Water Quality Study of the Finger Lakes: Part B: Sediment Core Investigation Clifford W
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Historic Aspects of the Phelps and Gorham Treaty of July 4-8, 1788
Edited by DEXTER PERKINS, City Historian and BLAKE MCKELVEY, Assistant City Historian VOL. 1 JANUARY, 1939 No. 1 Historic Aspects of the Phelps and Gorham Treaty of July 4-8, 1788 By BLAKE MCKELVEY The commemoration of the 150th anniversary of the Phelps and Gorham treaty with the Indians presents a challenge to the imagination. The years that have passed since that July council on Buffalo Creek have seen great changes come over this beautiful country. We think first of the marvellous material changes that have taken place, for they are obvious on all sides. We might with much profit consider the institu- tional and cultural developments that make those events of 150 years ago appear like the fanciful episodes of some romantic tale. But it is not the contrast or the changes that we wish to com- memorate. That council on Buffalo Creek was a very real, a very significant occasion. The chain of events of which it was a part, and the setting in which it occurred, were vital aspects of the history of Western New York, and influenced developments throughout the country. Therefore, the recollection of this historic occasion merits our close attention, even though we shall have to turn over many of history’s musty pages in the process. A brief study of the documents is enough to reveal that the men who took part in the treaty at Buffalo Creek, and in the far-flung intrigues that followed it, were sons of Adam as we know them today- some crafty and some straightforward, some simple and some endowed with foresight, some mean and selfish, and some honestly concerned ROCHESTER HISTORY, published quarterly by the Rochester Public Library, dis- tributed free at the Library, by mail 25 cents per year. -
Hemlock-Canadice Unit Management Plan
Division of Lands & Forests Bureau of State Land Management HEMLOCK-CANADICE UNIT MANAGEMENT PLAN Final Livingston County towns of Livonia, Conesus and Springwater Ontario County towns of Richmond and Canadice January 2015 NYS Department of Environmental Conservation Region 8 Sub-Office 7291 Coon Rd. Bath, New York 14810 Hemlock-Canadice Unit Management Plan New York State Department of Environmental Conservation’s Mission “The quality of our environment is fundamental to our concern for the quality of life. It is hereby declared to be the policy of the State of New York to conserve, improve and protect its natural resources and environment and to prevent, abate and control water, land and air pollution, in order to enhance the health, safety and welfare of the people of the state and their overall economic and social well-being.” - Environmental Conservation Law 1-0101(1) Preface It is the policy of the New York State Department of Environmental Conservation (NYS DEC) to manage state lands for multiple benefits to serve the people of New York State. This Unit Management Plan (Unit) is the first step in carrying out that policy. The plan has been developed to address management activities on this unit for the next 10 year period. Some management recommendations may extend beyond the 10 year period. Factors such as budget constraints, wood product markets, and forest health problems may necessitate deviations from the scheduled management activities. Vision Statement for All State Forests State Forests on the Hemlock-Canadice Unit will be managed in a sustainable manner by promoting ecosystem health, enhancing landscape biodiversity, protecting soil productivity and water quality. -
Sturgeon Research in NY 2017. NY Chapter, American Fisheries Society
Citation: 2017. Brooking, Thomas E. Sturgeon Research in NY 2017. NY Chapter, American Fisheries Society. Annual Meeting Abstracts. Feb. 1-3, 2017. Buffalo, NY. 45 pp. Thursday February 2, 2017 Keynote Speakers 8:35 AM-9:20 AM Title: Lake Sturgeon recovery: Optimism for long-term success Author: Ron Bruch Affiliation: Fisheries Chief (retired), Wisconsin Dept. of Natural Resources Contact: [email protected] Abstract: Biologists who have worked with Lake Sturgeon are all aware of the devastating declines in abundance and habitat the species experienced in the Great Lakes and elsewhere throughout its range in North America in the late 1800s and early 1900s. Yet today in the early part of the 21st Century Lake Sturgeon populations overall enjoy much greater protection from over-exploitation, and have greater opportunities for recovery and sustainability throughout their range than they have experienced since the early 19th Century. A combination of factors including: increased attention over the last 30-40 years by state and provincial governments to effectively manage harvest and conduct proper assessments, increased public awareness of LS and their extreme vulnerability to overexploitation, improvements in assessment techniques, improvement in LS propagation techniques and stocking strategies, exponential expansion of population studies and research, increasing awareness and efforts to improve habitat and water quality, and the formation of the North American Sturgeon and Paddlefish and World Sturgeon Conservation Societies have all contributed to greater protection and recovery potential. While these are all positive steps that collectively should allow many LS populations to continue or start down the road to recovery, there are still waters and populations that may not be getting the attention needed to allow their recovery to occur. -
Holocene Climate Change in Keuka Lake, Ny
Lyons, D.I. 2006. 19th Annual Keck Symposium; http://keck.wooster.edu/publications GETTING TO THE BOTTOM OF IT: HOLOCENE CLIMATE CHANGE IN KEUKA LAKE, NY DAVIN I. LYONS Skidmore College Sponsor: Kyle Nichols INTRODUCTION Site Description Lakes often respond to variations in temperature Keuka Lake is the third largest of the 11 Finger and precipitation by changing their hydrologic Lakes by surface area (47 km2) and fifth by balance. Previous studies suggest the timing of volume (1.4 km3) (Mullins et al., 1996) (Fig1 lake highstands and lowstands in the Midwest Not available). The lake has two unique does not correlate with those in the eastern characteristics compared to the other Finger United States. The mid-Holocene Hypsithermal Lakes. It has a Y-shape and it drains eastward (~9 - ~5 ka) is recorded as a period of warm, dry into another Finger Lake, Seneca Lake. Its climate in western and central North America present morphology results from the deepening (COHMAP 1988; Dean et al. 1996), but as a of pre-existing stream valleys during the warm, wet interval in the eastern Great Lakes Wisconsin glaciation, which explains why the region (Dwyer at al. 1996; Silliman et al. 1996). Keuka Lake is narrow (3.3 km max. width) and In the White Mountains, NH, pollen records long (32 km). The narrow, deep basin (up to indicate a moister climate than present between 57 m) allows for the collection of undisturbed 10,000 and 8,000 yr BP and a warmer period sediment that preserve suitable records of (2°C warmer than present) occurred at ~9,000 environmental changes since the retreat of the yr BP (Shuman et al., 2002; Davis et al., 1980). -
Summertime 2020 Hilary Lambert CLWN Steward Many People Have Been Noting That Nature’S Annual Seasonal Rounds Have Continued, Regardless of Our Human Problems
CAYUGA LAKE WATERSHED 2020 i2 Network It takes a Network to protect a watershed. News Summertime 2020 Hilary Lambert CLWN Steward Many people have been noting that nature’s annual seasonal rounds have continued, regardless of our human problems. As our human cacophony has died down, some have wondered if nature is emerging, edging outward. Here’s my recent experience: When I went outside to walk my dog at 5:30 a.m., a deer was sleeping in the front yard on the recently-mown grass, halfway between my bedroom window and Hanshaw Road. She woke up, stared at us, and ambled slowly across the empty road to the fields. here’s a redwing blackbird just down next door pond wandered freely and the out-of-doors during these interesting, the road who daily divebombs talkatively around my yard, unafraid tragic, and strange times. Tme, my dog, and the neighbors, I of my household. I have heard of many Many people have gone to the lake to suppose for getting too close to the family other such close encounters, since shortly paddle, walk, and swim, are hiking along nest. It is probable that a bobcat visited after the pandemic began and people- creeks and to waterfalls for solace and the backyard in April (falling off a white pressure retreated. release. Families and friends sheltered pine branch with a yowl), terrifying my Is it us, or is it them? In any case, we at lakeside cottages outside the usual cats. The mallard ducks situated at the should treasure our deeper immersion in summer season, to be together and avoid pandemic dangers. -
2014 Update on the Chloride Hydrogeochemistry in Seneca Lake, New York
A 2014 UPDATE ON THE CHLORIDE HYDROGEOCHEMISTRY IN SENECA LAKE, NEW YORK. John Halfman Department of Geoscience, Environmental Studies Program, Finger Lakes Institute Hobart & William Smith Colleges Geneva, NY 14456 [email protected] 12/10/2014 Introduction: Seneca Lake is the largest of the 11, elongated, north-south trending, Finger Lakes in central and western New York State (Fig. 1). It has a volume, surface area, watershed area, and maximum depth of 15.5 km3, 175 km2, 1,621 km2 (including Keuka watershed), and 188 m, respectively (Mullins et al., 1996). The lake basins were formed by glacial meltwaters eroding and deepening former stream valleys underneath the retreating Pleistocene Ice Sheet cutting into the Paleozoic sedimentary rocks approximately 10,000 years ago. Each basin was subsequently filled with a thick deposit of glacial tills and a thin veneer of pro-glacial lake clays. Basins not completely filled with sediment (e.g., Tully Valley), were subsequently filled with water and slowly accumulating postglacial muds. Seneca Lake is classified as a Class AA water resource by the New York State Department of Environmental Conservation (NYS DEC), except for a few locations along the shore (http://www.dec.ny.gov/regs/4592.html, Halfman et al., 2012). It supplies drinking water to approximately 100,000 people in the surrounding communities. Berg (1963) and Schaffner and Oglesby (1978) noted that chloride concentrations were significantly larger in Seneca Lake, and to a lesser extent in Cayuga Lake, than the other Finger Lakes. Wing et al. (1995) argued that the elevated chloride concentrations required an extra source of chloride beyond the measured fluvial fluxes to the lake. -
Harmful Algal Bloom Action Plan Conesus Lake
HARMFUL ALGAL BLOOM ACTION PLAN CONESUS LAKE www.dec.ny.gov EXECUTIVE SUMMARY SAFEGUARDING NEW YORK’S WATER Protecting water quality is essential to healthy, vibrant communities, clean drinking water, and an array of recreational uses that benefit our local and regional economies. 200 NY Waterbodies with HABs Governor Cuomo recognizes that investments in water quality 175 protection are critical to the future of our communities and the state. 150 Under his direction, New York has launched an aggressive effort to protect state waters, including the landmark $2.5 billion Clean 125 Water Infrastructure Act of 2017, and a first-of-its-kind, comprehensive 100 initiative to reduce the frequency of harmful algal blooms (HABs). 75 New York recognizes the threat HABs pose to our drinking water, 50 outdoor recreation, fish and animals, and human health. In 2017, more 25 than 100 beaches were closed for at least part of the summer due to 0 HABs, and some lakes that serve as the primary drinking water source for their communities were threatened by HABs for the first time. 2012 2013 2014 2015 2016 2017 GOVERNOR CUOMO’S FOUR-POINT HARMFUL ALGAL BLOOM INITIATIVE In his 2018 State of the State address, Governor Cuomo announced FOUR-POINT INITIATIVE a $65 million, four-point initiative to aggressively combat HABs in Upstate New York, with the goal to identify contributing factors fueling PRIORITY LAKE IDENTIFICATION Identify 12 priority waterbodies that HABs, and implement innovative strategies to address their causes 1 represent a wide range of conditions and protect water quality. and vulnerabilities—the lessons learned will be applied to other impacted Under this initiative, the Governor’s Water Quality Rapid Response waterbodies in the future. -
Ulysses Ithaca Antiques Mall, 1607 Trumansburg Rd
Touring the Towns of 1827, has been used as office, commercial, and residential space. Morning Glory, 89 Cayuga St, Trumansburg. 607-387-5305. Cemeteries C Tompkins County, New York At 1822 Trumansburg Rd is The Trees, a handsome early www.morningglory.com.laurie corner of Cemetery and Falls Sts, Trumansburg. See #7. Italianate house built in 1865 by James M. Mattison, owner of a Grove, popular nursery and tree farm on the site, which was started in Reunion House, 7550 Willow Creek Rd. 607-387-6553. Jones-Goodwin’s Point, Gorge Rd, west of Taughannock Farms 1845 and continued through the early 1870s. It is a private www.reunion-house.com Inn. residence today. Taughannock Farms Inn, Rt 89 at Taughannock Falls State Park. Quaker, see #9. 607-387-7711. www.t-farms.com. See #2. 9.9 Hector Monthly Meeting House, at 5066 Perry City Rd, St. James, Searsburg Rd, Trumansburg. 1 mile W of the Rt 96 intersection on the north side of the road, Westwind, 1662 Taughannock Blvd. 607-387-3377. this white clapboard building was erected c.1910, for the area’s www.fingerlakes.net/westwind Historical Markers Ħ Quaker community. There is also a cemetery. An old stone post Camp Site – Taughannock Falls State Park, north side. Site of at the driveway entrance has the carved letters HMMSOF, Antiques and Speciality Shops S 1788 exploring party’s camp. Hector Monthly Meeting, Society of Friends. Today the building Cold Springs Pottery Studio, 4088 Cold Springs Rd. Samuel Weyburn – Taughannock Falls State Park, south side. is used by the Ithaca Society of Friends for summer worship only. -
Town of Seneca
TOWN OF BRISTOL Inventory of Land Use and Land Cover Prepared for: Ontario County Water Resources Council 20 Ontario Street, 3rd Floor Canandaigua, New York 14424 and Town of Bristol 6740 County Road 32 Canandaigua, New York 14424 Prepared by: Dr. Bruce Gilman Department of Environmental Conservation and Horticulture Finger Lakes Community College 3325 Marvin Sands Drive Canandaigua, New York 14424-8395 2020 Cover image: Ground level view of a perched swamp white oak forest community (S1S2) surrounding a shrub swamp that was discovered and documented on Johnson Hill north of Dugway Road. This forest community type is rare statewide and extremely rare locally, and harbors a unique assemblage of uncommon plant species. (Image by the Bruce Gilman). Acknowledgments: For over a decade, the Ontario County Planning Department has supported a working partnership between local towns and the Department of Environmental Conservation and Horticulture at Finger Lakes Community College that involves field research, ground truthing and digital mapping of natural land cover and cultural land use patterns. Previous studies have been completed for the Canandaigua Lake watershed, the southern Honeoye Valley, the Honeoye Lake watershed, the complete Towns of Canandaigua, Gorham, Richmond and Victor, and the woodlots, wetlands and riparian corridors in the Towns of Seneca, Phelps and Geneva. This report summarizes the latest land use/land cover study conducted in the Town of Bristol. The final report would not have been completed without the vital assistance of Terry Saxby of the Ontario County Planning Department. He is gratefully thanked for his assistance with landowner information, his patience as the fieldwork was slowly completed, and his noteworthy help transcribing the field maps to geographic information system (GIS) shape files. -
REFERENCES CITED __.(1920). Animal Life and Sewage in The
REFERENCES CITED BAKER, F. C. ( 1911). The Lymnaeidae ofNorth and Middle America - Recent and Fossil. Chicago Acad Sci. Special Pub. 3:1-539. PI. 1-57. __.(1920). Animal life and sewage in the Genesee River , N.Y. Amer. Nat. 54:152-161. In Ill. Bio. Mono. Vol. VII . April 1922 . NO . 2. Forbes, Trelease and Ward (Eds.), Univ . of Ill. Press. __. (1928a). The freshwater mollusca of Wisconsin, Part 1. Gastropoda. Wisconsin Geol. Nat. Hist. Surv. Bul. 70(1):1-507. PI. 1-28. __. (1945). The molluscan family Planorbidae. Univ. Ill. Press, Urbana, 530 pp. BINNEY, G. W. (1865). Land and freshwater snails of North America. Smithsonian Mise. Coll. No. 144, pt 3, p 113, Fig 225 . CHANDLER, A. C. and P. R. CLARK. (1961). Introduction to Parasitology, John Wiley (lOth ed.). DeKAY, J. E. (1843). Zoology of New York, Part 5. Mollusca of New York . Carroll and Cook, AJbany, 271 pp, PI. 1-40. FOREST, H.S., J. Q. WADE and T. F. MAXWELL. (1978). The Umnology of Conesus Lake. In Bloomfield, J. A. (ed.), Ecology of the Finger Lakes of New York State, AcademJc Press . HARMAN, W. N. and C. O. BERG. (1971). The freshwater Gastropoda of Central New York, with illus. keys to the genera and species. Search: Cornell Univ. Agr. Exp. Sta., Ent.lthaca, 1(4):1-68. HYMAN, L. H. (1968). The Invertebrates: Mollusca, Vol. 6. McGraw-Hill. Book Co. New York. MAURY, C. J. (1916). Freshwater shells from central and western New York. Nautilus 30:329-33. PENNAK, R. W. (1953). Freshwater invertebrates of the United States. -
Appendices Section
APPENDIX 1. A Selection of Biodiversity Conservation Agencies & Programs A variety of state agencies and programs, in addition to the NY Natural Heritage Program, partner with OPRHP on biodiversity conservation and planning. This appendix also describes a variety of statewide and regional biodiversity conservation efforts that complement OPRHP’s work. NYS BIODIVERSITY RESEARCH INSTITUTE The New York State Biodiversity Research Institute is a state-chartered organization based in the New York State Museum who promotes the understanding and conservation of New York’s biological diversity. They administer a broad range of research, education, and information transfer programs, and oversee a competitive grants program for projects that further biodiversity stewardship and research. In 1996, the Biodiversity Research Institute approved funding for the Office of Parks, Recreation and Historic Preservation to undertake an ambitious inventory of its lands for rare species, rare natural communities, and the state’s best examples of common communities. The majority of inventory in state parks occurred over a five-year period, beginning in 1998 and concluding in the spring of 2003. Funding was also approved for a sixth year, which included all newly acquired state parks and several state parks that required additional attention beyond the initial inventory. Telephone: (518) 486-4845 Website: www.nysm.nysed.gov/bri/ NYS DEPARTMENT OF ENVIRONMENTAL CONSERVATION The Department of Environmental Conservation’s (DEC) biodiversity conservation efforts are handled by a variety of offices with the department. Of particular note for this project are the NY Natural Heritage Program, Endangered Species Unit, and Nongame Unit (all of which are in the Division of Fish, Wildlife, & Marine Resources), and the Division of Lands & Forests. -
Bulletin of the United States Fish Commission
A LIMNOLOGICAL STUDY OF THE FINGER LAKES OF NEW YORK By Edward A. Birge and Chancey Juday Wisconsin Geological and Natural History Survey Madison, Wisconsin =========== ... _-_._._-_-----_... _---_.... _------=--__._.- Blank page retained for pagination CONTENTS. .:I- Page. Introduction. .. .. .. .. .. .. .. 529 Methods and authorities. ................................................................ 530 Topography and hydrography of the Finger Lakes district. .. .. .. .. 532 General account. ...................................................................... 532 Lakes of the Seneca Basin " "", ,. .. .. 539 Seneca and Cayuga Lakes. .. .. .. .. .. .... .. .. .. .. .. .. .... .. .... .. .. .. ....... 539 Owasco Like " , .. .. 540 Keuka Lake....................... 540 Canandaigua Lake. .. .. .. .. .. .. .. .. .. .. .. .. 54I Skaneateles Lake. .................................................................. 54I Otisco Lake. ...................................................................... 542 Lakes of the Genesee Basin...... .. .. .. ...... .. .... .. .. .. .. 543 Honeoye, Canadice, Hemlock, and Conesus Lakes. .. ....... 543 Temperatures " .. .. .. .. ... 546 General observations. ........ .. ........................................................ 546 Summer temperatures , .. .. .. 547 Surface and epilimnion ; ............................. 550 Thermocline... " ................................................. .. ............... 55I Hypolimnion. ...................................................................... 553 Winter temperatures