Lake Champlain Research Consortium
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Vermont Department of Environmental Conservation Agency of Natural Resources
Vermont Department of Environmental Conservation Agency of Natural Resources WATER INVESTMENT DIVISION National Life Building, DAVIS 3 1 National Life Drive Montpelier, VT 05620-3510 FAX: (802)828-1552 Ms. Megan Moir, Assistant DPW Director of Water Resources Authorized Representative City of Burlington 234 Penny Lane Burlington, VT 05401 January 14, 2021 Expiration Date: January 14, 2026 Re: Manhattan Drive Outfall Repairs Project Vermont/ USEPA Clean Water Revolving Loan Number RF1‐2xx (Pending) Notice of Intent to Issue a Finding of No Significant Impact Dear Megan: The Department of Environmental Conservation intends to issue a Finding of No Significant Impact (FONSI) for the Manhattan Drive Outfall Repairs Project. The project has positive environmental impacts consisting of the reduction of erosion and sediment movement into the adjacent waters of the state and improved reliability and resiliency of the adjacent municipal sewer and stormwater systems. This project additionally involves impacts to wetlands and floodplains in the form of permitted wetlands impacts and de minimus floodplain impacts. Otherwise, this project may have been eligible for Categorical Exclusion from detailed environmental review; additionally, the direct and indirect environmental effects of the project are still not significant enough to necessitate an Environmental Impact Statement (EIS). The Department's environmental review procedures require a 30‐day public comment period following the issuance of a Notice of Intent to Issue a Finding of No Significant Impact. If no public comments received during that period demonstrate that this Notice of Intent is in error, then the Finding of No Significant Impact will become effective. Page 2 of 2 Megan Moir, Authorized Representative, City of Burlington Manhattan Drive Outfall Repairs Finding of No Significant Impact January 14, 2021 Copies of documents supporting a Finding of No Significant Impact are enclosed. -
Dams and Reservoirs in the Lake Champlain Richelieu River Basin
JUST THE FACTS SERIES June 2019 DAMS AND RESERVOIRS IN THE LAKE CHAMPLAIN RICHELIEU RIVER BASIN MYTH Water released from tributary dams in the United States causes flooding in Lake Champlain and the Richelieu River. FACT Water levels in Lake Champlain and the Richelieu River Generally, mass releases of water from flood control are primarily affected by precipitation from rain or dams are avoided. In addition to compromising the snowmelt. structural integrity of the dams, mass releases would also endanger the very communities that these dams are built Because of its size, Lake Champlain can store a lot of to protect. water; the flood control dams and reservoirs in the basin, which are very small in comparison to the lake, do not When conditions force the release of more water than significantly change water levels of the lake and river as hydropower plants can handle, the increase in water they release water. levels immediately below the dam will be much greater than the increase on Lake Champlain. This is true even during high water and flooding events. Consider, for instance, when Lake Champlain and the Richelieu River experienced extreme flooding between April and June 2011, the additional releases flowing from Waterbury Reservoir—the largest flood control reservoir in the Vermont portion of the basin, contributed less than 2 centimetres (¾ inch) to the elevation of Lake Champlain and the upper Richelieu River. International Lake Champlain-Richelieu River Study Board FACT FACT Dams in the US portion of the basin are built for one of Waterbury Reservoir in Vermont is the largest reservoir two purposes: flood control or hydroelectric power. -
Wholesale Sales Reps by State Effective July 1, 2021 "Independent
Wholesale Sales Reps by State effective July 1, 2021 "Independent" Customers in these Sales Representative Phone E-mail states Alabama Renee Cohen 802-864-1808 ext. 2151 [email protected] Alaska Market 2 Market 800-228-2157 [email protected] Arizona Skotak & Company (602) 538-1740 [email protected] Arkansas Renee Cohen 802-864-1808 ext. 2151 [email protected] Renaissance & GMI distributor for everyday/ seasonal = LCC Team and California Barbara Emmerich (Nor CA select accts) (707) 526-1592 [email protected] Colorado CA Fortune (630) 539-3100 [email protected] Connecticut Travis Edwards 617-913-8062 [email protected] Delaware Travis Edwards 617-913-8063 [email protected] District of Columbia Travis Edwards 617-913-8063 [email protected] Florida The Cristol Group 954-486-4129 [email protected] Georgia Renee Cohen 802-864-1808 ext. 2151 [email protected] Hawaii LCC sales/customer service team Idaho CA Fortune (630) 539-3100 [email protected] Illinois Specialty Food Sales 847-763-8601 [email protected] Indiana Renee Cohen 802-864-1808 ext. 2151 [email protected] Iowa Maria Green & Associates 800-509-9775 [email protected] Kansas Maria Green & Associates 800-509-9775 [email protected] Kentucky Renee Cohen 802-864-1808 ext. 2151 [email protected] Louisiana Renee Cohen 802-864-1808 ext. 2151 [email protected] Maine Giovanni Cassano 802-557-8110 -
Constraints on Lake Agassiz Discharge Through the Late-Glacial Champlain Sea (St
Quaternary Science Reviews xxx (2011) 1e10 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Constraints on Lake Agassiz discharge through the late-glacial Champlain Sea (St. Lawrence Lowlands, Canada) using salinity proxies and an estuarine circulation model Brandon Katz a, Raymond G. Najjar a,*, Thomas Cronin b, John Rayburn c, Michael E. Mann a a Department of Meteorology, 503 Walker Building, The Pennsylvania State University, University Park, PA 16802, USA b United States Geological Survey, 926A National Center, 12201 Sunrise Valley Drive, Reston, VA 20192, USA c Department of Geological Sciences, State University of New York at New Paltz, 1 Hawk Drive, New Paltz, NY 12561, USA article info abstract Article history: During the last deglaciation, abrupt freshwater discharge events from proglacial lakes in North America, Received 30 January 2011 such as glacial Lake Agassiz, are believed to have drained into the North Atlantic Ocean, causing large Received in revised form shifts in climate by weakening the formation of North Atlantic Deep Water and decreasing ocean heat 25 July 2011 transport to high northern latitudes. These discharges were caused by changes in lake drainage outlets, Accepted 5 August 2011 but the duration, magnitude and routing of discharge events, factors which govern the climatic response Available online xxx to freshwater forcing, are poorly known. Abrupt discharges, called floods, are typically assumed to last months to a year, whereas more gradual discharges, called routing events, occur over centuries. Here we Keywords: Champlain sea use estuarine modeling to evaluate freshwater discharge from Lake Agassiz and other North American Proglacial lakes proglacial lakes into the North Atlantic Ocean through the St. -
17 Major Drainage Basins
HUC 8 HYDROLOGIC UNIT NAME CLINTON 04120101 Chautauqua-Conneaut FRANKLIN 04150409 CHAMPLAIN MASSENA FORT COVINGTON MOOERS ST LAWRENCE CLINTON 04120102 Cattaraugus BOMBAY WESTVILLE CONSTABLE CHATEAUGAY NYS Counties & BURKE LOUISVILLE 04120103 Buffalo-Eighteenmile BRASHER 04150308 CHAZY ALTONA ELLENBURG BANGOR WADDINGTON NORFOLK MOIRA 04120104 Niagara ESSEX MALONE DEC Regions JEFFERSON 6 04150307 BEEKMANTOWN MADRID 05010001 Upper Allegheny LAWRENCE BELLMONT STOCKHOLM DANNEMORA BRANDON DICKINSON PLATTSBURGH LEWIS OGDENSBURG CITY LISBON 05010002 Conewango 5 PLATTSBURGH CITY HAMILTON POTSDAM SCHUYLER FALLS SARANAC 05010004 French WARREN OSWEGATCHIE DUANE OSWEGO 04150306 PERU 04130001 Oak Orchard-Twelvemile CANTON PARISHVILLE ORLEANS WASHINGTON NIAGARA DE PEYSTER ONEIDA MORRISTOWN HOPKINTON WAVERLY PIERREPONT FRANKLIN 04140101 Irondequoit-Ninemile AUSABLE MONROE WAYNE BLACK BROOK FULTON SARATOGA DEKALB HERKIMER BRIGHTON GENESEE SANTA CLARA CHESTERFIELD 04140102 Salmon-Sandy ONONDAGA NYS Major 04150406 MACOMB 04150304 HAMMOND ONTARIO MADISON MONTGOMERY RUSSELL 04150102 Chaumont-Perch ERIE SENECA CAYUGA SCHENECTADY HERMON WILLSBORO ST ARMAND WILMINGTON JAY WYOMING GOUVERNEUR RENSSELAER ALEXANDRIA CLARE LIVINGSTON YATES 04130002 Upper Genesee OTSEGO ROSSIE COLTON CORTLAND ALBANY ORLEANS 04150301 04150404 SCHOHARIE ALEXANDRIA LEWIS 7 EDWARDS 04150408 CHENANGO FOWLER ESSEX 04130003 Lower Genesee 8 TOMPKINS CLAYTON SCHUYLER 9 4 THERESA 04150302 TUPPER LAKE HARRIETSTOWN NORTH ELBA CHAUTAUQUA CATTARAUGUS PIERCEFIELD 02050104 Tioga ALLEGANY STEUBEN -
Welcome to the Walk of Change Nature Trail
Welcome to the Walk of Change 3. Monarch butterflies former land clearing for farming. The size of the 6. Is this The End? Monarch butterflies have one of the most stones may reveal whether the adjacent land was As you walked to this stop you may have noticed Nature Trail unusual and extreme life cycles of North used for crops or pasture. Stone piles or walls with a change in light and temperature. You just walked American butterflies. Adults migrate north, large rocks usually suggest the adjacent land was through a climax community. In this case, it is a Here at Knight Island State Park, the arriving in the northeast early in the growing a mowed field or a pasture in which only the large patch of mature forest. This does not mean the end landscape has been affected by many physical season. After mating, a female lays her eggs rocks needed to be removed. Small stones need to of change, though, or static condition in the forest. environmental and cultural factors over the on Common Milkweed, like you can see here. be removed from cultivated plots annually. This New growth slows as the forest canopy becomes geologic timescale. These include weather pile of small stones reveals that the surrounding enclosed with fewer, larger trees that are more extremes, glaciers, human habitation and area was used for crops. The crops grown on spaced out. At this state in a forest’s evolution, livestock grazing. Enjoy a walk along the Knight Island were beans, com and peas. change is brought by natural events such as storms trail system, and keep watch for signs of Common milkweed bringing wind and ice, or from cultural means like these changes; you might even witness some logging. -
The Late Quaternary Paleolimnology of Lake Ontario
Western University Scholarship@Western Electronic Thesis and Dissertation Repository 9-4-2014 12:00 AM The Late Quaternary Paleolimnology of Lake Ontario Ryan Hladyniuk The University of Western Ontario Supervisor Dr. Fred J. Longstaffe The University of Western Ontario Graduate Program in Geology A thesis submitted in partial fulfillment of the equirr ements for the degree in Doctor of Philosophy © Ryan Hladyniuk 2014 Follow this and additional works at: https://ir.lib.uwo.ca/etd Part of the Geochemistry Commons Recommended Citation Hladyniuk, Ryan, "The Late Quaternary Paleolimnology of Lake Ontario" (2014). Electronic Thesis and Dissertation Repository. 2401. https://ir.lib.uwo.ca/etd/2401 This Dissertation/Thesis is brought to you for free and open access by Scholarship@Western. It has been accepted for inclusion in Electronic Thesis and Dissertation Repository by an authorized administrator of Scholarship@Western. For more information, please contact [email protected]. THE LATE QUATERNARY PALEOLIMNOLOGY OF LAKE ONTARIO (Thesis format: Integrated Article) by Ryan Hladyniuk Graduate Program in Earth Sciences A thesis submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy The School of Graduate and Postdoctoral Studies The University of Western Ontario London, Ontario, Canada © Ryan Hladyniuk 2014 Abstract We examined the oxygen isotopic composition of biogenic carbonates, carbon and nitrogen abundances and isotopic compositions of bulk organic matter (OM), and the abundances and carbon isotopic compositions of individual n-alkanes (C17 to C35) for samples from three, 18 m long sediment cores from Lake Ontario in order to: (i) assess how changing environmental parameters affected the hydrologic history of Lake Ontario, and (ii) evaluate changes in organic productivity and sources since the last deglaciation. -
By Mary K. Roden-Tice. Center for Earth and Environmental Science, Plattsburgh State University Ofnew York, Plattsburgh
A2-1 BEST KEPT GEOLOGIC SECRETS OF THE ADIRONDACKS AND CHAMPLAIN VALLEY by Mary K. Roden-Tice. Center for Earth and Environmental Science, Plattsburgh State University ofNew York, Plattsburgh. NY 12901 INTRODUCTION Finding clear, well-exposed field locations to help illustrate important aspects of petrology and structural geology to undergraduate students can be a challenge for a professor. In this field trip, we will visit the following four field stops in the Adirondack Mountains and Champlain Vaney that are routinely used in my classes: the Cannon Point intrusive south ofEssex; the Craig Harbor faultIine scarp in Port Henry; the intrusion breccia in Roaring Brook on Giant Mt.; and Split Rock Falls crackle zone south of New Russia. In structural geology, the class works on field exercises that illustrate normal faulting at Craig Harbor and different orientations ofjoint sets at Split Rock Falls. Petrology students compare Proterozoic anorthosite containing xenoliths of metasedimentary rocks from the Roaring Brook intrusion breccia on Giant Mt. with a Cretaceous laccolith of trachyte porphyry on the shore of Lake Champlain. All oftbese outcrops are easily accessible and provide excellent opportunities for experientialleaming. REGIONAL GEOLOGY Summary The Adirondack Mountains are a regionallyelevllted exposure of Grenville age (ca. 1.0-1.35 Ga; McLelland et aI., 1988; McLelland and Chiarenzelli, 1990; Mezger et al., 1991; McLelland et at, 1996) higb-grade metamorphic rocks in northern New York state. This field trip will examine granulite-facies metaplutonic rocks (McLelland and Isachsen, 1986) in the Adirondack Highlands which comprise the central and eastern portions of the massif. An abrupt transition in topography occurs between the Adirondack Highlands and the Lake Champlain Valley between New York and Vermont with local relief along Lake Champlain varying from -170 to 370 m. -
Oxygen-Isotope Variations in Post-Glacial Lake Ontario Ryan Hladyniuk the University of Western Ontario, [email protected]
Western University Scholarship@Western Earth Sciences Publications Earth Sciences Department 1-5-2016 Oxygen-isotope Variations in Post-glacial Lake Ontario Ryan Hladyniuk The University of Western Ontario, [email protected] Fred J. Longstaffe The University of Western Ontario, [email protected] Follow this and additional works at: https://ir.lib.uwo.ca/earthpub Part of the Earth Sciences Commons Citation of this paper: Hladyniuk, Ryan and Longstaffe, Fred J., "Oxygen-isotope Variations in Post-glacial Lake Ontario" (2016). Earth Sciences Publications. 4. https://ir.lib.uwo.ca/earthpub/4 1 1 Oxygen-isotope variations in post-glacial Lake Ontario 2 3 Ryan Hladyniuk1 and Fred J. Longstaffe1 4 5 1Department of Earth Sciences, The University of Western Ontario, London, Ontario, 6 Canada N6A5B7 7 8 Corresponding authors, [email protected] 1-519-619-3857; [email protected], 1-519-661- 9 3177 10 11 Keywords: Lake Ontario, oxygen isotopes, glacial meltwater, Laurentide Ice Sheet, late- 12 Quaternary climate change 13 14 15 16 17 18 19 20 21 22 2 23 Abstract 24 The role of glacial meltwater input to the Atlantic Ocean in triggering the Younger Dryas 25 (YD) cooling event has been the subject of controversy in recent literature. Lake Ontario 26 is ideally situated to test for possible meltwater passage from upstream glacial lakes and 27 the Laurentide Ice Sheet (LIS) to the Atlantic Ocean via the lower Great Lakes. Here, we 28 use the oxygen-isotope compositions of ostracode valves and clam shells from three Lake 29 Ontario sediment cores to identify glacial meltwater contributions to ancient Lake 30 Ontario since the retreat of the LIS (~16,500 cal [13,300 14C] BP). -
October 1980 Volume 1 the Geology of the Lake
OFPCE OF THE STATE GEOLOGIST VERMONT GEOLOGY OCTOBER 1980 VOLUME 1 THE GEOLOGY OF THE LAKE CHAMPLAIN BASIN AND VICINITY Proceedings of a Symposium CONTENTS Introduction to the environmental geology of Lake Champlain and shoreland areas R. Montgomery Fischer 1 The application of Lake Champlain water level studies to the investigation of Adirondack and Lake Champlain crustal movements Stockton G. Barnett Yngvar W. Isachsen 5 The stratigraphy of unconsolidated sediments of Lake Champlain Allen S. Hunt 12 Alkalic dikes of the Lake Champlain Valley J. Gregory McHone E. Stanley Corneille 16 Mesozoic faults and their environmental significance in western Vermont Rolfe S. Stanley 22 Estimating recharge to bedrock ground- water in a small watershed in the Lake Champlain drainage basin Craig D. Heindel 33 EDITOR Jeanne C. Detenbeck EDI TORIAL COMMI TTEE Charles A. Ratte' Frederick D. Larsen VERMONT GEOLOGICAL SOCIETY, INC. Vermont Geological Society Box 304 Montpelier, Vermont 05602 FOR WA RD The Vermont Geological- Society was founded in 1974 for the purpose of C1) advancing the science and profession of geology and its related branches by encouraging education, research and service through the holding of meetings, maintaining communications, and providing a common union of its members; 2) contributing to the public education of the geology of Vermont and prcsnoting the proper use and protection of its natural resources; and 3) advancing the professional conduct of those engaged in the collection, interpretation and use of geologic d a t aC. To these ends, in its 7 year history, the society has prcnnoted a variety of field trips, an exposition on Vermont geology, , presentations of papers by both professional and student researchers, teachers workshops, a seminar on water quality, a soils workshop and a seismic workshop. -
Lake Champlain Basin Bibliography
Lake Champlain Basin Bibliography www.lcbp.org Prepared by: Lake Champlain Basin Program Date: Updated 7/17/10 Contact the LCBP: 802-372-3213 (LCBP Main Office located in Grand Isle, VT) 802-864-1848 ext. 109 (LCBP Resource Room, Leahy Center for Lake Champlain, Upper Level, ECHO Lake Aquarium and Science Center) Please Note: This bibliography is intended for general use and is not a comprehensive academic reference. The LCBP is not responsible for the content or accuracy of these books, or of any non-LCBP publication. Bibliography comments and suggestions are welcomed. Lake Champlain History - General Beach, Allen Penfield. Lake Champlain as Centuries Pass. Basin Harbor, VT: Lake Champlain Maritime Museum, 1994. (Reprint.) Bellico, Russell P. Chronicles of Lake Champlain: Journeys in War and Peace. Fleischmanns, NY: Purple Mountain Press, 1999. Bellico, Russell P. Sails and Steam in the Mountains: A Maritime and Military History of Lake George and Lake Champlain. Fleischmanns, NY: Purple Mountain Press, 2001. Coffin, Howard, Will Curtis and Jane Curtis. Guns Over the Champlain Valley: A Guide to Historic Military Sites and Battlefields. Woodstock, VT: Countryman Press, 2005. Crockett, Walter Hill. A History of Lake Champlain. Burlington, VT: McAuliffe Paper Co., Revised edition 1936. (Originally published in 1909.) Hill, Ralph Nading. Lake Champlain: Key to Liberty. Revised edition. Woodstock, VT: Countryman Press, 1995. Lundeberg, Philip. The Gunboat Philadelphia and the Defense of Lake Champlain in 1776. Basin Harbor, VT: Lake Champlain Maritime Museum, 1995. Lake Champlain: An Illustrated History. Jay, NY: Adirondack Life, 2009. Millard, James P. The Secrets of Crab Island. South Hero, VT: America’s Historic Lakes, 2004. -
Nutrient Loading and Impacts in Lake Champlain, Missisquoi Bay, and the Richelieu River
Nutrient Loading and Impacts in Lake Champlain, Missisquoi Bay, and the Richelieu River Draft Report prepared by: New England Interstate Water Pollution Control Commission Lake Champlain Basin Program Organisme de basin versant de la baie Missisquoi For : International Joint Commission Table of Contents Executive Summary 1 1 Introduction 2 1.1 Background, Purpose, and Scope 2 1.2 Prior IJC Work in the Lake Champlain Basin 3 1.2.1 Causeway Removal Water Quality Study 3 1.2.2 Identification of Critical Source Areas 4 1.2.3 Lake Champlain-Richelieu River Flood Mitigation Studies 4 1.3 Study Areas 5 1.3.1 Lake Champlain 5 1.3.2 Richelieu River 6 1.3.3 Missisquoi Bay 6 1.4 Literature Review and Quality Assurance 9 2 Key Nutrient Loading and Cyanobacteria Issues 9 2.1 Overview of Nutrient Loading and Cyanobacteria Issues in Lake Champlain and Missisquoi Bay 9 2.2 Detailed Analyses of Missisquoi Bay and Its Sub-Basin 12 2.2.1 Hydrodynamics 14 2.2.2 Nutrient Enrichment 14 Dynamics, Sources, and Causes 14 2.2.3 Cyanobacteria Blooms 19 Cyanobacteria & Cyanotoxins 19 Sources and Causes 22 2.2.4 Health Risks and Recreational Impacts 23 2.2.5 Economic Impacts 25 3 Overview of Potential In-Lake Restoration Measures and Technologies 26 3.1 International Overview of Restoration Efforts and Results 26 3.1.1 Canada 26 3.1.2 U.S. 27 Commonly Used In-Lake Restoration Techniques 27 Regional Lake Restoration Efforts 28 3.2 Effectiveness Results and Analysis, Estimated Cost-Benefit, and Adaptability to Missisquoi Bay 35 4 Programs and Policies Influencing Key