Massachusetts Estuaries Project
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Disappearing Kettle Ponds Reveal a Drying Kenai Peninsula by Ed Berg
Refuge Notebook • Vol. 3, No. 38 • October 12, 2001 Disappearing kettle ponds reveal a drying Kenai Peninsula by Ed Berg A typical transect starts at the forest edge, passes through a grass (Calamagrostis) zone, into Sphagnum peat moss, and then into wet sedges, sometimes with pools of standing water, and then back through these same zones on the other side of the kettle. Three of the four kettles we surveyed this summer were quite wet in the middle (especially after the July rains), and we had to wear hip boots. These plots can be resurveyed in future decades and, if I am correct, they will show a succession of drier and drier plants as the water table drops lower and lower, due to warmer summers and increased evap- Photo of a kettle pond by the National Park Service. otranspiration. If I am wrong, and the climate trend turns around toward cooler and wetter, these plots will When the glaciers left the Soldotna-Sterling area be under water again, as they were on the old aerial some 14,000 years ago, the glacier fronts didn’t re- photos. cede smoothly like their modern descendants, such as By far the most striking feature that we have Portage or Skilak glaciers. observed in the kettles is a band of young spruce Rather, the flat-lying ice sheets broke up into nu- seedlings popping up in the grass zones. These merous blocks, which became partially buried in hilly seedlings can form a halo around the perimeter of a moraines and flat outwash plains. In time these gi- kettle. -
A Survey of the Nation's Lakes
A Survey of the Nation’s Lakes – EPA’s National Lake Assessment and Survey of Vermont Lakes Vermont Agency of Natural Resources Department of Environmental Conservation - Water Quality Division 103 South Main 10N Waterbury VT 05671-0408 www.vtwaterquality.org Prepared by Julia Larouche, Environmental Technician II January 2009 Table of Contents List of Tables and Figures........................................................................................................................................................................... ii Introduction................................................................................................................................................................................................. 1 What We Measured..................................................................................................................................................................................... 4 Water Quality and Trophic Status Indicators.......................................................................................................................................... 4 Acidification Indicator............................................................................................................................................................................ 4 Ecological Integrity Indicators................................................................................................................................................................ 4 Nearshore Habitat Indicators -
Moe Pond Limnology and Fisii Population Biology: an Ecosystem Approach
MOE POND LIMNOLOGY AND FISII POPULATION BIOLOGY: AN ECOSYSTEM APPROACH C. Mead McCoy, C. P.Madenjian, J. V. Adall1s, W. N. I-Iannan, D. M. Warner, M. F. Albright, and L. P. Sohacki BIOLOGICAL FIELD STArrION COOPERSTOWN, NEW YORK Occasional Paper No. 33 January 2000 STATE UNIVERSITY COLLEGE AT ONEONTA ACKNOWLEDGMENTS I wish to express my gratitude to the members of my graduate committee: Willard Harman, Leonard Sohacki and Bruce Dayton for their comments in the preparation of this manuscript; and for the patience and understanding they exhibited w~lile I was their student. ·1 want to also thank Matthew Albright for his skills in quantitative analyses of total phosphorous and nitrite/nitrate-N conducted on water samples collected from Moe Pond during this study. I thank David Ramsey for his friendship and assistance in discussing chlorophyll a methodology. To all the SUNY Oneonta BFS interns who lent-a-hand during the Moe Pond field work of 1994 and 1995, I thank you for your efforts and trust that the spine wounds suffered were not in vain. To all those at USGS Great Lakes Science Center who supported my efforts through encouragement and facilities - Jerrine Nichols, Douglas Wilcox, Bruce Manny, James Hickey and Nancy Milton, I thank all of you. Also to Donald Schloesser, with whom I share an office, I would like to thank you for your many helpful suggestions concerning the estimation of primary production in aquatic systems. In particular, I wish to express my appreciation to Charles Madenjian and Jean Adams for their combined quantitative prowess, insight and direction in data analyses and their friendship. -
RIPARIAN AREASAREAS Updatedupdated June 21, 2012
RIPARIAN AREASAREAS UpdatedUpdated June 21, 2012 A 2012 Critical Areas Update Fact Sheet THE ROLE OF RIPARIAN AREAS Some of our most valuable habitat for the diverse Trees that fall into the wildlife in Thurston County – “riparian habitat” – is water form sheltered pools found along water bodies such as rivers, streams, where fi sh can lay eggs. lakes and marine (salt water) shorelines. In the past, The trees and pools also these areas have been referred to as buffers, and the supply insects and organic terms are still used interchangeably in some cases. materials for the aquatic food chain. Approximately Riparian habitat refers to the transitional areas 90 percent of all wildlife use between the upland environment and the water. riparian areas for part or all Riparian habitats moderate the temperature of water of their life cycles. bodies, help prevent erosion, and provide a home for many types of animals and vegetation. Although Potential amendments to the Critical Areas Ordinance riparian areas are located alongside the water, they seek to protect habitat and healthy functioning also provide habitat within the water. ecosystems in order to support viable populations of fi sh and wildlife in Thurston County. ABOUT WATER TYPE CLASSIFICATIONS Like the existing Critical Areas Ordinance, the The DNR classifi cations are: potential amendments would set riparian areas according to how the streams and water bodies • Type S: Streams and water bodies that are are classifi ed or “typed” by the state Department designated “Shorelines of the State” as defi ned in of Natural Resources. The water types are based chapter 90.58.030 RCW. -
Hogback Trail Greenfield State Park Greenfield, New Hampshire
Hogback Trail Greenfield State Park Greenfield, New Hampshire Self-Guided Hike 1. The Hogback Trail is 1.2 miles long and relatively flat. It will take you approximately 45 minutes to go around the pond. As you walk, keep an eye out for the abundant wildlife and unique plants that are in this secluded area of the park. Throughout the trail, there are numbered stations that correspond to this guide and benches to rest upon. Practice “Leave No Trace” on your hike; Take only photographs, leave only footprints. 2. Hogback Pond is a glacial kettle pond formed when massive chunks of Stop #5: ridge is an example of glacial esker ice were buried in the sand, then slowly melted leaving a huge depression in the landscape that eventually filled with water. Kettle ponds generally have no streams running into them or out of them, resulting in a still body of water. Water in the pond is replenished by rain and is acidic, prohibiting many common wetland species from flourishing. 3. The blueberry bushes around Hogback Pond and throughout Greenfield State Park are two species; low-bush and high-bush. Many animals such as Black Bear and several species of birds seek out these berries as an important summer food source. Between Stops #2 & 3: example of unique vegetation found on kettle ponds 4. The Eastern Hemlocks that you see around you are one of the several varieties of evergreen that grow around Hogback Pond. This slow- growing, long-lived tree grows well in the shade. They have numerous short needles spreading directly from the branches in one flat layer. -
Analyzing Trends of Dike-Ponds Between 1978 and 2016 Using Multi-Source Remote Sensing Images in Shunde District of South China
sustainability Article Analyzing Trends of Dike-Ponds between 1978 and 2016 Using Multi-Source Remote Sensing Images in Shunde District of South China Fengshou Li 1, Kai Liu 1,* , Huanli Tang 2, Lin Liu 3,4,* and Hongxing Liu 4,5 1 Guangdong Key Laboratory for Urbanization and Geo-simulation, Guangdong Provincial Engineering Research Center for Public Security and Disaster, School of Geography and Planning, Sun Yat-Sen University, Guangzhou 510275, China; [email protected] 2 Guangzhou Zengcheng District Urban and Rural Planning and Surveying and Mapping Geographic Information Institute, Guangzhou 511300, China; [email protected] 3 Center of Geo-Informatics for Public Security, School of Geographic Sciences, Guangzhou University, Guangzhou 510006, China 4 Department of Geography and Geographic Information Science, University of Cincinnati, Cincinnati, OH 45221, USA; [email protected] 5 Department of Geography, the University of Alabama, Tuscaloosa, AL 35487, USA * Correspondence: [email protected] (K.L.); [email protected] (L.L.); Tel.: +86-020-8411-3044 (K.L.); +1-513-556-3429 (L.L.); Fax: +86-020-8411-3057 (K.L. & L.L.) Received: 27 August 2018; Accepted: 26 September 2018; Published: 30 September 2018 Abstract: Dike-ponds have experienced significant changes in the Pearl River Delta region over the past several decades, especially since China’s economic reform, which has seriously affected the construction of ecological environments. In order to monitor the evolution of dike-ponds, in this study we use multi-source remote sensing images from 1978 to 2016 to extract dike-ponds in several periods using the nearest neighbor classification method. -
The Fishes Found in the Vicinity of Woods Hole
U. S. COMMISSION OF FISH AND FISHERIES. JOHN J. BRICE, Commissioner. THE FISHES FOUND IN THE VICINITY OF \VOODS HOLE. BY HUGH M. SMITH, Chief of Division of Scientific Inquiry, U. S. Fisk Commission. Ennwted li'OIII 0.8. FIsh CommiaslOD Bulletin for 1897. Article 3, Pages 86 to 11 .P1&te 3, and 1 ~ Spt Da~ of pnbliCl&t1ou, lunary 6,1898. UOf·1'1 WASHINGTON: GOVERNMENT PRINTING Oll'll'ICB. 1898. PLATE S. o , r A N .Dlgltized by Google LATE 3. 3.-THE FISHES FOUND IN THE ,vICINITY OF WOODS HOLE. BY HUGH M. SMITH, Ckief of Division of Scientific Inquiry, U. S. Fisk Ctmtmission. Since the establishment of the United States Commission of Fish and Fisheries in 1871, systematic fish collecting has boon carried on at Woods Hole, MlUlsachusetts, by Commission assistants. In the year named, l'rof. Spencer F. Baird studied the fish fauna of the region and later pnblished a list of the specIes then observed which has served as a valuable guide in subsequent investigation. For more than a quarter of a century almost daily observations, based on collec· tions, have been made and recorded, and it may be safely asserted that nowhere else iu the United States has such long-continued and comprehensive work of this char acter been done. The duty of collecting specimens and recordin~ information has fallen chiefly to the lot of :Mr. Vinal N. Edwards, of the Fish Commission, to whose assiduous labors the principal additions to the fish fauna are due. The collection of specimens hal'! been done chiefly with fine-meshed bag seines, about 150 feet long, hauled from the shore in harbors and coves and on the beaches in Vineyard Sound anrl Buzzards Bay. -
Weather Conditions and Currents in Vineyard Sound for the Sonar Worlds
Weather Conditions and Currents in Vineyard Sound for the Sonar Worlds by Rocky Geyer, Woods Hole Oceanographic Inst. and Falmouth Y.C. Cape Cod is famous for moderate temperatures, strong sea breezes and strong tidal currents. The sea breeze is due to the southward orientation of the shoreline, which means that the thermally induced sea breeze is nearly aligned with the prevailing southwesterly gradient wind. This pattern is most common in July and August, when the Bermuda High is strongest. In September, the sea breeze still occurs, but the differential between air and water temperatures is diminished and the Bermuda High is sometimes displaced by weak frontal systems. Southwesterlies are still the most common winds, but they are not typically as strong as mid-summer conditions. Here are the statistics on the wind conditions at Vineyard Haven, several miles from the race course: Average high air temp: 70-72 F (20-22 C) Average low air temp: 54-62 F (12-17 C) Average water temp: 68 F (20 C) Winds: 50% daily peak wind speeds >15 mph (13 kts) 12% daily peak wind speeds >20 mph (17 kts) 50% SSW-W 25% WNW-N 25% N-E The southwesterlies are the steadiest, as they are relatively unobstructed by land and tend to be associated with stable atmospheric conditions. Northwesterlies are puffy and shifty, just like most of the East Coast. Easterlies are also shifty, for reasons that I do not understand. Tidal currents are strong in Vineyard Sound, and particular attention should be paid to the times of slack and maximum currents, as they will have a major infuence on the positions of laylines. -
Des Moines Lobe Retreated North- What It Means to Be Minnesotan
Route Map Geology of the Carleton College Esri, HERE, DeLorme, MapmyIndia, © OpenStreetMap contributors, and the GIS ¯ user community 1 Cannon River Cowling Arboretum 2 Glacial Landscapes 3 Glacial Erratics 4 Local Bedrock A Guided Tour 5 Kettle Hole Marsh College BoundaryH - Back IA Parking Glacial Erratic Cannon River Tour Route Other Trails 0250 500 1 000 Feet, 5 HWY 3 4 LOWER ARBORETUM 3 2 H IA 1 Arb Office HWY 19 UPPER Tunnel IA ARBORETUM under Hwy 19 Lower Lyman Recreation IA Center HALL AVE HALL West IA Gym Library Published 5/2016 Product of the Carleton College Cowling Arboretum. For more information visit our website: apps.carleton.edu/campus/arb or contact us at (507)-222-4543 Introduction Hello and welcome to Carleton College’s Cowling Arboretum. This 1 800 acre natural area, owned and managed by Carleton, has long been one of the most beloved parts of Carleton for students, faculty and community members alike. Although the Arb is best known for its prairie ecosystem, an amazing history full of thundering riv- ers, massive glaciers, and the journeys of massive boulders lies just below the surface. This geologic history of the Arb is a fascinating story and one that you can experience for yourself by following this 2 self-guided tour. I hope it’s a beautiful day for a walk hope and that you enjoy learning about the geology of the Arb as much as I did. The route for this tour is about three miles long and will take you 1-2 hours to complete, depending on your walking speed. -
Coastal Resources Element 2.2
Coastal Resources Element 2.2 Inventory The Coastal Resources inventory identifies and summarizes a variety of Falmouth’s beaches, coastal banks, shellfish beds, commercial waterfronts, harbors, access points and coastal facilities. Detailed and specific coastal resource information, such as the Shellfish Management Plan and The Future of Falmouth’s South Shore, are found in various Town Hall departments. Shellfish Beds & Habitat Areas The majority of Falmouth’s tidal ponds and rivers are seasonally approved for the harvest of shellfish from November thru April on an annual basis, with each water-body having various quantities of quality shellfish habitat. Areas open for year-round harvest vary from year to year and are more limited in scope, but typically consist of locations in Waquoit Bay, Bournes Pond, Little Harbor (Woods Hole), Great Harbor (Woods Hole), Quissett Harbor and Megansett Harbor. Shellfish resource habitat maps highlight these water-bodies and are available at the Town of Falmouth Shellfish Department and the Conservation Commission office. The significant shellfish habitat areas are as follows: The Megansett Harbor area (1,049 acres) has significant populations of seeded quahogs, clams and oysters as well as occasional populations of bay scallops. West Falmouth Harbor (201 acres) is a significant resource for quahogs, soft-shell clams, oysters and scallops. The scallop population has been recently improved due to a local scallop program executed by the Shellfish Constable. Great Sippewissett Marsh (29 acres) has pockets of clams and quahogs, but has been experiencing degradation in water quality from runoff and septic systems, which has led to a prohibition on shellfishing. -
Waquoit Bay: Prehistory, History, and Natural History by Nancy Church
20 Waquoit Bay: Prehistory, History, and Natural History by Nancy Church Ellen Little and her brother Edward fshing from the beach on Washburn Island in the 1890s. Photo possibly by Edith Little. Courtesy D. W. Bourne. (Reprinted from Te Book of Falmouth.) Anniversaries are milestones and cause for celebration Research Reserve System. WBNERR uses the local and refection. 2013 marks the 25th Anniversary of estuary system as a living laboratory to conduct the creation of the Waquoit Bay National Estuarine and support research and to educate community Research Reserve (WBNERR), an organization members and decision makers across the region. Im- which manages almost 3,000 acres of land and water provements to the headquarters are underway now. in the towns of Mashpee and Falmouth. Work to Tis is an ideal time to revisit the long history of hu- establish the Reserve frst began in 1974 yet it wasn’t man activity around the Bay and the Reserve’s role in until 1988 that the deal was complete and Waquoit protecting coastal resources for future generations. Bay Reserve became part of the National Estuarine Te Reserve is a state and federal partnership between 20 21 the Massachusetts Department of Conservation and across the Cape with increased settlement over time, Recreation (DCR) and the National Oceanic and especially during the Woodland period 1500 to Atmospheric Administration (NOAA). It consists of 1,100 years ago when Native people lived in small the Headquarters and Visitor Center on the former villages or seasonal camps near abundant fresh and Sargent/Swift Estate, the 300 acre Washburn Island, salt water resources. -
Chapter One the Vision of A
Oak Ridges Trail Association 1992 - 2017 The Vision of a Moraine-wide Hiking Trail Chapter One CHAPTER ONE The Oak Ridges Moraine is defined by a sub-surface geologic formation. It is evident as a 170 km long ridge, a watershed divide between Lake Ontario to the south and Lake Simcoe, Lake Scugog and Rice Lake to the north. Prior to most THE VISION OF A MORAINE-WIDE HIKING TRAIL being harvested, Red Oak trees flourished along the ridge – hence its name. Appended to this chapter is an account of the Moraine’s formation, nature and Where and What is the Oak Ridges Moraine? history written by two Founding Members of the Oak Ridges Trail Association. 1 Unlike the Niagara Escarpment, the Oak Ridges Moraine is not immediately observed when travelling through the region. During the 1990s when the Oak The Seeds of the Vision Ridges Moraine became a news item most people in the Greater Toronto Area had no idea where it was. Even local residents and visitors who enjoyed its From the 1960s as the population and industrialization of Ontario, particularly particularly beautiful landscape characterized by steep rolling hills and substantial around the Golden Horseshoe from Oshawa to Hamilton grew rapidly, there was forests had little knowledge of its boundaries or its significance as a watershed. an increasing awareness of the stress this placed on the environment, particularly on the congested Toronto Waterfront and the western shore of Lake Ontario. The vision of a public footpath that would span the entire Niagara Escarpment - the Bruce Trail - came about in 1959 out of a meeting between Ray Lowes and Robert Bateman of the Federation of Ontario Naturalists.