A Ravine's Web of Life
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Gills Coulee Creek, 2006 [PDF]
Wisconsin Department of Natural Resources Bureau of Watershed Management Sediment TMDL for Gills Coulee Creek INTRODUCTION Gills Coulee Creek is a tributary stream to the La Crosse River, located in La Crosse County in west central Wisconsin. (Figure A-1) The Wisconsin Department of Natural Resources (WDNR) placed the entire length of Gills Coulee Creek on the state’s 303(d) impaired waters list as low priority due to degraded habitat caused by excessive sedimentation. The Clean Water Act and US EPA regulations require that each state develop Total Maximum Daily Loads (TMDLs) for waters on the Section 303(d) list. The purpose of this TMDL is to identify load allocations and management actions that will help restore the biological integrity of the stream. Waterbody TMDL Impaired Existing Codified Pollutant Impairment Priority WBIC Name ID Stream Miles Use Use Gills Coulee 0-1 Cold II Degraded 1652300 168 WWFF Sediment High Creek 1-5 Cold III Habitat Table 1. Gills Coulee use designations, pollutants, and impairments PROBLEM STATEMENT Due to excessive sedimentation, Gills Coulee Creek is currently not meeting applicable narrative water quality criterion as defined in NR 102.04 (1); Wisconsin Administrative Code: “To preserve and enhance the quality of waters, standards are established to govern water management decisions. Practices attributable to municipal, industrial, commercial, domestic, agricultural, land development, or other activities shall be controlled so that all waters including mixing zone and effluent channels meet the following conditions at all times and under all flow conditions: (a) Substances that will cause objectionable deposits on the shore or in the bed of a body of water, shall not be present in such amounts as to interfere with public rights in waters of the state. -
Biodiversity Work Group Report: Appendices
Biodiversity Work Group Report: Appendices A: Initial List of Important Sites..................................................................................................... 2 B: An Annotated List of the Mammals of Albemarle County........................................................ 5 C: Birds ......................................................................................................................................... 18 An Annotated List of the Birds of Albemarle County.............................................................. 18 Bird Species Status Tables and Charts...................................................................................... 28 Species of Concern in Albemarle County............................................................................ 28 Trends in Observations of Species of Concern..................................................................... 30 D. Fish of Albemarle County........................................................................................................ 37 E. An Annotated Checklist of the Amphibians of Albemarle County.......................................... 41 F. An Annotated Checklist of the Reptiles of Albemarle County, Virginia................................. 45 G. Invertebrate Lists...................................................................................................................... 51 H. Flora of Albemarle County ...................................................................................................... 69 I. Rare -
Pleistocene Drainage Changes in Uncompahgre Plateau-Grand
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/32 Pleistocene drainage changes in Uncompahgre Plateau-Grand Valley region of western Colorado, including formation and abandonment of Unaweep Canyon: a hypothesis Scott Sinnock, 1981, pp. 127-136 in: Western Slope (Western Colorado), Epis, R. C.; Callender, J. F.; [eds.], New Mexico Geological Society 32nd Annual Fall Field Conference Guidebook, 337 p. This is one of many related papers that were included in the 1981 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States. -
Prairie Ridge Species Checklist 2018
Prairie Ridge Species Checklist Genus species Common Name Snails Philomycus carolinianus Carolina Mantleslug Gastrocopta contracta Bottleneck Snaggletooth Glyphalinia wheatleyi Bright Glyph Triodopsis hopetonensis Magnolia Threetooth Triodopsis juxtidens Atlantic Threetooth Triodopsis fallax Mimic Threetooth Ventridens cerinoideus Wax Dome Ventridens gularis Throaty Dome Anguispira fergusoni Tiger Snail Zonitoides arboreus Quick Gloss Deroceras reticulatum Gray Garden Slug Mesodon thyroidus White-lip Globe Slug Stenotrema stenotrema Inland Stiltmouth Melanoides tuberculatus Red-rim Melania Spiders Argiope aurantia Garden Spider Peucetia viridans Green Lynx Spider Phidippus putnami Jumping Spider Phidippus audax Jumping Spider Phidippus otiosus Jumping Spider Centipedes Hemiscolopendra marginata Scolopocryptops sexspinosus Scutigera coleoptrata Geophilomorpha Millipedes Pseudopolydesmus serratus Narceus americanus Oxidus gracilis Greenhouse Millipede Polydesmidae Crayfishes Cambarus “acuminatus complex” (= “species C”) Cambarus (Depressicambarus) latimanus Cambarus (Puncticambarus) (="species C) Damselflies Calopteryx maculata Ebony Jewelwing Lestes australis Southern Spreadwing Lestes rectangularis Slender Spreadwing Lestes vigilax Swamp Spreadwing Lestes inaequalis Elegant Spreadwing Enallagma doubledayi Atlantic Bluet Enallagma civile Familiar Bluet Enallagma aspersum Azure Bluet Enallagma exsulans Stream Bluet Enallegma signatum Orange Bluet Ischnura verticalis Eastern Forktail Ischnura posita Fragile Forktail Ischnura hastata Citrine -
A Comparison of Flooded Forest and Floating Meadow Fish Assemblages
Journal of Fish Biology (2008) 72, 629–644 doi:10.1111/j.1095-8649.2007.01752.x, available online at http://www.blackwell-synergy.com A comparison of flooded forest and floating meadow fish assemblages in an upper Amazon floodplain S. B. CORREA*†,W.G.R.CRAMPTON‡, L. J. CHAPMAN§k AND J. S. ALBERT{ *Zoology Department, University of Florida, 223 Bartram Hall, Gainesville, FL 32611–8525, U.S.A.,‡Department of Biology, University of Central Florida, Orlando, FL 32816-2368, U.S.A.,§McGill University, Biology Department, 1205 Avenue Docteur Penfield, Montreal, Quebec, H3A 1B1 Canada, kWildlife Conservation Society, 2300 Southern Boulevard, Bronx, NY 10460, U.S.A. and {Department of Biology, University of Louisiana at Lafayette, Lafayette, LA 70504-2451, U.S.A. (Received 31 August 2006, Accepted 20 October 2007) Matched sets of gillnets of different mesh-sizes were used to evaluate the degree to which contiguous and connected flooded forest and floating meadow habitats are characterized by distinct fish faunas during the flooding season in the Peruvian Amazon. For fishes between 38–740 mm standard length (LS) (the size range captured by the gear), an overriding pattern of faunal similarity emerged between these two habitats. The mean species richness, diversity, abundance, fish mass, mean and maximum LS, and maximum mass did not differ significantly between flooded forest and floating meadows. Species abundances followed a log-normal distribution in which three species accounted for 60–70% of the total abundance in each habitat. Despite these similarities, multivariate analyses demonstrated subtle differences in species composition between flooded forest and adjacent floating macrophytes. -
Ravine Sedge (Aka—Impressed- on the Same Stem; Each Spike with 5 - 11 Habitat Fragmentation, and Certain Forest Nerve Sedge) Fruits
U.S. Fish & Wildlife Service February 2019 Conserving South Carolina’s At-Risk Species: www.fws.gov/charleston www.fws.gov/southeast/endangered-species-act/at-risk-species Species facing threats to their survival Ravine sedge (aka—Impressed- on the same stem; each spike with 5 - 11 habitat fragmentation, and certain forest nerve sedge) fruits. The fruit body is about ⅛ inch long management practices. (Carex impressinervia) with a short, bent stalk and sharply bent tip, tightly enclosed in a 3-sided, heavily Management/Protection Needs veined sac. Few-fruited sedge (Carex oli- Protect hardwood slope forests and flood- gocarpa) is a similar species that also forms plain forests from clearing, logging, and dense clumps in rich forests but does not stream impoundment as the species tends have old leaf bases persisting at the base of to grow in transition zones between the the plant. Also, its leaf sheaths are purple floodplain and slope, making it particular- rather than light green. Ravine sedge, like ly vulnerable to changes in water levels. most sedges, are wind-pollinated. Little is Management primarily involves avoiding known about seed dispersal or other as- removal of the tree canopy and preventing pects of reproduction for this species. any activity that would change the hydrol- ogy of the ravines. Exotic species that Range invade forested area may need to be con- Ravine sedge is currently known from trolled on some sites. approximately 25 disjunct sites in Ala- bama, Mississippi, North Carolina, South Carolina, and possibly Georgia. In South Carolina, the plant is known only from a small tributary to Cuffeytown Creek in Greenwood County where it occurs with Dwarf palmetto (Sabal minor) and Ogle- thorpe oak (Quercus oglethorpensis). -
Westport, Connecticut Department of Public Works Town Hall, 110 Myrtle Avenue Westport, Connecticut 06880 (203) 341 1120
WESTPORT, CONNECTICUT DEPARTMENT OF PUBLIC WORKS TOWN HALL, 110 MYRTLE AVENUE WESTPORT, CONNECTICUT 06880 (203) 341 1120 MEMORANDUM Date: 04/08/2020 To: Conservation Commission From: Edward Gill, Engineer II Re: 222 Wilton Road, Appl. #IWW-10978-20 Reference Materials Reviewed: Application, Westport Conservation Commission, dated 03/12/2020. Plan prepared by J. Edwards & Associates, LLC entitled “Proposed Site Plan, Lot B, 222 Wilton Road, Westport, Connecticut,” dated 08/10/2015 as revised to 01/28/2016. Plan prepared by Brautigam Land Surveyors, P.C. entitled “Improvement Location Survey Prepared for FBCH CT Holdings LLC, 222 Westport – Wilton Road, Westport, Connecticut,” dated 01/15/2019. Plan prepared by Landtech entitled “Proposed Site Improvement Plan, Prepared for FBCH Holdings, LLC, 222 Wilton Road, Westport, CT,” dated 02/05/2020 as revised to 04/08/2020. Corresponding Stormwater Management Report dated 03/11/2020. Dear Conservation Commission: Our office has reviewed the proposed activity as depicted by the above referenced documents. Based on these criteria, we offer the following comments: 1. Project Description. The applicant is proposing to legalize changes to a previously approved permit for a single-family residence. These changes include construction of a patio and placement of significant fill within the 100-foot upland review setback from wetlands located on a neighboring property. The applicant is also proposing to remove a septic system installed within the 100-foot setback, construct a code complying system outside the setback, and remove a portion of the driveway previously approved for removal. 2. Flood & Erosion Control Board (FECB). The project will be subject to an administrative review from the associated staff. -
X. Chuckanut Creek SMA Summary: the Chuckanut Creek SMA Is 91.8 Acres in Size and Has Very Low Density Development, but Has the Potential for Significant Infill
X. Chuckanut Creek SMA Summary: The Chuckanut Creek SMA is 91.8 acres in size and has very low density development, but has the potential for significant infill. Infrastructure is limited within the SMA and a lack of sanitary sewer service to most the area currently limits growth. This SMA currently is functioning at high levels for most ecological parameters. Fecal coliform and dissolved oxygen levels have exceeded Washington State water quality parameters and their management should be a high priority for this SMA. Habitat quality is excellent throughout most this drainage and conservation is recommended. X.1 Watershed Analysis X.1.1 Landscape Setting The drainage is located at the northern toe of Chuckanut Mountain and approximately half the drainage occurs within the City limits. The Chuckanut Watershed is heavily forested and part of a large forested corridor that extends south to Blanchard Mountain. It is also of the only remaining forested corridor in Washington State that extends from the Cascade Mountains to the marine system. Chuckanut Creek flows within an incised ravine cut into continental sedimentary material and bedrock. The channel is naturally confined within the narrow ravine. The narrow nature of the ravine bottom is not conducive to channel migration to any significant extent. Squalicum-Chuckanut-Nati soils are the dominant soils types in this drainage. The soils can be generally described as moderately deep to very deep, moderately well drained, gently sloping to very steep soils, on foothills, plateaus and landslides. The side slopes of the ravine along most this SMA area range between 20% to 100%. -
Violent Crimes in Aid of Racketeering 18 U.S.C. § 1959 a Manual for Federal Prosecutors
Violent Crimes in Aid of Racketeering 18 U.S.C. § 1959 A Manual for Federal Prosecutors December 2006 Prepared by the Staff of the Organized Crime and Racketeering Section U.S. Department of Justice, Washington, DC 20005 (202) 514-3594 Frank J. Marine, Consultant Douglas E. Crow, Principal Deputy Chief Amy Chang Lee, Assistant Chief Robert C. Dalton Merv Hamburg Gregory C.J. Lisa Melissa Marquez-Oliver David J. Stander Catherine M. Weinstock Cover Design by Linda M. Baer PREFACE This manual is intended to assist federal prosecutors in the preparation and litigation of cases involving the Violent Crimes in Aid of Racketeering Statute, 18 U.S.C. § 1959. Prosecutors are encouraged to contact the Organized Crime and Racketeering Section (OCRS) early in the preparation of their case for advice and assistance. All pleadings alleging a violation of 18 U.S.C. § 1959 including any indictment, information, or criminal complaint, and a prosecution memorandum must be submitted to OCRS for review and approval before being filed with the court. The submission should be approved by the prosecutor’s office before being submitted to OCRS. Due to the volume of submissions received by OCRS, prosecutors should submit the proposal three weeks prior to the date final approval is needed. Prosecutors should contact OCRS regarding the status of the proposed submission before finally scheduling arrests or other time-sensitive actions relating to the submission. Moreover, prosecutors should refrain from finalizing any guilty plea agreement containing a Section 1959 charge until final approval has been obtained from OCRS. The policies and procedures set forth in this manual and elsewhere relating to 18 U.S.C. -
Great Glen Trails Special Use Permit Trail and Warming Hut Construction
United States Department of Agriculture Great Glen Trails Forest Special Use Permit Service Trail and Warming Hut August 2005 Construction Scoping Report Androscoggin Ranger District White Mountain National Forest Greens Grant Coos County, New Hampshire For Information Contact: Joe Gill Eastern Region Winter Sports Team Specialist Androscoggin Ranger District White Mountain National Forest 300 Glen Road Gorham, NH 03581 (603)466-2713, ext 221 FAX/TTY (603) 466-2856 www.fs.fed.us/r9/white or Susan Howle Interdisciplinary Team Leader Eastern Region Winter Sports Team 99 Ranger Road Rochester, VT 05767 (802)767-4261 ext 543 FAX/TTY (802)767-4777 Page 1 of 5 What is the Forest Service Proposing? The Androscoggin Ranger District of the White Mountain National Forest has received a special use permit application from Great Glen. They are proposing to construct and maintain 1.3 miles of cross-country ski trails and a warming hut approximately 20 feet by 20 feet. Great Glen feels that there is a need to expand their trail system to service the northern New Hampshire cross-country skiing population to offer more varied and challenging terrain and provide a more efficient trail system. All of the additional trail system and warming hut will occur inside their current trail system area (Figure 2). Background Great Glen Trails operates a Nordic ski area on lands conveyed by its parent company, the Mount Washington Summit Road Company (Auto Road), to the United States in 1993 (Figure 1). Upon conveyance, the Auto Road retained easements for a trail system. Several of these easements have proven to be impractical to construct without creating undesirable impacts on the natural resources in the area. -
! 1! a Millennium-Length Reconstruction of Bear River Stream Flow, Utah 1! 2
1! A millennium-length reconstruction of Bear River stream flow, Utah 2! 3! DeRose, R.J., USDA, Forest Service, Forest Inventory and Analysis, Rocky Mountain Research 4! Station, 507 25th Street Ogden, UT 84401, Email: [email protected], Phone: 801-625- 5! 5795 6! Bekker, M.F., Department of Geography, 690 SWKT, Brigham Young University, Provo, UT 7! 84602. 8! Wang, S.-Y., Plant, Soil, and Climate Department, 4820 Old Main Hill, Utah State University, 9! Logan, UT 84322-4820. 10! Buckley, B.M., Tree Ring Lab, Room 108, Lamont-Doherty Earth Observatory, Columbia 11! University, 61 Route 9W, Palisades, NY 10964 12! Kjelgren, R.K., Plant, Soil, and Climate Department, 4820 Old Main Hill, Utah State University, 13! Logan, UT 84322-4820. 14! Bardsley, T, Western Water Assessment, 2242 West North Temple, Salt Lake City, UT 84116. 15! Rittenour, T.M., Department of Geology, 4505 Old Main Hill, Utah State University, Logan, UT 16! 84322-4505. 17! Allen, E.B., United States Geological Survey, 4200 New Haven Road, Columbia, MO 65201. 18! 19! 1! ! 20! Abstract: The Bear River contributes more water to the eastern Great Basin than any other river 21! system. It is also the most significant source of water for the burgeoning Wasatch Front 22! metropolitan area in Northern Utah. Despite its importance for water resources for the region’s 23! agricultural, urban, and wildlife needs, our understanding of the variability of Bear River’s 24! stream flow derives entirely from the short instrumental record (1943-2010). Here we present a 25! 1,200-year calibrated and verified tree-ring reconstruction of stream flow for the Bear River that 26! explains 67% of the variance of the instrumental record over the period from 1943-2010. -
Riparian Forest, Aquatic Habitat, and Vertebrate Influences on Macroinvertebrate Assemblages in Headwater Streams of Northeast Ohio Kathryn L
Riparian Forest, Aquatic Habitat, and Vertebrate Influences on Macroinvertebrate Assemblages in Headwater Streams of Northeast Ohio Kathryn L. Holmes, P. Charles Goebel, Lance R. Williams, Marie Schrecengost School of Environment and Natural Resources, Ohio Agricultural Research and Development Center, The Ohio State University Introduction Riparian Forest Species- Environment Relationships It has long been recognized that streams and rivers are integrally tied to terrestrial riparian Transects were established perpendicular to stream-flow across the stream We used canonical correspondence analysis (CCA), to examine the relationships areas (Minshall 1967). Especially in headwaters, stream biota are dependent on allochthonous valley at 33, 66, and 100 m within each reach. For each transect, circular between relative abundance of macroinvertebrate families and functional feeding inputs from surrounding riparian corridors for nutrients and habitat (Vannote et al. 1980). plots (400m2) were centered on riparian geomorphic landforms (e.g. guilds and environmental factors. CCA is comparable to multiple regression, where Headwater streams (typically defined as draining < 13 km2 watershed area) comprise up to floodplain, terrace, valley toe-slope) and all tree stems greater than 10 cm “species” are dependent variables and constrained by measured environmental 80% of a watershed’s stream network (Meyer et al. 2003). These small streams should be the DBH (diameter at breast height= 1.35 m) were identified and measured. factors, which serve as independent variables. Three separate CCAs were focus of restoration efforts because of their potential importance for diversity (Vannote et al. Using a concave spherical densiometer, riparian canopy cover was conducted for families and feeding guilds, one for each group of environmental 1980) and nutrient processing (Peterson et al.