Guidebook for Hydrogeomorphic (HGM)–Based Assessment of Oregon Wetland and Riparian Sites: Statewide Classification and Profiles
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Revegetation Strategies for Rangelands
Revegetation Strategies for Rangelands Russellagri.nv.gov Wilhelm, Seed Program Manager January 7, 2021 About the Presenter • Russ Wilhelm • Seed Program Manager at Nevada Dept. of Agriculture – Since January 2015 • Graduate from University of Nevada, Reno • Been working intensively with native seed in NV for past 4 years agri.nv.gov Synopsis of Presentation Martin Fire, 2018 – High Country News 440,000 acres burnt Restoration of rangelands throughout the intermountain West has been an excitedly discussed topic for centuries. New strategies are on the rise throughout the West that will help promote rangeland health and longevity, while assisting to suppress wildfire intensity and decrease frequency. Martin Reseeding - USFWS Photo taken by SKulpa Several revegetation methods and new reseeding technologies will be investigated and the use of locally adapted, genetically appropriate, seed will be the focal point. agri.nv.gov Primary Reasons for Rangeland Restoration Wildfire Mining reclamation rehabilitation Preventing spread Erosion control of invasive species Preserving wildlife Many, many more… habitat agri.nv.gov Common Restoration Methods Revegetation Grazing Management The use of plant propagules Controlling grazing habits of livestock or game to decrease (seed), native or non-native, the level of disturbance to a to reintroduce desirable landscape. species to a disturbed site. Ex. Implementing stockmanship Ex. Designing an herbicide protected principles to effectively rotate livestock seed mix, to re-apply to a burn site. across allotments. Invasive Species Inventory & Monitoring Management Assessing the conditions of an Preventing the introduction or area to determine the needs spread of undesirable species and strategize on control to a vulnerable site. methods. -
Bioenergy Harvest, Climate Change, and Forest Carbon in the Oregon Coast Range
Portland State University PDXScholar Environmental Science and Management Faculty Publications and Presentations Environmental Science and Management 3-2016 Bioenergy Harvest, Climate Change, and Forest Carbon in the Oregon Coast Range Megan K. Creutzburg Portland State University, [email protected] Robert M. Scheller Portland State University, [email protected] Melissa S. Lucash Portland State University, [email protected] Louisa B. Evers Bureau of Land Management Stephen D. LeDuc United States Environmental Protection Agency See next page for additional authors Follow this and additional works at: https://pdxscholar.library.pdx.edu/esm_fac Part of the Forest Biology Commons Let us know how access to this document benefits ou.y Citation Details Creutzburg, M. K., Scheller, R. M., Lucash, M. S., Evers, L. B., LeDuc, S. D., & Johnson, M. G. (2015). Bioenergy harvest, climate change, and forest carbon in the Oregon Coast Range. GCB Bioenergy. This Article is brought to you for free and open access. It has been accepted for inclusion in Environmental Science and Management Faculty Publications and Presentations by an authorized administrator of PDXScholar. Please contact us if we can make this document more accessible: [email protected]. Authors Megan K. Creutzburg, Robert M. Scheller, Melissa S. Lucash, Louisa B. Evers, Stephen D. LeDuc, and Mark G. Johnson This article is available at PDXScholar: https://pdxscholar.library.pdx.edu/esm_fac/118 GCB Bioenergy (2016) 8, 357–370, doi: 10.1111/gcbb.12255 Bioenergy harvest, climate change, and forest carbon in the Oregon Coast Range MEGAN K. CREUTZBURG1 , ROBERT M. SCHELLER1 , MELISSA S. LUCASH1 , LOUISA B. EVERS2 , STEPHEN D. LEDUC3 and MARK G. -
The Oregon Coast Range- Considerations for Ecological Restoration Joe Means Tom Spies Shu-Huei Chen Jane Kertis Pete Teensma
Forests of the Oregon Coast Range- Considerations for Ecological Restoration Joe Means Tom Spies Shu-huei Chen Jane Kertis Pete Teensma The Oregon Coast Range supports some of the most dense Ocean, so they are warm and often highly productive, com- and productive forests in North America. In the pre-harvest- pared to the Cascade Range and central Oregon forests. ing period these forests arose as a result of large fires-the Isaac's (1949) site index map shows much more site class I largest covering 330,000 ha (Teensma and others 1991). and I1 land in the Coast Range than in the Cascades. In the These fires occurred mostly at intervals of 150 to 300 years. summers, humid maritime air creates a moisture gradient The natural disturbance regime supported a diverse fauna from the coastal western hemlock-Sitka spruce (Tsuga and large populations of anadromous salmonids (salmon heterophylla-Piceasitchensis) zone with periodic fog extend- and related fish). In contrast, the present disturbance re- ing 4 to 10 km inland, through Douglas-fir (Pseudotsuga gime is dominated by patch clearcuts of about 10-30 ha menziesii var. rnenziesii)-western hemlock forests in the superimposed on most of the forest land with agriculture on central zone to the drier interior-valley foothill zone of the flats near rivers. Ages of most managed forests are less Douglas-fir, bigleaf maple (Acer rnacrophyllum)and Oregon than 60 years. This logging has coincided with significant oak (Quercus garryana). declines in suitable habitat and populations of some fish and wildlife species. Some of these species have been nearly extirpated. -
Mill Creek Watershed Assessment
Yamhill Basin Council Mill Watershed Assessment December 30, 1999 Funding for the Mill Assessment was provided by the Oregon Watershed Enhancement Board and Resource Assistance for Rural Environments. Mill Assessment Project Manager: Robert J. Bower, Principal Author Co-authors: Chris Lupoli, Linfield College intern, for Riparian section and assisted with Wetlands Conditions section. Tamara Quandt, Linfield College intern, for Sensitive Species section. Editors: Melissa Leoni, Yamhill Basin Council, McMinnville, OR Alison Bower, Forest Ecologist, Corvallis, OR Contributors: Bill Ferber, Salem, Water Resources Department (WRD) Chester Novak, Salem, Bureau Land Management (BLM) Dan Upton, Dallas, Willamette Industries David Anderson, Monmouth, Boise Cascade Dean Anderson, Dallas, Polk County Geographical Information Systems (GIS) Dennis Ades, Salem, Department of Environmental Quality (DEQ) Gary Galovich, Corvallis, Oregon Department Fish and Wildlife (ODFW) Mark Koski, Salem, Bureau of Land Management (BLM) Patrick Hawe, Salem, Bureau of Land Management (BLM) Rob Tracey, McMinnville, Natural Resource and Conservation Service (NRCS) Stan Christensen, McMinnville, Yamhill Soil Water Conservation District Susan Maleki, Corvallis, Oregon Watershed Enhancement Board (OWEB) Warren Tausch, Tillamook Bureau of Land Management (BLM) Special Thanks: ! John Cruickshank, Gooseneck Creek resident for his assistance with the Historical, and Channel Modification sections and in the gathering of historical photographs. ! Gooseneck Creek Watershed Group for their support and guidance. ! John Caputo, Yamhill County GIS. ! BLM and Polk County GIS for providing some of the GIS base layers used to create the maps in this assessment. ! USDA Service Center, Natural Resource Conservation Service, McMinnville, for copying and office support. ! Polk and Yamhill Soil and Water Conservation Districts. ! Nick Varnum, PNG Environmental Inc., Tigard, for assisting with the Hydrology and Channel Habitat Typing sections. -
Land Cover Change Along the Willamette River, Oregon
AN ABSTRACT OF THE THESIS OF Doug R. Oetter for the degree of Doctor of Philosophy in Geography presented on August 16, 2002. Title: Land CoverChange along the Willamette River, Oregon. Abstract approved: A. Jon Kimerling The Willamette River and its floodplain in northwest Oregon have changed dramatically since European settlement. At one time, the river was a vast complex system of braided channels with a broad floodplain forest; it has now been simplified by channelization and dams, and the forest has been removed to support agricultural and urban expansion. This thesis presents three research manuscripts, each of which uses remote sensing and Geographical Information System methods to capture the dynamic nature of land along the Willamette River. In the first article, the river and its floodplain were mapped at four time periods, ranging from pre-settlement to modern day. The paper reports that the river system has been greatly simplified, and the floodplain has lost much of its original forest. An overlay technique was used to identify potential floodplain restoration sites. The second paper details the creation of a landcover map for the Willamette Valley, which shows that the largest portion of the floodplain is now in agriculture, with a significant amount in a built condition. The third manuscript outlines a methodology for detecting land cover change along the river during a twenty-year period that coincides with the implementation of the Willamette River Greenway, a land use designation designed to restrict riparian land conversion. It shows that regressive change is still occuring along the river, although not at thesame rate asoutside the greenway. -
The District of Columbia Water Quality Assessment
THE DISTRICT OF COLUMBIA WATER QUALITY ASSESSMENT 2008 INTEGRATED REPORT TO THE ENVIRONMENTAL PROTECTION AGENCY AND U.S. CONGRESS PURSUANT TO SECTIONS 305(b) AND 303(d) CLEAN WATER ACT (P.L. 97-117) District Department of the Environment Natural Resources Administration Water Quality Division Government of the District of Columbia Adrian M. Fenty, Mayor PREFACE PREFACE The Water Quality Division of the District of Columbia's District Department of the Environment, Natural Resources Administration, prepared this report to satisfy the listing requirements of §303(d) and the reporting requirements of §305(b) of the federal Clean Water Act (P.L. 97-117). This report provides water quality information on the District of Columbia’s surface and ground waters that were assessed during 2008 and updates the water quality information required by law. Various programs in the Natural Resources Administration contributed to this report including the Fisheries and Wildlife Division and the Watershed Protection Division. Questions or comments regarding this report or requests for copies should be forwarded to the address below. The District of Columbia Government District Department of the Environment Natural Resources Administration Water Quality Division 51 N St., NE Washington, D.C. 20002-3323 Attention: N. Shulterbrandt ii TABLE OF CONTENTS TABLE OF CONTENTS PREFACE ................................................................... ii TABLE OF CONTENTS........................................................iii LIST OF TABLES........................................................... -
"Preserve Analysis : Saddle Mountain"
PRESERVE ANALYSIS: SADDLE MOUNTAIN Pre pare d by PAUL B. ALABACK ROB ERT E. FRENKE L OREGON NATURAL AREA PRESERVES ADVISORY COMMITTEE to the STATE LAND BOARD Salem. Oregon October, 1978 NATURAL AREA PRESERVES ADVISORY COMMITTEE to the STATE LAND BOARD Robert Straub Nonna Paul us Governor Clay Myers Secretary of State State Treasurer Members Robert Frenkel (Chairman), Corvallis Bill Burley (Vice Chainnan), Siletz Charles Collins, Roseburg Bruce Nolf, Bend Patricia Harris, Eugene Jean L. Siddall, Lake Oswego Ex-Officio Members Bob Maben Wi 11 i am S. Phe 1ps Department of Fish and Wildlife State Forestry Department Peter Bond J. Morris Johnson State Parks and Recreation Branch State System of Higher Education PRESERVE ANALYSIS: SADDLE MOUNTAIN prepared by Paul B. Alaback and Robert E. Frenkel Oregon Natural Area Preserves Advisory Committee to the State Land Board Salem, Oregon October, 1978 ----------- ------- iii PREFACE The purpose of this preserve analysis is to assemble and document the significant natural values of Saddle Mountain State Park to aid in deciding whether to recommend the dedication of a portion of Saddle r10untain State Park as a natural area preserve within the Oregon System of I~atural Areas. Preserve management, agency agreements, and manage ment planning are therefore not a function of this document. Because of the outstanding assemblage of wildflowers, many of which are rare, Saddle r·1ountain has long been a mecca for· botanists. It was from Oregon's botanists that the Committee initially received its first documentation of the natural area values of Saddle Mountain. Several Committee members and others contributed to the report through survey and documentation. -
Geologic History of Siletzia, a Large Igneous Province in the Oregon And
Geologic history of Siletzia, a large igneous province in the Oregon and Washington Coast Range: Correlation to the geomagnetic polarity time scale and implications for a long-lived Yellowstone hotspot Wells, R., Bukry, D., Friedman, R., Pyle, D., Duncan, R., Haeussler, P., & Wooden, J. (2014). Geologic history of Siletzia, a large igneous province in the Oregon and Washington Coast Range: Correlation to the geomagnetic polarity time scale and implications for a long-lived Yellowstone hotspot. Geosphere, 10 (4), 692-719. doi:10.1130/GES01018.1 10.1130/GES01018.1 Geological Society of America Version of Record http://cdss.library.oregonstate.edu/sa-termsofuse Downloaded from geosphere.gsapubs.org on September 10, 2014 Geologic history of Siletzia, a large igneous province in the Oregon and Washington Coast Range: Correlation to the geomagnetic polarity time scale and implications for a long-lived Yellowstone hotspot Ray Wells1, David Bukry1, Richard Friedman2, Doug Pyle3, Robert Duncan4, Peter Haeussler5, and Joe Wooden6 1U.S. Geological Survey, 345 Middlefi eld Road, Menlo Park, California 94025-3561, USA 2Pacifi c Centre for Isotopic and Geochemical Research, Department of Earth, Ocean and Atmospheric Sciences, 6339 Stores Road, University of British Columbia, Vancouver, BC V6T 1Z4, Canada 3Department of Geology and Geophysics, University of Hawaii at Manoa, 1680 East West Road, Honolulu, Hawaii 96822, USA 4College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, 104 CEOAS Administration Building, Corvallis, Oregon 97331-5503, USA 5U.S. Geological Survey, 4210 University Drive, Anchorage, Alaska 99508-4626, USA 6School of Earth Sciences, Stanford University, 397 Panama Mall Mitchell Building 101, Stanford, California 94305-2210, USA ABSTRACT frames, the Yellowstone hotspot (YHS) is on southern Vancouver Island (Canada) to Rose- or near an inferred northeast-striking Kula- burg, Oregon (Fig. -
The District of Columbia Water Quality Assessment
THE DISTRICT OF COLUMBIA WATER QUALITY ASSESSMENT 2012 INTEGRATED REPORT TO THE US ENVIRONMENTAL PROTECTION AGENCY AND CONGRESS PURSUANT TO SECTIONS 305(b) AND 303(d) CLEAN WATER ACT (P.L. 97-117) District Department of the Environment Natural Resources Administration Water Quality Division i PREFACE The Water Quality Division of the District of Columbia's District Department of the Environment, Natural Resources Administration, prepared this report to satisfy the listing requirements of §303(d) and the reporting requirements of §305(b) of the federal Clean Water Act (P.L. 97-117). The report provides water quality information on the District of Columbia’s surface and ground waters that were assessed during 2010-2011 and updates the water quality information required by law. Various programs in the Natural Resources Administration contributed to this report including the Fisheries and Wildlife Division, the Stormwater Management Division, and the Watershed Protection Division. The Lead and Healthy Housing Division, Environmental Protection Administration also contributed to this report. Questions or comments regarding this report should be forwarded to the address below. The District of Columbia Government District Department of the Environment Natural Resources Administration Water Quality Division 1200 First Street, NE 5th Floor Washington, D.C. 20002 Attention: N. Shulterbrandt ii TABLE OF CONTENTS PREFACE ...................................................................................................................................... -
Beardless Wildrye (Leymus Triticoides) Plant Guide
Plant Guide reptiles, rodents and other small mammals (McAdoo et BEARDLESS WILDRYE al., 2006; Olson, 2001). Leymus triticoides (Buckl.) Pilger Ethnobotanical: Beardless wildrye seed was used Plant Symbol = LETR5 historically by Native Americans as meal, or pinole (Chesnut, 1902). Contributed by: USDA NRCS Lockeford Plant Materials Center, California & Bridger Plant Materials Center, Status Montana Please consult the PLANTS Web site and your State Department of Natural Resources for this plant’s current status (e.g., threatened or endangered species, state noxious status, and wetland indicator values). Description General: Grass Family (Poaceae). Beardless wildrye is a cool-season, perennial, sod-forming native grass. It grows 18 to 51 inches tall (45-130 cm) and is strongly rhizomatous (Hickman, 1993). Stems are usually smooth, but are occasionally hairy. Leaf blades are green to blue- green, stiff and flat early in the growth season, becoming rolled later in the year, and are 0.1 to 0.2 inch wide (2.5-4 mm). The spike is narrow and 2 to 7.9 inches long (5-20 cm), with typically two or more spikelets occurring per node, except for occasional single spikelets near the top. Photo by Anna Young-Mathews, Lockeford PMC Glumes and lemmas are sharp pointed, and lemmas are Alternate Names generally tipped with an approximately 0.1 inch (3 mm) Creeping wildrye, alkali ryegrass, valley wild rye, Elymus awn. triticoides Identification: Beardless wildrye hybridizes with Leymus Uses condensatus, L. mollis and L. cinereus. It may be Beardless wildrye is primarily used for soil stabilization, confused with western wheatgrass (Pascopyrum smithii) especially along channel or river banks, and for wildlife due to their similar habitat and growth habit (OSU habitat in wetland and riparian plantings. -
Federal Register/Vol. 79, No. 139/Monday, July 21
Federal Register / Vol. 79, No. 139 / Monday, July 21, 2014 / Rules and Regulations 42197 connection with the acquisition or experimental or laboratory sense. Because When these regulations are enforced, production of depreciable property to be $50,000 of Z’s costs to construct the new test certain restrictions are placed on marine used in the taxpayer’s trade or business bed was incurred for research and traffic in specified areas. This are limited to amounts expended for experimentation, the costs qualify as research rulemaking project promotes efficiency or experimental expenditures under section research or experimentation within the 174. Paragraph (b)(2) of this section applies by eliminating the need to produce a meaning of section 174 and paragraph to $50,000 of Z’s costs for the test bed separate rule for each individual (a) of this section. because they are expenditures for research or recurring event, and serves to provide (5) Examples. The following examples experimentation that result in depreciable notice of the known recurring events illustrate the application of paragraph property to be used in the taxpayer’s trade or requiring a special local regulation or (b) of this section. business. Z’s remaining $4,950,000 of costs is safety zone throughout the year. not allowable under section 174 because Example 1. Amounts paid to others for DATES: This rule is effective August 20, these costs were not incurred for research or research or experimentation resulting in 2014. experimentation. depreciable property. X is a tool ADDRESSES: Documents mentioned in manufacturer. X has developed a new tool * * * * * this preamble are part of docket [USCG– design, and orders a specially-built machine (d) Effective/applicability date. -
Flood Risk Management Planning Resources for Washington DC
Flood Risk Management Planning Resources for Washington, DC January 20181 Flood Risk Management Planning Resources for Washington, DC January 2018 NOTICE: Usage: This is not a regulatory document. Updating: This document is current as of January 2018. It may be updated from time to time, at which point the dates will be changed. Disclaimer: Mention of a commercial company or product does not constitute an endorsement by the DC Silver Jackets or the National Capital Planning Commission. Cover Photo: The wake from a passing boat crashes over a flooded walkway on East Potomac Park during high tide on September 28, 2013. Credit: John Cochran 2 Table of Contents 1. Introduction 4 2. Flood Risk Management Resources 10 3. Mapping Current Flood Risk 28 4. Riverine Flooding 36 5. Interior Flooding 40 6. Coastal Flooding 44 7. Summary 56 8. Appendices 58 3 1. Introduction 4 Document Purpose Washington, DC and the surrounding National Capital Region (NCR) have experienced significant river, coastal, and interior floods that have negatively impacted federal and local operations, land and facility assets, and supporting infrastructure. As a result, flooding is one of the hazards that property and asset managers must consider to ensure a more secure and resilient capital. This guide provides a short summary of key flood risks in the NCR, an overview of recent studies and tools that address current and future flood risks in the region, and brief descriptions of how these studies can be used in flood risk management. While much of the information addresses the entire NCR, the guide focuses on Washington, DC and its monumental core.