Changes in Stratigraphic Nomenclature by the U.S. Geological Survey, 1972 By GEORGE V. COHEE and WILNA B. WRIGHT CONTRIBUTIONS TO STRATIGRAPHY GEOLOGICAL SURVEY BULLETIN 1394-A UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1974 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 73-600312 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Price $1.00 (paper cover) Stock Number 2401-02450 CONTENTS Page Listing of nomenclatural changes _ _ Al Big Dome Formation and revised Tertiary stratigraphy in the Ray- San Manuel area, Arizona, by Medora H. Krieger, Henry R. Corn wall, and Norman G. Banks ______________________________ 54 Big Dome Formation ___________________________ 58 Relation to other formations __ _ ____ 61 Problems in correlating the San Manuel Formation and Whitetail Conglomerate _____ __ ____ _____________ 62 Knifley Sandstone and Cane Valley Limestone: Two new members of the Fort Payne Formation (Lower Mississippian) in south-central Kentucky, by Roy C. Kepferle and Richard Q. Lewis, Sr _____ 63 Measured sections ___________________________ 68 Metadiabase sills in Negaunee Iron-formation near National Mine, Mich., by George C. Simmons ___________________ 70 Tilden Lake sill ______________________________ 71 National Mine sill _____________________________ 71 Ash-flow stratigraphy and caldera structures in the San Juan volcanic field, southwestern Colorado, by T. A. Steven, P. W. Lipman, and J. C. Olson ___________________________________ 75 Fish Canyon (and La Garita) Tuff __________________ 77 Carpenter Ridge (and Bachelor Mountain) Tuff ___________ 78 Rat Creek and Nelson Mountain Tuffs ________________ 80 Bull Ridge Member of Mission Canyon Limestone, Beartooth Moun tains, southern Montana, by William J. -
Taking Flight / New York State Ornithological Association Annual Conference Hosted by the Catskill Center Kingston, NY September 13‐15, 2019
Taking Flight / New York State Ornithological Association Annual Conference Hosted by the Catskill Center Kingston, NY September 13‐15, 2019 Two ways to register: 1) Register and Pay with credit card online at: www.catskillcenter.org/takingflight/registration 2) Mail this completed form and payment: Catskill Center, c/o Katie Palm, PO Box 504, Arkville, NY Registrant #1 Name ____________________________________________________________________ Address________________________________ City___________________State________ Zip________ Phone(______)__________________________ Email_________________________________________ Delegate? Yes ______ No ______ Name of Club_____________________________________________ Registrant #2 Name ____________________________________________________________________ Address________________________________ City___________________State________ Zip________ Phone(______)__________________________ Email_________________________________________ Delegate? Yes ______ No ______ Name of Club_____________________________________________ Per Qty Person Total Registration postmarked by $55 August 2, 2019 Mail completed form and Registration postmarked after payment to: $65 August 2, 2019 Catskill Center Student registration fee $35 C/O Katie Palm PO Box 504 Saturday evening Banquet‐ buffet** $55 Arkville, NY 12406 Friday evening Hudson River Birding [email protected] $40 Cruise (845) 586‐2611 Snack for Saturday morning hike (fruit, $10 drink, granola bar, hiking snacks) ** * Checks payable to: Snack for Sunday morning -
Hiking Dix Mountain
FREE! COVERING SEPTEMBER UPSTATE NY 2016 SINCE 2000 Hiking Dix Mountain CONTENTS A Scenic Trail with 1 Hiking & Backpacking Dix Mountain Expansive Lookouts 3 Running & Walking By Bill Ingersoll Leaves, Pumpkins & ▲ HIKERS REACHING THE DIX his trail is arguably the most scenic approach to Dix By all means, make the short SUMMIT ARE REWARDED WITH Fall Classics THIS PERFECT VIEW OF GOTHICS. Mountain, the sixth highest peak in the High Peaks. Although side trip if you have the time. BILL INGERSOLL 5 News Briefs T it is nearly seven miles long, there are several attractive If you are planning to linger, landmarks to enjoy along the way: Round Pond, the North Fork 5 From the Publisher & Editor note that Round Pond has been stocked with brook trout. Boquet and its lean-to, and the brief traverse of Dix’s northern The main trail bears right at the junction and circles through 6-9 CALENDAR OF EVENTS slide. Although Bob Marshall and other hikers in the 1920s found the birch forest to Round’s northern shore. Of all the Round September to cause for complaint in the condition of the trail after the twin fires Ponds in the Adirondack Park, this is one of the few in which November Events of 1903 and 1913, many of those sins have been erased by the pas- the name is almost geometrically appropriate. The trail passes sage of time. The one fault that remains is the steepness that exists close around the shore, with numerous opportunities to enjoy 11 Bicycling on the uppermost portion of the trail, above the slide. -
John Burroughs Black Creek Trail Plan
N Eltings Rd d R rs e n r o C LILLY s LAKE ley aw 15 H Tony WIlliams Swartekill Rd 16 B la ck Town Park Loughran Ln C re e k Martin Ave d R e d i s r P e O U v Chodikee Lake S i S R E Illinois S Boat Launch Chodik e R Mountain 12 N ee Lak d New Paltz Rd d CHODIKEE t R er J LAKE k Blacka Creek Canoe c n A e Valli Rd d H W y Berean &o Kayak Launch H o o le l d l i d i k F d R Pa k Park d e e Black Creek John Burroughs 44 N e d R R i Nature Sactuary e v State Forest k k e r a s i i L S Chodikee d B e Rd Gordon Highland O Y 299 L L D Property 44 Black Creek 9W S Burroughs Dr 9W Preserve Franny Reese State Park Walkway Over HUDSON RIVER the Hudson 9 Y D E 9 9 H 40A P A R K 41 BlackBlack CreekCreek TrailTrail Plan Bike | Paddle | Hike Black Creek Trail Table of Contents Sections Maps & Graphics 1| Introduction 7 Trail Concept 6-7 1.1| Executive Summary 8 1.2| Conserved Lands 11 Conserved Lands 10 2| Existing Conditions 13 Conserved Lands 12-13 2.1| Access & Connections 15 Issues 15 2.2| Trail Conditions 16 2.3| Educational Programing 17 2.4| Corridor Ecology 18 2.5| Economic Development 19 Potential Redevelopment Sites 19 2| Recommendations 21 Trail Route 20-21 3.1| Recommended Trail Route 23 Trail Route 23 3.1.1| Biking 24 Ose Road Crossing & BCSF Entrance 24 3.1.2| Paddling 25 3.1.3| Hiking 26 Hiking Trail Detail 27 3.2| Access Improvements 29 Trail Access 29 3.3| Wayfinding & Branding 30 3.4| Environmental Protection 31 3.5| Land Conservation 32 3.6| Educational Programing 33 3.7| Revitalize Properties 34 3.8| Develop Businesses 35 3.9| -
Stratigraphic and Structural Relationships of the Ordovician
NYSGA 2009 Trip 3 - Pratt Trip 3 - Pratt Stratigraphic and Structural Relationships of the Ordovician Flysch and Molasse along the Western Boundary of the Taconic Allochthon near Kingston NY Gerald Pratt New York State Department of Environmental Conservation Overview This trip will visit recently described exposures of the allochthonous Ordovician Normanskill Group juxtaposed against autochthonous Quassaic and Martinsburg sedimentary rocks. Exposures in the Kingston and Esopus Town- ships demonstrate through stratigraphic position, sedimentary structures and fossils, the collapse of a foredeep basin and subsequent down warping of a foreland basin during the latest stages of the Taconic Orogeny. The trip includes several stops at outcroppings of the allochthon strata, Taconic Unconformity and the later arenites of the Quassaic, which contain an unusual molasse facies. Introduction Sandstone petrology of compositions of the strata in the field trip area indicate Ordovician formations originate from a volcanic terrain and are classified as recycled orogen blocks directly or indirectly. It is likely that these formations were formed proximal to one another. A structural inlier consisting of fossiliferous thin shale and siltstone is identi- fied and delineated within unfossiliferous massive arenites. Structural geometry, biostratigraphy and sedimentology were analyzed to constrain the inlier stratigraphic boundaries to the Martinsburg Formation. Massive Ordovician arenites in the study area are uncharacteristic of those of the Normanskill Group, lacking fauna and allocyclic char- acteristic. Bedding is massive, exceeding 5 meters containing laminate sets and contained greater amounts of quart and lesser amounts of calcite and lithic fragments as well. Sedimentology of the massive arenites suggests this form- ation is an alluvial or olistostrome deposit and its structural position would place it above the Normanskill Group. -
Marlborough, NY
Town of Marlborough, NY LOCAL WATERFRONT REVITALIZATION PROGRAM COMPREHENSIVE PLAN AND DRAFT GENERIC ENVIRONMENTAL IMPACT STATEMENT SEPTEMBER 2020 PREPARED BY: Cover Page Local Waterfront Revitalization Program (LWRP), Comprehensive Plan, and Draft Generic Environmental Impact Statement (GEIS) For the Town of Marlborough, New York Title of the Action: Adoption of the Town of Marlborough Local Waterfront Revitalization Program (LWRP) including a Harbor Management Plan, Local Consistency Review Law, and Harbor Management Law; and adoption of the Town of Marlborough Comprehensive Plan Project Location: Town of Marlborough, Ulster County, New York Lead Agency: Town of Marlborough Town Board 21 Milton Turnpike, Suite 200/ PO Box 305 Milton, NY 12547 Contact: Alphonso Lanzetta, Town Supervisor 845-795-5100 Prepared by: Town of Marlborough LWRP and Comprehensive Plan Advisory Committee, with assistance from Behan Planning and Design Comprehensive Plan Adopted: December 11, 2017 LWRP Adopted: Town of Marlborough Town Board, May 11, 2020 LWRP Approved: New York State Secretary of State, Rossana Rosado: November 12, 2020 U.S. Office for Coastal Management: Draft Generic Environmental Impact Statement Introduction and Orientation to the Documents. These documents represent a coordinated effort by the Town of Marlborough to create and adopt a local waterfront revitalization program (LWRP) and to prepare and adopt an update to the town’s comprehensive plan. The LWRP also includes a harbor management plan. To implement the LWRP and the harbor management plan contained herein the town has also drafted a local law to ensure future actions taken by agencies of the town are consistent with the waterfront revitalization policies. A harbor management local law has also been prepared to regulate the use of waters within the town in conformance with the LWRP including the harbor management plan. -
Appendix 1: Community Profile and Review of Past Plans January 30, 2019
Town of Esopus Comprehensive Plan Appendix 1: Community Profile and Review of Past Plans January 30, 2019 (518) 458-7112 • [Page Intentional left blank] Town of Esopus Comprehensive Plan Table of Contents REVIEW OF PAST PLANS .........................................................................................................................................................1 COMMUNITY PROFILE ..........................................................................................................................................................10 Demographic and Growth Trends Analysis .................................................................................................................................................... 10 Housing and Marketing Trends....................................................................................................................................................................... 19 Education ........................................................................................................................................................................................................ 24 Civic and Community Organizations .............................................................................................................................................................. 26 Arts,Culture, and Historic Resources .............................................................................................................................................................. 29 Community -
4. Water Temperature
A. GENERAL OVERVH3W The cultural and natural history of the Hudson River has been studied and described by individuals and institutions with diverse interests and opinions since the beginning of recorded history in America. There is a wealth of orm mat ion and data to describe the environmental setting for the proposed action; this chapter summarizes this idormation, highlighting and describing in detail those aspects of the environment that are potentially influenced by the action. Information from many sources has been reviewed and included; however, the bulk of the data used to describe the biology, chemistry, and physical processes of the Hudson River come ffom the monitoring program developed in consultation with the DEC over the past 12 years. The sampling design, equipment, and standard operating procedures for all aspects of the monitoring studies have been described in detail in annual reports (see Appendix V-1). A synopsis of the program is included in Appendix V-2. For the reader's convenience key elements of the program are summarized as appropriate in the sections on biological and chemical characteristics. Few water bodies have been the subject of sampling and evaluation over a multiyear period. The major deterrents to accumulating usable multiyear data are year-to-year inconsistencies in sampling and analysis protocols. All sampling and analyses are described in detail in the references listed in Appendix V-1 . To control bias introduced by changes, even inadvertent, in standard procedures, the Hudson River Utilities Monitoring Program was the subject of an extensive, documented, quality control and assurance program. The components of the QNQC pro- and its results are described in Young et al.