Oregon Silverspot Recovery Plan
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CLATSOP COUNTY Scale in Mlles
CLATSOP COUNTY Scale In Mlles 81 8 I A 0,6 O 6 Secmide 0 10 6 7 WASV INGTON T I L LAMOOK COUNTY CO Clatsop County Knappa Prairie U. S. Army Fort Stevens, Ruth C. Bishop Dean H. Byrd (1992) Janice M. Healy (1952) Oregon Burial Site Guide Clatsop County Area: 873 square miles Population (1998): 35,424 County seat: Astoria, Population: 10,130 County established: 22 June 1844 Located on the south bank of the lower Columbia River where it enters the Pacific Ocean. Clatsop County was the site of the first white trading post in Oregon and therefore the earliest established cemetery. This was Fort Astoria founded in the spring of 1811 for the fur trade. It was occupied by the British in the fall of I 813 during the War of 1812 and was renamed Fort George. Returned to the Americans in 1818 and once again called Fort Astoria, the name was gradually transferred to a small civilian settlement as Astoria. The earliest burials after 1811 and those dating from the 1850's to about 1878 are now built over. Eventually most of Astoria's known burials were transferred to Ocean View which was established in 1872. The Clatsop Plains Pioneer Cemetery was begun in 1846 and is the earliest organized cemetery outside of Astoria. By the 1870's there were at least four other organized cemeteries. There were many family burial sites and still some Indian burials sites and a United States Military cemetery begun as early as 1868 at Fort Stevens. The most prominent ethnic nationalities from Europe were Finns and Swedes who are scattered through many cemeteries and family burial sites. -
APPENDIX a FRPA Regulation Species Recommended for FSP
APPENDIX A FRPA Regulation Species Recommended for FSP Inclusion by Former Coastal Forest District & BEC Zone FRPA Species of Concern / Applicable BEC Zone Former Forest District (and specific areas of concern within BEC zone) B Campbell River 1. Dalmatian toadflax Linaria dalmatica / CDF B 2. Diffuse knapweed Centaurea diffusa / CDF 3. Giant knotweed Polygonum sachalinense / CDF, CWH, MH 4. Gorse Ulex europaeus / CDF 5. Hoary alyssum Berteroa incana / CDF 6. Japanese knotweed Polygonum cuspidatum / CDF, CWH, MH 7. Leafy spurgeB Euphorbia esula / CDF 8. Meadow hawkweed Hieracium pilosella / CDF 9. Meadow knapweedB Centaurea pratensis / CDF & CWH (near Comox) 10. Orange hawkweed Hieracium aurantiacum / CWH 11. Purple loosestrifeB Lythrum salicaria / CDF & CWH (near Comox & Campbell River) 12. Scotch broom Cytisus scoparius / CDF, CWH & MH 13. Spotted knapweedB Centaurea maculosa / CDF 14. Sulphur cinquefoil Potentilla recta / CDF 15. Tansy ragwortBSenecio jacobaea / CDF & CWH (near Sayward) 16.Yellow Iris Iris pseudacorus / CDF & CWH (near Comox and Campbell River) Chilliwack 1. Baby's breath Gypsophila paniculata / IDF (between Lillooet & Boston Bar) 2. Blueweed Echium vulgare / IDF & CWH 3. Dalmatian toadflaxBLinaria dalmatica / IDF 4. Diffuse knapweedB Centaurea diffusa / IDF 5. Giant knotweed Polygonum sachalinense / CWH, MH 6. Hoary alyssum Berteroa incana / IDF 7. Hound's-tongueB Cynoglossum officinale / IDF (between Lytton & Boston Bar) 8. Japanese knotweed Polygonum cuspidatum / CWH, MH 9. Leafy spurgeB Euphorbia esula / IDF 10. Meadow hawkweed Hieracium pilosella / IDF & CWH 11. Orange hawkweed Hieracium aurantiacum / IDF & CWH 12. Purple loosestrifeB Lythrum salicaria / CDF & CWH (near Fraser Valley) 13. Scotch broom Cytisus scoparius / CWH & MH 14. Spotted knapweedB Centaurea maculosa / IDF 15. Sulphur cinquefoil Potentilla recta / IDF 16. -
Protecting O&C Lands: Mount Hebo
A fact sheet from Sept 2013 Bob Van Dyk Bob Van Dyk Bob Van Dyk Protecting O&C Lands Mount Hebo Location: Northern Oregon Coast Range Rising 3,175 feet from its densely forested surroundings, Mount Hebo is one of the highest peaks 11,310 Acres: in the northern Oregon Coast Range. The prominent Ecological value: Historical significance, lookout is a popular day hike for those willing to breathtaking vistas, hemlock and Douglas fir climb far above the massive hemlock and Douglas fir forests, and abundant wildflowers forest to fully experience the breathtaking scope of the Northwest’s landscape. Along the path, a traveler Economic value: Hiking and biking will find an abundance of towering trees and rare wildflowers. North of the mountain’s summit lies the last remaining roadless area in northwest Oregon, What are the O&C lands? providing a unique wild land experience in this part In 1866, Congress established a land-grant program for the Oregon of the state. This area should be forever protected & California (O&C) Railroad Co. to spur the completion of the as wilderness. rail line between Portland and San Francisco that required the company to sell the deeded land to settlers. Forty years later, when Pioneers dubbed the peak “Heave Ho” because of the the company failed to meet the terms of the agreement fully, the way it seemed to erupt from the surrounding forest. federal government reclaimed more than 2 million acres of mostly Over the years, the name “Heave Ho” morphed into forested land. Today, those O&C lands remain undeveloped and “Hebo.” These explorers discovered what Native are administered by the Bureau of Land Management and the U.S. -
Fort Clatsop by Unknown This Photo Shows a Replica of Fort Clatsop, the Modest Structure in Which the Corps of Discovery Spent the Winter of 1805-1806
Fort Clatsop By Unknown This photo shows a replica of Fort Clatsop, the modest structure in which the Corps of Discovery spent the winter of 1805-1806. Probably built of fir and spruce logs, the fort measured only fifty feet by fifty feet, not a lot of space for more than thirty people. Nevertheless, it served its purpose well, offering Expedition members shelter from the incessant rains of the coast and giving them security against the Native peoples in the area. Although the Corps named the fort after the local Indians, they did not fully trust either the Clatsop or the related Chinook people, and kept both at arms length throughout their stay on the coast. The time at Fort Clatsop was well spent by Meriwether Lewis and William Clark. The captains caught up on their journal entries and worked on maps of the territory they had traversed since leaving St. Louis in May 1804. Many of the captains’ most important observations about the natural history and Native cultures of the Columbia River region date from this period. Other Expedition members hunted the abundant elk in the area, stood guard over the fort, prepared animal hides, or boiled seawater to make salt, but mostly they bided their time, eagerly anticipating returning east at the first sign of spring. The Corps set off in late March 1806, leaving the fort to Coboway, headman of the Clatsop. In a 1901 letter to writer Eva Emery Dye, a pioneer by the name of Joe Dobbins noted that the remains of Fort Clatsop were still evident in the 1850s, but “not a vestige of the fort was to be seen” when he visited Clatsop Plains in the summer of 1886. -
Forest Grove: a Historic Context
Forest Grove: A Historic Context Deve;loped by Peter J. Edwaidbi" C olumbiø Hßtor íc al Re s e ar c h 6l?ß Southwest Corbett Portland, Oregorr g72OI for The City of Forest'Grove Community Developmg¡1t", Depa4$r,ne4t - SePtember 1993 This project is funded by th9 C-ity-of ded by the National Park Servíce, U.S.'Dep of thej Oregon State Table of Contents List of Figures List of Tables Section I Historic Overview Introduction 1 Historic Periods 4 1792-1811 Exploration 4 1812-1846 Fur Tbade and Mission to the Indians 5 1847-1865 Settlement, Statehood & Steampower 10 1866-1883 Railroad and Industrial Gnowth 16 1884-1913 Ttre Progressive Era 2t 1914-1940 The Motor Age 25 I94l-L967 War and Post-War Era 27 Section II Identification 28 Resource Themes 29 Distribution Patterns of Resources 36 SectionIII Registration 38 Section IV Recommendations for Theatment 40 Bibliography 44 Appendix A 47 I List of Figures Figure 1 City of Forest Grove 2 Figure 2 Western Oregon Indians in 1800 3 Figure 3 General Land OfEce Plat, 1852 9 Figure 4 Willamette Valley Inten¡rban Lines 23 Figure 5 Forest Gncve Tnntng Map, 1992 42 List of Tables Table 1 Greater Forest Grove Occupations, 1850 L2 Table 2 Greater Forest Grove Population Origin, 1850 13 Table 3 Greater Forest Grove Occupations, 1860 T4 Table 4 Greater Forest Grove Population Origin, 1860 t4 Table 5 Greater Forest Grove Occupations, 1870 16 Table 6 Greater Forest Grove Population Origin, 1870 L7 t SECTION I: HISTORIC OYERVIE\il INTRODUCTION The City of Forest Grove Historic Overview is a study of events and themes as they relate to the history of Forest Grove. -
Geologic Map of the Cascade Head Area, Northwestern Oregon Coast Range (Neskowin, Nestucca Bay, Hebo, and Dolph 7.5 Minute Quadrangles)
(a-0g) R ago (na. 96-53 14. U.S. DEPARTMENT OF THE INTERIOR , U.S. GEOLOGICAL SURVEY Alatzi2/6 (Of (c,c) - R qo rite 6/6-53y Geologic Map of the Cascade Head Area, Northwestern Oregon Coast Range (Neskowin, Nestucca Bay, Hebo, and Dolph 7.5 minute Quadrangles) by Parke D. Snavely, Jr.', Alan Niem 2 , Florence L. Wong', Norman S. MacLeod 3, and Tracy K. Calhoun 4 with major contributions by Diane L. Minasian' and Wendy Niem2 Open File Report 96-0534 1996 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American stratigraphic code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 1/ U.S. Geological Survey, Menlo Park, CA 94025 2/ Oregon State University, Corvallis, OR 97403 3/ Consultant, Vancouver, WA 98664 4/ U.S. Forest Service, Corvallis, OR 97339 TABLE OF CONTENTS INTRODUCTION 1 GEOLOGIC SKETCH 2 DESCRIPTION OF MAP UNITS SURFICIAL DEPOSITS 7 BEDROCK UNITS Sedimentary and Volcanic Rocks 8 Intrusive Rocks 14 ACKNOWLEDGMENTS 15 REFERENCES CITED 15 MAP SHEETS Geologic Map of the Cascade Head Area, Northwestern Oregon Coast Range, scale 1:24,000, 2 sheets. Geologic Map of the Cascade Head Area, Northwest Oregon Coast Range (Neskowin, Nestucca Bay, Hebo, and Dolph 7.5 minute Quadrangles) by Parke D. Snavely, Jr., Alan Niem, Florence L. Wong, Norman S. MacLeod, and Tracy K. Calhoun with major contributions by Diane L. Minasian and Wendy Niem INTRODUCTION The geology of the Cascade Head (W.W. -
Newsletter No 250 July 2018
Published by RUGBY NATURAL HISTORY SOCIETY www.rugbynaturalhistory.org.uk PRESIDENT – Dr P Reeve Newsletter No 250 July 2018 Contents this edition ~Minibus trip: Rutland Water (book now!) ~News of members ~Summer field visit reports ~ Winter indoor meetings: dates for your diary ~Data protection information ~Current committee members (with contact information) Appendices included: species lists for Grove Hill, Snitterfield Bushes, Dunchurch Meadows, Stockton Cutting and Tasker’s Meadow Photos © Paul Hodges: cowslip carpet; thimble morel; semi-free morel at Grove Hill reserve Minibus trip? Speak up now! Rutland Water. Would you like to travel by minibus to our Rutland Water field visit on Thursday 6 September? Several members requested that we arrange this and David Knapp is willing to do so as long as there is sufficient interest - at least sixteen people would be 1 needed. The cost of a minibus would be £20 per person. The departure/return point would, as usual, be St Mark’s Church car park in Bilton, with additional pick up/drop off points in Long Itchington and Marton. The proposed return visit to Oxford Natural History Museum was cancelled because there were not enough people to make it viable. This is therefore now the FINAL CALL (!) for Rutland Water. If you would be interested in travelling by minibus, please let David know by Wednesday 1 August 2018 and he will then get back to you with further details. Tel. 01788 817346 or e:mail [email protected] News of members Most members will already know that Frank Ollerenshaw died in May. Nine of us attended his funeral, where we learned that he had served in young people’s organisations, as well as being a member both of the society and of Warwickshire Wildlife Trust and having many other interests. -
Land-Use Changes, Farm Management and the Decline of Butterflies Associated with Semi-Natural Grasslands in Southern Sweden
A peer-reviewed open-access journal Nature Conservation Land-use6: 31–48 (2013) changes, farm management and the decline of butterflies.... 31 doi: 10.3897/natureconservation.6.5205 APPLIED ECOLOGY http://www.pensoft.net/natureconservation Launched to accelerate biodiversity conservation Land-use changes, farm management and the decline of butterflies associated with semi-natural grasslands in southern Sweden Sven G. Nilsson1, Markus Franzén1,2, Lars B. Pettersson1,3 1 Biodiversity Unit, Department of Biology, Lund University, Ecology Building, SE-223 62 Lund, Sweden 2 UFZ Helmholtz Centre for Environmental Research, Department of Community Ecology, Theodor-Lieser- Straße 4, D-06120 Halle, Germany 3 Swedish Butterfly Monitoring Scheme, Lund University, Ecology Buil- ding, SE-223 62 Lund, Sweden Corresponding author: Lars B. Pettersson ([email protected]) Academic editor: L. Penev | Received 26 March 2013 | Accepted 30 October 2013 | Published 18 November 2013 Citation: Nilsson SG, Franzén M, Pettersson LB (2013) Land-use changes, farm management and the decline of butterflies associated with semi-natural grasslands in southern Sweden. Nature Conservation 18: 31–48. doi: 10.3897/ natureconservation.6.5205 Abstract Currently, we are experiencing biodiversity loss on different spatial scales. One of the best studied taxo- nomic groups in decline is the butterflies. Here, we review evidence for such declines using five systematic studies from southern Sweden that compare old butterfly surveys with the current situation. Additionally, we provide data on butterfly and burnet moth extinctions in the region’s counties. In some local areas, half of the butterfly fauna has been lost during the last 60–100 years. -
FINE FESCUE for HOME LAWNS Home Garden Series
FINE FESCUE FOR HOME LAWNS Home Garden Series By Dr. Gwen K. Stahnke, Extension Turfgrass Agronomist (retired), WSU Puyallup Research and Extension Center. Dr. William J. Johnston, Professor of Turfgrass Science, Washington State University. Marianne Ophardt, WSU Extension Area Horticulture Specialist FS200E FS200E | Page 1 | ext.wsu.edu WSU EXTENSION | FINE FESCUE FOR HOME LAWNS Fine Fescue for Home Lawns General Description Fine fescues (Festuca spp.) are species of flowering plants belonging to the grass family. They are cross-pollinated and propagated from seed. Fescues are some of the most drought and shade tolerant of the cool-season grasses grown in temperate regions. Turfgrass breeders have divided fine fescues into different types or classifications, each with different attributes, such as creeping habit, quicker germination, or moderate green color. Chewing’s fescue (Festuca rubra ssp. commutata), hard fescue (Festuca trachyphylla), sheep fescue (Festuca ovina), slender- creeping red fescue (Festuca rubra ssp. littoralis), and strong- Figure 1. Fine fescue close up for grass identification. creeping red fescue (Festuca rubra. ssp. rubra) are the fine- leaf Festuca species currently used for turfgrass in the United States. Most turf-type fine-leaf fescue species are native to North America, including red, hard, and sheep fescues. Fine fescues are moderately wear tolerant and can be used in a mixture with Kentucky bluegrass (Poa pratensis L.) or perennial ryegrasses (Lolium perenne L.) in moderate traffic areas in Washington. Fine fescues spread mainly by tillers or primary lateral shoots that begin within the crown. The lateral shoots have very limited internode length. However, the creeping forms do spread by underground rhizomes or lateral stems. -
Poaceae: Pooideae) Based on Phylogenetic Evidence Pilar Catalán Universidad De Zaragoza, Huesca, Spain
Aliso: A Journal of Systematic and Evolutionary Botany Volume 23 | Issue 1 Article 31 2007 A Systematic Approach to Subtribe Loliinae (Poaceae: Pooideae) Based on Phylogenetic Evidence Pilar Catalán Universidad de Zaragoza, Huesca, Spain Pedro Torrecilla Universidad Central de Venezuela, Maracay, Venezuela José A. López-Rodríguez Universidad de Zaragoza, Huesca, Spain Jochen Müller Friedrich-Schiller-Universität, Jena, Germany Clive A. Stace University of Leicester, Leicester, UK Follow this and additional works at: http://scholarship.claremont.edu/aliso Part of the Botany Commons, and the Ecology and Evolutionary Biology Commons Recommended Citation Catalán, Pilar; Torrecilla, Pedro; López-Rodríguez, José A.; Müller, Jochen; and Stace, Clive A. (2007) "A Systematic Approach to Subtribe Loliinae (Poaceae: Pooideae) Based on Phylogenetic Evidence," Aliso: A Journal of Systematic and Evolutionary Botany: Vol. 23: Iss. 1, Article 31. Available at: http://scholarship.claremont.edu/aliso/vol23/iss1/31 Aliso 23, pp. 380–405 ᭧ 2007, Rancho Santa Ana Botanic Garden A SYSTEMATIC APPROACH TO SUBTRIBE LOLIINAE (POACEAE: POOIDEAE) BASED ON PHYLOGENETIC EVIDENCE PILAR CATALA´ N,1,6 PEDRO TORRECILLA,2 JOSE´ A. LO´ PEZ-RODR´ıGUEZ,1,3 JOCHEN MU¨ LLER,4 AND CLIVE A. STACE5 1Departamento de Agricultura, Universidad de Zaragoza, Escuela Polite´cnica Superior de Huesca, Ctra. Cuarte km 1, Huesca 22071, Spain; 2Ca´tedra de Bota´nica Sistema´tica, Universidad Central de Venezuela, Avenida El Limo´n s. n., Apartado Postal 4579, 456323 Maracay, Estado de Aragua, -
Appendices Appendix A
APPENDICES APPENDIX A HISTORY OF SKIPANON RIVER WATERSHED Prepared by Lisa Heigh and the Skipanon River Watershed Council Appendix A - Skipanon River Watershed History 2 APPENDIX A HISTORY Skipanon River Watershed Natural History TIMELINE · 45 million years ago - North American Continent begins collision with Pacific Ocean Seamounts (now the Coast Range) · 25 million years ago Oregon Coast began to emerge from the sea · 20 million years ago Coast Range becomes a firm part of the continent · 15 million years ago Columbia River Basalt lava flows stream down an ancestral Columbia River · 12,000 years ago last Ice Age floods scour the Columbia River · 10,000 years ago Native Americans inhabit the region (earliest documentation) - Clatsop Indians used three areas within the Skipanon drainage as main living, fishing and hunting sites: Clatsop Plains, Hammond and a site near the Skipanon River mouth, where later D.K. Warren (Warrenton founder) built a home. · 4,500 years ago Pacific Ocean shoreline at the eastern shore of what is now Cullaby Lake · 1700’s early part of the century last major earthquake · 1780 estimates of the Chinook population in the lower Columbia Region: 2,000 total – 300 of which were Clatsops who lived primarily in the Skipanon basin. · 1770’s-1790’s Robert Gray and other Europeans explore and settle Oregon and region, bringing with them disease/epidemic (smallpox, malaria, measles, etc.) to native populations · 1805-1806 Lewis and Clark Expedition, camp at Fort Clatsop and travel frequently through the Skipanon Watershed -
Gearhart to Fort Stevens, Prelim
NOTICE The Oregon Department of Geology and Mineral Industries is publishing this paper because the information furthers the mission of the Department. To facilitate timely distribution of the information, this report is published as received from the authors and has not been edited to our usual standards. STATE OF OREGON DEPARTMENT OF GEOLOGY AND MINERAL INDUSTRIES Suite 965, 800 NE Oregon St., #28 Portland, Oregon 97232 OPEN-FILE REPORT O-01-04 COASTAL EROSION HAZARD ZONES ALONG THE CLATSOP PLAINS, OREGON: GEARHART TO FORT STEVENS PRELIMINARY TECHNICAL REPORT TO CLATSOP COUNTY 2001 By JONATHAN C. ALLAN AND GEORGE R. PRIEST Oregon Department of Geology and Mineral Industries, Coastal Field Office, 313 SW 2nd St, Suite D, Newport, OR 97365 NOTICE The results and conclusions of this report are necessarily based on limited geologic and geophysical data. At any given site in any map area, site-specific data could give results that differ from those shown in this report. This report cannot replace site-specific investigations. The hazards of an individual site should be assessed through geotechnical or engineering geology investigation by qualified practitioners. Table of Contents EXECUTIVE SUMMARY ............................................................................................... iii INTRODUCTION .............................................................................................................. 1 BEACH PROCESSES AND FEATURES......................................................................... 2 Beach Erosion –