Conservation Genetics of High Elevation Five-Needle White Pines
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Washington Division of Geology and Earth Resources Open File Report
l 122 EARTHQUAKES AND SEISMOLOGY - LEGAL ASPECTS OPEN FILE REPORT 92-2 EARTHQUAKES AND Ludwin, R. S.; Malone, S. D.; Crosson, R. EARTHQUAKES AND SEISMOLOGY - LEGAL S.; Qamar, A. I., 1991, Washington SEISMOLOGY - 1946 EVENT ASPECTS eanhquak:es, 1985. Clague, J. J., 1989, Research on eanh- Ludwin, R. S.; Qamar, A. I., 1991, Reeval Perkins, J. B.; Moy, Kenneth, 1989, Llabil quak:e-induced ground failures in south uation of the 19th century Washington ity of local government for earthquake western British Columbia [abstract). and Oregon eanhquake catalog using hazards and losses-A guide to the law Evans, S. G., 1989, The 1946 Mount Colo original accounts-The moderate sized and its impacts in the States of Califor nel Foster rock avalanches and auoci earthquake of May l, 1882 [abstract). nia, Alaska, Utah, and Washington; ated displacement wave, Vancouver Is Final repon. Maley, Richard, 1986, Strong motion accel land, British Columbia. erograph stations in Oregon and Wash Hasegawa, H. S.; Rogers, G. C., 1978, EARTHQUAKES AND ington (April 1986). Appendix C Quantification of the magnitude 7.3, SEISMOLOGY - NETWORKS Malone, S. D., 1991, The HAWK seismic British Columbia earthquake of June 23, AND CATALOGS data acquisition and analysis system 1946. [abstract). Berg, J. W., Jr.; Baker, C. D., 1963, Oregon Hodgson, E. A., 1946, British Columbia eanhquak:es, 1841 through 1958 [ab Milne, W. G., 1953, Seismological investi earthquake, June 23, 1946. gations in British Columbia (abstract). stract). Hodgson, J. H.; Milne, W. G., 1951, Direc Chan, W.W., 1988, Network and array anal Munro, P. S.; Halliday, R. J.; Shannon, W. -
Production and Saturation of Porosity in the Lunar Highlands from Impact Cratering
The fractured Moon: Production and saturation of porosity in the lunar highlands from impact cratering The MIT Faculty has made this article openly available. Please share how this access benefits you. Your story matters. Citation Soderblom, Jason M., et al. “The Fractured Moon: Production and Saturation of Porosity in the Lunar Highlands from Impact Cratering.” Geophysical Research Letters, vol. 42, no. 17, Sept. 2015, pp. 6939–44. © 2015 American Geophysical Union As Published http://dx.doi.org/10.1002/2015GL065022 Publisher American Geophysical Union (AGU) Version Final published version Citable link http://hdl.handle.net/1721.1/118615 Terms of Use Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use. PUBLICATIONS Geophysical Research Letters RESEARCH LETTER The fractured Moon: Production and saturation 10.1002/2015GL065022 of porosity in the lunar highlands Key Points: from impact cratering • The relation between impact-generated porosity and crater size is quantified Jason M. Soderblom1, Alexander J. Evans2, Brandon C. Johnson1, H. Jay Melosh3, Katarina Miljković1,4, • Impacts into highly porous targets 5 6 7 8 3 result in positive gravity anomalies Roger J. Phillips , Jeffrey C. Andrews-Hanna , Carver J. Bierson , James W. Head III , Colleen Milbury , 9 7 1 2,10 11 • The cratering record of the oldest Gregory A. Neumann , Francis Nimmo , David E. Smith , Sean C. Solomon , Michael M. Sori , lunar surfaces is preserved in the -
Stuart, Trees & Shrubs
Excerpted from ©2001 by the Regents of the University of California. All rights reserved. May not be copied or reused without express written permission of the publisher. click here to BUY THIS BOOK INTRODUCTION HOW THE BOOK IS ORGANIZED Conifers and broadleaved trees and shrubs are treated separately in this book. Each group has its own set of keys to genera and species, as well as plant descriptions. Plant descriptions are or- ganized alphabetically by genus and then by species. In a few cases, we have included separate subspecies or varieties. Gen- era in which we include more than one species have short generic descriptions and species keys. Detailed species descrip- tions follow the generic descriptions. A species description in- cludes growth habit, distinctive characteristics, habitat, range (including a map), and remarks. Most species descriptions have an illustration showing leaves and either cones, flowers, or fruits. Illustrations were drawn from fresh specimens with the intent of showing diagnostic characteristics. Plant rarity is based on rankings derived from the California Native Plant Society and federal and state lists (Skinner and Pavlik 1994). Two lists are presented in the appendixes. The first is a list of species grouped by distinctive morphological features. The second is a checklist of trees and shrubs indexed alphabetically by family, genus, species, and common name. CLASSIFICATION To classify is a natural human trait. It is our nature to place ob- jects into similar groups and to place those groups into a hier- 1 TABLE 1 CLASSIFICATION HIERARCHY OF A CONIFER AND A BROADLEAVED TREE Taxonomic rank Conifer Broadleaved tree Kingdom Plantae Plantae Division Pinophyta Magnoliophyta Class Pinopsida Magnoliopsida Order Pinales Sapindales Family Pinaceae Aceraceae Genus Abies Acer Species epithet magnifica glabrum Variety shastensis torreyi Common name Shasta red fir mountain maple archy. -
Pines in the Arboretum
UNIVERSITY OF MINNESOTA MtJ ARBORETUM REVIEW No. 32-198 PETER C. MOE Pines in the Arboretum Pines are probably the best known of the conifers native to The genus Pinus is divided into hard and soft pines based on the northern hemisphere. They occur naturally from the up the hardness of wood, fundamental leaf anatomy, and other lands in the tropics to the limits of tree growth near the Arctic characteristics. The soft or white pines usually have needles in Circle and are widely grown throughout the world for timber clusters of five with one vascular bundle visible in cross sec and as ornamentals. In Minnesota we are limited by our cli tions. Most hard pines have needles in clusters of two or three mate to the more cold hardy species. This review will be with two vascular bundles visible in cross sections. For the limited to these hardy species, their cultivars, and a few hy discussion here, however, this natural division will be ignored brids that are being evaluated at the Arboretum. and an alphabetical listing of species will be used. Where neces Pines are readily distinguished from other common conifers sary for clarity, reference will be made to the proper groups by their needle-like leaves borne in clusters of two to five, of particular species. spirally arranged on the stem. Spruce (Picea) and fir (Abies), Of the more than 90 species of pine, the following 31 are or for example, bear single leaves spirally arranged. Larch (Larix) have been grown at the Arboretum. It should be noted that and true cedar (Cedrus) bear their leaves in a dense cluster of many of the following comments and recommendations are indefinite number, whereas juniper (Juniperus) and arborvitae based primarily on observations made at the University of (Thuja) and their related genera usually bear scalelikie or nee Minnesota Landscape Arboretum, and plant performance dlelike leaves that are opposite or borne in groups of three. -
VHSL Regionals 2012 Round #4
VHSL Regionals 2012 Round 4 First Period, Fifteen Tossups 1. This author tells of an attack "by three doors left unguarded" as "blue-eyed banditti" climb into his chair. This poet, who immortalized his daughters Alice, Allegra, and Edith in "The Children's Hour," also wrote a long poem set "by the shores of Gitche Gumee." In another poem, he described a character who feels "the secret dread of the lonely belfry and the dead" before sending a signal from the Old North Church. For 10 points, name this American poet of The Song of Hiawatha and "Paul Revere's Ride." ANSWER: Henry Wadsworth Longfellow 105-12-55-04101 2. One side in this incident, led by Yellow Bird and Big Foot, was urged to resist because their shirts would protect them from gunfire. The other side in this event was led by James Forsyth. Eighty-three years after this event occurred, Russell Means of the AIM led a seventy-one-day standoff with federal agents at the site of this incident. This event occurred days after Sitting Bull was killed in reaction to the popularity of the Ghost Dance. For 10 points, name this 1890 massacre of about 150 Sioux in South Dakota. ANSWER: Wounded Knee Massacre 131-12-55-04102 3. While living near the town of Templeton, this character clashes with Judge Marmaduke Temple and befriends the young hunter Oliver Edwards. In another novel, this character guides Cora and Alice Munro to their father’s command and kills Magua to avenge the death of his friend Uncas. -
Xerox University Microfilms 300 North Zeeb Road Ann Arbor, Michigan 48106 75-26,628
INFORMATION TO USERS This material was produced from a microfilm copy of the original document. While the most advanced technological means to photograph and reproduce this document have been used, the quality is heavily dependent upon the quality of the original submitted. The following explanation of techniques is provided to help you understand markings or patterns which may appear on this reproduction. 1. The sign or "target" for pages apparently lacking from the document photographed is "Missing Page(s)". If it was possible to obtain the missing page(s) or section, th ey are spliced into the film along with adjacent pages. This may have necessitated cutting thru an image and duplicating adjacent pages to insure you complete continuity. 2. When an image on th e film is obliterated with a large round black mark, it is an indication that the photographer suspected that the copy may have moved during exposure and thus cause a blurred image. You will find a good image of the page in the adjacent frame. 3. When a map, drawing or chart, etc., was part of the material being photographed the photographer followed a definite method in "sectioning" the material. It is customary to begin photoing at the upper left hand corner of a large sheet and to continue photoing from left to right in equal sections with a small overlap. If necessary, sectioning is continued again — beginning below the first row and continuing on until complete. 4. The majority of users indicate that the textual content is of greatest value, however, a som ewhat higher quality reproduction could be made from "photographs" if essential to the understanding of the dissertation. -
795-Rib NASA TECHNICAL MEMORANDUM NASA TM-88477
795-Rib NASA TECHNICAL MEMORANDUM NASA TM-88477 B.A. Ivanov Translation of: "Mekhanika krateroobrazovaniya," IN: Itogi nauki i teckhniki, Seriya: Mekhanika deformi- ruyemogo tverdogo tela, Vol. 14, 1981, Moscow, pp. 60-128 (UDC 624.131:551.215.6) NATIONAL AERONAUTICS AND SPACE ADMINISTRATION WASHINGTON, D.C. 20546 AUGUST 1986 (NASA-TM-08417) CHATERING HECHANICS (Naticnal Aercnautics and SFace N 8 7- 1 55 62 Bduinistration) 55 p CSCL O8G Unclas 53/46 40340 I Translation of: "Mekhanika krateroobrazovaniya," IN: Itogi nauki i Tekhniki, Seriya: Mekhanika deformiruyemogo tverdogo tela, Vol. 14, 1981, Moscow, pp. 60-128 (UDC 624.131:551.215.6 t Main concepts and theoretical models which are used for studying the mechanics of cratering are discussed. Numerical two-dimensional calculations are made of explosions near a surface and high- speed impact. Models are given for the motion of a medium during cratering. Gata from laboratory modeling are given. The effect of gravitational force and scales of cratering phenomena is analyzed. MECHANICS OF DEFORMABLE SOLID BODY UDC 624.131:551.215.6 CRATERING 'MECHANICS By B. A. Ivanov Introduction /E* One can define mechanics of craterins as a discipline , studying the formation of an indentation (crater or funnel) on the surface of a solid deformable body as a result of high-speed collision or explosion near the surface with regard for the resulting shock waves, high-speed plastic deformation of the destroyed materials, scattering of the ejecta and other concomitant phenomena. The mechanics of cratering thus applied is an applied dis- cipline using results of the physics of shock waves and high pressures, mechanics of a solid deformable bodyr hydro gas dynamicsr etc. -
Douglas- Fir Limber Pine Lodgepole Pine Ponderosa Pine Blue Spruce
NAME ORIGIN BARK FEMALE CONES NEEDLES WHERE USES TRIVIA Named by Smooth gray bark To 4ÂÂ long, Soft, flat, 2-sided, Found on north or Railroad crossties, State tree of Scottish botanist on young trees yellowish to light 1¼″ long and south-facing slopes, mine timbers, for Oregon. David Douglas. with numerous brown hanging cones rounded at the tip. in shady ravines and building ships and The Latin name DOUGLAS- Fir is from the resin scars. with uniquely 3- Dark yellow green or on rocky slopes boats, construction psuedotsuga Middle English pointed bracts blue green. Shortly where the soil is lumber, plywood, means FIR firre and Old protruding from cone stalked spreading fairly deep. telephone poles, ÂÂfalse Psuedotsuga English fyrh. scales like a snakes- mostly in two rows. fencing, railroad-car fir.ÂÂ menziesii tongue. Single small groove construction, boxes Can drop 2 on topside of needles and crates, flooring, million seeds in and single white line furniture, ladders a good year. on underside of and pulpwood. needles. Pine is from the Light gray to Big (to 9ÂÂ long) Stout in clusters of 5 Found on rocky, Lumber, railroad Cones start to LIMBER Latin pinus and blackish brown. cylindrical, greenish needles, to 3″ long. gravelly slopes, cross ties, poles, appear after the the Old English Smooth and silvery brown, with thick, Straight or slightly ridges and peaks. turpentine, tar and tree reaches 20 PINE pin. gray on young broad scales. Cone curved, not sticky to fuel. years of age. Pinus flexilis trees. scales lack prickles. the touch. Dark green. Pine is from the Bark is grayish or Light yellow brown, Stout, twisted Found in well Lumber, knotty Many Plains Latin pinus and light brown, thin reddish or dark green, needles, mostly in drained soils, dry pine paneling, Indian tribes the Old English and with many lopsided cones to pairs, to 2½″ long. -
Pinus Monticola Doulg. Ex D. Don Family: Pinaceae Western White Pine
Pinus monticola Doulg. Ex D. Don Family: Pinaceae Western White Pine The genus Pinus is composed of about 100 species native to temperate and tropical regions of the world. Wood of pine can be separated microscopically into the white, red and yellow pine groups. The word pinus is the classical Latin name. The word monticola means inhabiting mountains. Other Common Names: Berg-tall, Columbia pijn, finger-cone pine, Idaho white pine, little sugar pine, mountain pine, mountain white pine, Norway white pine, pin argente, pin argente americain, pino bianco americano, pino blanco americano, silver pine, soft pine, vasterns Weymouth-tall, western white pine, Weymouth berg-pijn, Weymouth mountain pine, white pine, yellow pine. Distribution: Western white pine is native to the mountains ffrom northwestern Montana, extreme southwestern Alberta and southern British Columbia, south to Washington, Oregon and California through the Sierra Nevada to western Nevada and central California. The Tree: Western white pine trees reach heights of 180 feet, with a clear bole for 70 to 100 feet and diameters of 3.5 feet. Over mature trees may reach heights of 197 feet, with diameters of almost 6 feet. They may grow for 300 to 400 years. General Wood Characteristics: The sapwood of western white pine is nearly white to pale yellow, while the heartwood is cream to light reddish brown and may turn darker upon exposure. The wood has a slight resinous odor, but no characteristic taste. It is straight grained and has a rather coarse texture. It is also soft, light, is moderately weak in bending, moderately strong in end compression and moderately low in shock resistance. -
Identifying Old Trees and Forests
Identifying Old Trees and Forests IN EASTERN WASHINGTON by Robert Van Pelt Acknowledgements This guide is a companion to Identifying Mature and Old Forests in Western Washing- ton (Van Pelt, 2007). It was conceived in response to the work of the Old Growth Definition Committee. The committee was convened at the request of the Washington State Legisla- ture to map and inventory old growth forests on state trust lands managed by DNR. In the course of the committee’s work, the need became apparent for field guidance to assist field personnel in identifying individual old trees and forests. It is essential to acknowledge the people I worked with on the Old Growth Definition Com- mittee: Dr. Jerry F. Franklin, Dr. Miles Hemstrom, Joe Buchanan, Rex Crawford, Steve Curry, Sabra Hull, and Walt Obermeyer, all of whom contributed to the concepts which form the basis of this guide. Many people reviewed the text during its various iterations, which greatly contributed to improvements in both readability and scientific content: Richard Bigley Jerry Franklin Andrew Larson Ron Brightman Keala Hagman Jim Lutz Joe Buchanan Miles Hemstrom Tami Miketa Angie Cahill Sabra Hull Bob Redling Chris Earle Arthur Jacobson Jeff Ricklefs The layout and design of this guide was ably and beautifully conducted by Nancy Charbonneau and Jane Chavey of the DNR Communications Group. Photos, maps, and drawings by author except where indicated otherwise. Washington State Department of Natural Resources This guide was produced under contract as part of the ongoing research and application of new information to inform both land management and resource protection goals of Washington’s Department of Natural Resources. -
Quaternary Research 79 (2013) 309
Quaternary Research 79 (2013) 309 Contents lists available at SciVerse ScienceDirect Quaternary Research journal homepage: www.elsevier.com/locate/yqres Corrigendum Corrigendum to “Late-Holocene response of limber pine (Pinus flexilis) forests to fire disturbance in the Pine Forest Range, Nevada, USA” [Quaternary Research 78 (2012) 465–473] Robert K. Shriver a,1, Thomas A. Minckley a,b,⁎ a Dept. of Botany, University of Wyoming, Laramie, WY 82071, USA b Roy J. Shlemon Center for Quaternary Studies, University of Wyoming, Laramie, WY 82071, USA The purpose of Shriver and Minckley (2012) “Late-Holocene re- The occurrence of such a large population of whitebark pine in this sponse of limber pine (Pinus flexilis) forests to fire disturbance in portion of northwestern Nevada is notable in itself. The Pine Forest the Pine Forest Range, Nevada, USA” was to assess historic responses Range is not particularly high in comparison to surrounding ranges to disturbance (fire) using pollen percentage data derived from a that do not have similar forest types. The presence of a few but exceed- sediment core using superimposed epoch analysis. This work was ingly rare limber pines suggests that there might have been historic conducted in a small glacial tarn, Blue Lake, located in an isolated processes that have favored one species versus the other over time — mountain range of northwestern Nevada, the Pine Forest Range. maybe even fire. The differences in the ecology of the two species are The benefit of this site was the unique setting of an isolated forest significant enough to suspect that they would have different climatic that added to our knowledge of disturbance in five-needle pine eco- and disturbance responses. -
Ecology of Whitebark Pine in the Pacific Northwest
USDA Forest Service R6-NR-FHP-2007-01 Ecology of Whitebark Pine in the Pacific Northwest Gregory J. Ettl College of Forest Resources, University of Washington Box 352100 Seattle, WA 98195 Whitebark pine (Pinus albicaulis) is found in the subalpine zone throughout the Coastal, Olympic, Cascade, and Klamath Mountains, extending well into California at high elevations along the Sierra Nevada. Precipitation is > 300 cm/yr on the western slopes of the Coastal Mountains in British Columbia and the Olympics & Washington Cascades (Franklin and Dyrness 1988). Precipitation generally decreases along the Oregon Cascades moving south, with 50-100 cm/yr common in southern Oregon. The coastal mountain ranges in southern Oregon and Northern California, including the Siskiyou, Trinity, and Klamath Mountain ranges also receive precipitation upwards of 300 cm/yr, decreasing to 150-200 cm/yr throughout much of the California Cascades and northern Sierra Nevada (Schoenherr 1992). In the coastal ranges and Cascade ranges of British Columbia, Washington, and northern Oregon heavy precipitation leads to persistent snowpack, and therefore whitebark pine is often restricted to exposed ridges of the subalpine zone or drier sites in the rain shadow of these ranges where it commonly grows in association with subalpine fir (Abies lasiocarpa), Engelmann spruce (Picea engelmannii), and lodgepole pine (Pinus contorta). Whitebark pine is also a minor component of moister subalpine sites, or in mixed subalpine forests at lower elevations. Moister subalpine sites west of the Cascade crest in the southern Washington and northern Oregon Cascades have mountain hemlock (Tsuga mertensiana) and whitebark pine in association on some of the highest and most exposed slopes (Diaz et al.