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Amelanchierspp. Family: Rosaceae Serviceberry
Amelanchier spp. Family: Rosaceae Serviceberry The genus Amelanchier contains about 16 species native to North America [5], Mexico [2], and Eurasia to northern Africa [4]. The word amelanchier is derived from the French common name amelanche of the European serviceberry, Amelanchier ovalis. Amelanchier alnifolia-juneberry, Pacific serviceberry, pigeonberry, rocky mountain servicetree, sarvice, sarviceberry, saskatoon, saskatoon serviceberry, western service, western serviceberry , western shadbush Amelanchier arborea-Allegheny serviceberry, apple shadbush, downy serviceberry , northern smooth shadbush, shadblow, shadblown serviceberry, shadbush, shadbush serviceberry Amelanchier bartramiana-Bartram serviceberry Amelanchier canadensis-American lancewood, currant-tree, downy serviceberry, Indian cherry, Indian pear, Indian wild pear, juice plum, juneberry, may cherry, sugar plum, sarvice, servicetree, shadberry, shadblow, shadbush, shadbush serviceberry, shadflower, thicket serviceberry Amelanchier florida-Pacific serviceberry Amelanchier interior-inland serviceberry Amelanchier sanguinea-Huron serviceberry, roundleaf juneberry, roundleaf serviceberry , shore shadbush Amelanchier utahensis-Utah serviceberry Distribution In North America throughout upper elevations and temperate forests. The Tree Serviceberry is a shrub or tree that reaches a height of 40 ft (12 m) and a diameter of 2 ft (0.6 m). It grows in many soil types and occurs from swamps to mountainous hillsides. It flowers in early spring, producing delicate white flowers, making -
Late Cenozoic Paleogeographic Evolution of Northeastern Nevada: Evidence from the Sedimentary Basins
Late Cenozoic paleogeographic evolution of northeastern Nevada: Evidence from the sedimentary basins Alan R. Wallace* U.S. Geological Survey, MS 176, Mackay School of Earth Sciences and Engineering, University of Nevada, Reno, Nevada 89557, USA Michael E. Perkins* Department of Geology and Geophysics, University of Utah, Salt Lake City, Utah 84112, USA Robert J. Fleck* U.S. Geological Survey, 345 Middlefi eld Road, Menlo Park, California 94025, USA ABSTRACT lier faults are more pronounced east of the hot-spring deposits formed at and near the Tuscarora Mountains, possibly refl ecting a paleosurface in the Chimney, Ivanhoe, and Field and geochronologic studies of Neo- hanging-wall infl uence related to uplift of the Carlin basins as those basins were forming. gene sedimentary basins in northeastern Ruby Mountains-East Humboldt core com- The Neogene geologic and landscape evolu- Nevada document the paleogeographic and plex on the east side of the Elko basin. The tion had variable effects on all of these depos- geologic evolution of this region and the later faults are concentrated along the north- its, including uplift, weathering, supergene effects on major mineral deposits. The broad northwest–trending northern Nevada rift enrichment, erosion, and burial, depending area that includes the four middle Miocene west of the Tuscarora Mountains. The area on the events at any particular deposit. As basins studied—Chimney, Ivanhoe, Car- west of the rift contains major tilted horsts such, this study documents the importance of lin, and Elko, from west to east—was an and alluvium-fi lled grabens, and differential evaluating post-mineralization processes at upland that underwent prolonged middle extension between this more highly extended both regional and local scales when exploring Tertiary exposure and moderate erosion. -
Amelanchier Canadensis
AmelanchierAmelanchier canadensiscanadensis ShadblowShadblow serviceberry,serviceberry, CanadianCanadian serviceberry,serviceberry, DownyDowny serviceberry,serviceberry, Shadbush,Shadbush, Juneberry,Juneberry, ChuckleberryChuckleberry Amelanchier canadensis(Shadblow serviceberry) is native to South Canada and the eastern United States. The shrub was introduced in Europe in 1746. The Shadblow serviceberry grows up to 5 to 6 metres tall and wide with a finely branched, wide vase-shaped crown. Before the leaves start to sprout, the Amelanchier canadensisblooms bountifully racemes of white flowers that hang over slightly. In late July, it bears red-violet to blue-black fruits that are edible. The leaves are relatively large and bud in a lovely bronze-red. In the summer, the Shadblow serviceberry has green leaves with a grey-green underside. The autumn colours are yellow-orange to brown and less striking than those of other serviceberry shrubs. The species has a preference for sunlight and moist, humous, slightly acidic soil. It will tolerate a temporarily dry environment, as well as strong wind. That makes Amelanchier canadensis very suitable for use in containers and roof gardens. SEASONAL COLOURS jan feb mar apr mei jun jul aug sep okt nov dec TYPES OF PLANTING Tree types: fruit trees, solitary shrubs | Topiary on stem: multi-stem umbrella USE Location: park, central reservation, in containers, roof garden, large garden, small garden, patio, cemetery, countryside, ecological zone | Pavement: none, open | Planting concepts: Eco planting, -
Plant Collecting Expedition for Berry Crop Species Through Southeastern
Plant Collecting Expedition for Berry Crop Species through Southeastern and Midwestern United States June and July 2007 Glassy Mountain, South Carolina Participants: Kim E. Hummer, Research Leader, Curator, USDA ARS NCGR 33447 Peoria Road, Corvallis, Oregon 97333-2521 phone 541.738.4201 [email protected] Chad E. Finn, Research Geneticist, USDA ARS HCRL, 3420 NW Orchard Ave., Corvallis, Oregon 97330 phone 541.738.4037 [email protected] Michael Dossett Graduate Student, Oregon State University, Department of Horticulture, Corvallis, OR 97330 phone 541.738.4038 [email protected] Plant Collecting Expedition for Berry Crops through the Southeastern and Midwestern United States, June and July 2007 Table of Contents Table of Contents.................................................................................................................... 2 Acknowledgements:................................................................................................................ 3 Executive Summary................................................................................................................ 4 Part I – Southeastern United States ...................................................................................... 5 Summary.............................................................................................................................. 5 Travelog May-June 2007.................................................................................................... 6 Conclusions for part 1 ..................................................................................................... -
(1987): "Tectonomagmatic Evolution of Cenozoic Extension in the North American Cordillera"
Downloaded from http://sp.lyellcollection.org/ by Frances J Cooper on January 21, 2013 Geological Society, London, Special Publications Tectonomagmatic evolution of Cenozoic extension in the North American Cordillera Brian P. Wernicke, Philip C. England, Leslie J. Sonder and Robert L. Christiansen Geological Society, London, Special Publications 1987, v.28; p203-221. doi: 10.1144/GSL.SP.1987.028.01.15 Email alerting click here to receive free e-mail alerts when service new articles cite this article Permission click here to seek permission to re-use all or request part of this article Subscribe click here to subscribe to Geological Society, London, Special Publications or the Lyell Collection Notes © The Geological Society of London 2013 Downloaded from http://sp.lyellcollection.org/ by Frances J Cooper on January 21, 2013 Tectonomagmatic evolution of Cenozoic extension in the North American Cordillera B.P. Wernicke, R.L. Christiansen, P.C. England & L.J. Sonder SUMMARY: The spatial and temporal distributions of Cenozoic extension and magmatism in the Cordillera suggest that the onset of major crustal extension at a particular latitude was confined to a relatively narrow belt (< 100 km, pre-extension) and followed the onset of intermediate and silicic magmatism by no more than a few million years. Extension began in early Eocene time in southern British Columbia, northern Washington, Idaho and Montana. Farther S, extension began at about the Eocene- Oligocene boundary in the Great Basin and slightly later in the Mojave-Sonora Desert region. The intervening area, at the latitude of Las Vegas, remained quiescent until mid- Miocene time. Compositional and isotopic characteristics of most pre-Miocene magmas are consistent with their containing major components of melted continental crust. -
USDA Plant Guide (Pdf)
Plant Guide stomach problems. Bark and twigs provided a SASKATOON medicine for recovery after childbirth. In Amelanchier alnifolia (Nutt.) combination with other plants, it was used to make a Nutt. ex Roemer contraceptive. The strong and straight-grained wood Plant Symbol = AMAL2 was used to make arrows, digging sticks, spear shafts, tool handles, and seed beaters. Young branches were Contributed By: USDA NRCS National Plant Data twisted into a type of rope. Center & the Biota of North America Program Saskatoon is attractive as an ornamental shrub or may be trimmed as a hedge. It is an important species for reclamation, wildlife, watershed, and shelterbelt plantings. It can be started from seed or vegetative cuttings. Status Please consult the PLANTS Web site and your State Department of Natural Resources for this plant’s current status, such as, state noxious status and wetland indicator values. Description General: Rose Family (Rosaceae). Native shrubs or small trees growing to 7 meters high, variable in growth form, forming thickets, mats, or clumps, the William R. Hewlitt underground portions including a massive root © California Academy of Sciences crown, horizontal and vertical rhizomes, and an @ CalPhotos extensive root system; bark: thin, light brown and tinged with red, smooth or shallowly fissured. Alternate common names Leaves are deciduous, simple, alternate, ovate to Saskatoon service-berry, service-berry, juneberry, nearly round, 2.5-3 cm long, with lateral, parallel shadbush veins in 8-13 pairs, the margins coarsely serrate or dentate to below middle or sometimes entire or with Uses only a few small teeth at the top. Flowers are in Saskatoon is planted as an ornamental and to produce short, dense, 5-15-flowered, upright racemes, the commercial fruit crops. -
(Rosaceae), I. Differentiation of Mespilus and Crataegus
Phytotaxa 257 (3): 201–229 ISSN 1179-3155 (print edition) http://www.mapress.com/j/pt/ PHYTOTAXA Copyright © 2016 Magnolia Press Article ISSN 1179-3163 (online edition) http://dx.doi.org/10.11646/phytotaxa.257.3.1 STUDIES IN MESPILUS, CRATAEGUS, AND ×CRATAEMESPILUS (ROSACEAE), I. DIFFERENTIATION OF MESPILUS AND CRATAEGUS, EXPANSION OF ×CRATAEMESPILUS, WITH SUPPLEMENTARY OBSERVATIONS ON DIFFERENCES BETWEEN THE CRATAEGUS AND AMELANCHIER CLADES JAMES B. PHIPPS Department of Biology, The University of Western Ontario, London, Ontario N6A 5B7, Canada; email: [email protected] Abstract The paper argues the position for retaining a monotypic Mespilus, i.e., in the sense of M. germanica, the medlar. Recent cladistic papers lend support for Mespilus being sister to Crataegus, and there is a clear morphological distinction from Cra- taegus, emphasized by adaptation to carnivore frugivory. Mespilus secured, the paper then treats each of the known hybrids between Mespilus and Crataegus, making the new combination Crataemespilus ×canescens (J.B. Phipps) J.B. Phipps. Keywords: Crataemespilus ×canescens (J.B. Phipps) J.B. Phipps comb. nov.; inflorescence position; medlar; Mespilus a folk-genus; Mespilus distinct from Crataegus; Rosaceae; taxonomic history of Mespilus Introduction The author has a long-standing interest in generic delimitation in the Maloid genera of the Rosaceae (Maleae Small, formerly Maloideae C. Weber, Pyrinae Dumort.), as shown particularly in a series of papers with K. Robertson, J. Rohrer, and P.G. Smith (Phipps et al. 1990, 1991; Robertson at al. 1991, 1992; Rohrer at al. 1991, 1994) which treated all 28 genera of Maleae as recognised by us. There is also a revisionary treatment of New World Heteromeles M.J. -
Edibles Shrubstrees for Sale
# Common Name Latin Name 1 Saskatoon Serviceberry Amelanchier alnifolia 'Regent' 2 Juneberry Amelanchier alnifolia 'Northline' 3 Juneberry Amelanchier alnifolia 'Smoky' 4 Juneberry Amelanchier alnifolia 'Smoky' 5 Shadblow Serviceberry Amelanchier canadensis 'Prince William' 6 Shadblow Serviceberry Amelanchier canadensis 'Success' 7 Running Serviceberry Amelanchier stolonifera 'Fergie' 8 Serviceberry Amelanchier grandiflora 'Autumn Brilliance' 9 Black Chokeberry Aronia melanocarpa 'Nero' 10 PawPaw Asimina triloba unknown 11 PawPaw Michigan cultivar 12 PawPaw Asimina triloba 'Wilson' 13 PawPaw Asimina triloba 'Sunflower' 14 Cornelian Cherry Cornus mas unknown 15 Cornelian Cherry Cornus mas 'Pioneer' 16 Cornelian Cherry Cornus mas 'Elegant' 17 Cornelian Cherry Cornus mas 'Yellow' 18 American Filbert (Hazelnut) Corylus americana 'Winkler' 19 American Hazelnut Corylus americana (AMHA_PP_18‐24) 20 American Hazelnut Corylus americana 'Ecos' 21 American Hazelnut Corylus americana 'Precocious' 22 Hazelbert Corylus 'Winkler' x 'Skinner' 23 Contorted filbert Corylus avellana 'contorta' 24 Hybrid Hazelnut Corylus avellana x Americana 25 Gumi/Cherry Elaeagnus Elaeagnus multiflora 'Red Gem' 26 Autumn Olive Bush Elaeagnus umbellata 'garnet 27 Hawthorne Hawthorne pinnatifida 'Big Golden Star' 28 Sea Buckthorn Hippophae rhamnoides 'Golden Sweet Female' 29 Sea Buckthorn Hippophae rhamnoides 'Hergo Female' 30 Blue Honeysuckle Lonicera caerulea edulis 'Blue Pacific' 31 Blue Honeysuckle Lonicera caerulea edulis 'Kamchatka' 32 Medlar Mespilus germanica 'Breda -
Amelanchier Laevis Allegheny Serviceberry1 Edward F
Fact Sheet ST-75 November 1993 Amelanchier laevis Allegheny Serviceberry1 Edward F. Gilman and Dennis G. Watson2 INTRODUCTION The Allegheny Serviceberry grows in shade or partial shade as an understory tree (Fig. 1). The small tree grows 30 to 40 feet tall and spreads 15 to 20 feet. Multiple stems are upright and highly branched forming a dense shrub, or if properly pruned a small tree. The tree is short-lived, has a rapid growth rate, and can be used as a filler plant or to attract birds. The main ornamental feature is the white flowers borne in drooping clusters in mid spring. The purplish black berries are sweet and juicy but are soon eaten by birds. The fall color is yellow to red. It is well- adapted for planting beneath power lines due to its small size. GENERAL INFORMATION Scientific name: Amelanchier laevis Pronunciation: am-meh-LANG-kee-er LEE-viss Common name(s): Allegheny Serviceberry Family: Rosaceae USDA hardiness zones: 5 through 8 (Fig. 2) Figure 1. Middle-aged Allegheny Serviceberry. Origin: native to North America Uses: container or above-ground planter; near a deck or patio; specimen Crown density: moderate Availability: somewhat available, may have to go out Growth rate: medium of the region to find the tree Texture: fine DESCRIPTION Foliage Height: 30 to 40 feet Leaf arrangement: alternate (Fig. 3) Spread: 15 to 20 feet Leaf type: simple Crown uniformity: irregular outline or silhouette Leaf margin: serrate Crown shape: upright; vase shape 1. This document is adapted from Fact Sheet ST-75, a series of the Environmental Horticulture Department, Florida Cooperative Extension Service, Institute of Food and Agricultural Sciences, University of Florida. -
Carlin-Type Gold Deposits in Nevada: Critical Geologic Characteristics and Viable Models
©2005 Society of Economic Geologists, Inc. Economic Geology 100th Anniversary Volume pp. 451–484 Carlin-Type Gold Deposits in Nevada: Critical Geologic Characteristics and Viable Models JEAN S. CLINE,† University of Nevada, Las Vegas, 4505 Maryland Parkway, Box 454010, Las Vegas, Nevada 89154-4010 ALBERT H. HOFSTRA, Mineral Resources Program, U.S. Geological Survey, Mail Stop 973, Box 25046, Denver, Colorado 80225 JOHN L. MUNTEAN, Nevada Bureau of Mines and Geology, Mail Stop 178, University of Nevada, Reno, Nevada 89557-0088 RICHARD M. TOSDAL, AND KENNETH A. HICKEY Mineral Deposit Research Unit, University of British Columbia, 6339 Stores Road, Vancouver, British Columbia, Canada V6T 1Z4 Abstract Carlin-type Au deposits in Nevada have huge Au endowments that have made the state, and the United States, one of the leading Au producers in the world. Forty years of mining and numerous studies have pro- vided a detailed geologic picture of the deposits, yet a comprehensive and widely accepted genetic model re- mains elusive. The genesis of the deposits has been difficult to determine owing to difficulties in identifying and analyzing the fine-grained, volumetrically minor, and common ore and gangue minerals, and because of postore weathering and oxidation. In addition, other approximately contemporaneous precious metal deposits have overprinted, or are overprinted by, Carlin-type mineralization. Recent geochronological studies have led to a consensus that the Nevada deposits formed ~42 to 36 m.y. ago, and the deposits can now be evaluated in the context of their tectonic setting. Continental rifting and deposi- tion of a passive margin sequence followed by compressional orogenies established a premineral architecture of steeply dipping fluid conduits, shallow, low dipping “traps” and reactive calcareous host rocks. -
Flora Mediterranea 26
FLORA MEDITERRANEA 26 Published under the auspices of OPTIMA by the Herbarium Mediterraneum Panormitanum Palermo – 2016 FLORA MEDITERRANEA Edited on behalf of the International Foundation pro Herbario Mediterraneo by Francesco M. Raimondo, Werner Greuter & Gianniantonio Domina Editorial board G. Domina (Palermo), F. Garbari (Pisa), W. Greuter (Berlin), S. L. Jury (Reading), G. Kamari (Patras), P. Mazzola (Palermo), S. Pignatti (Roma), F. M. Raimondo (Palermo), C. Salmeri (Palermo), B. Valdés (Sevilla), G. Venturella (Palermo). Advisory Committee P. V. Arrigoni (Firenze) P. Küpfer (Neuchatel) H. M. Burdet (Genève) J. Mathez (Montpellier) A. Carapezza (Palermo) G. Moggi (Firenze) C. D. K. Cook (Zurich) E. Nardi (Firenze) R. Courtecuisse (Lille) P. L. Nimis (Trieste) V. Demoulin (Liège) D. Phitos (Patras) F. Ehrendorfer (Wien) L. Poldini (Trieste) M. Erben (Munchen) R. M. Ros Espín (Murcia) G. Giaccone (Catania) A. Strid (Copenhagen) V. H. Heywood (Reading) B. Zimmer (Berlin) Editorial Office Editorial assistance: A. M. Mannino Editorial secretariat: V. Spadaro & P. Campisi Layout & Tecnical editing: E. Di Gristina & F. La Sorte Design: V. Magro & L. C. Raimondo Redazione di "Flora Mediterranea" Herbarium Mediterraneum Panormitanum, Università di Palermo Via Lincoln, 2 I-90133 Palermo, Italy [email protected] Printed by Luxograph s.r.l., Piazza Bartolomeo da Messina, 2/E - Palermo Registration at Tribunale di Palermo, no. 27 of 12 July 1991 ISSN: 1120-4052 printed, 2240-4538 online DOI: 10.7320/FlMedit26.001 Copyright © by International Foundation pro Herbario Mediterraneo, Palermo Contents V. Hugonnot & L. Chavoutier: A modern record of one of the rarest European mosses, Ptychomitrium incurvum (Ptychomitriaceae), in Eastern Pyrenees, France . 5 P. Chène, M. -
Mineralogy of Non-Silicified Fossil Wood
Article Mineralogy of Non-Silicified Fossil Wood George E. Mustoe Geology Department, Western Washington University, Bellingham, WA 98225, USA; [email protected]; Tel: +1-360-650-3582 Received: 21 December 2017; Accepted: 27 February 2018; Published: 3 March 2018 Abstract: The best-known and most-studied petrified wood specimens are those that are mineralized with polymorphs of silica: opal-A, opal-C, chalcedony, and quartz. Less familiar are fossil woods preserved with non-silica minerals. This report reviews discoveries of woods mineralized with calcium carbonate, calcium phosphate, various iron and copper minerals, manganese oxide, fluorite, barite, natrolite, and smectite clay. Regardless of composition, the processes of mineralization involve the same factors: availability of dissolved elements, pH, Eh, and burial temperature. Permeability of the wood and anatomical features also plays important roles in determining mineralization. When precipitation occurs in several episodes, fossil wood may have complex mineralogy. Keywords: fossil wood; mineralogy; paleobotany; permineralization 1. Introduction Non-silica minerals that cause wood petrifaction include calcite, apatite, iron pyrites, siderite, hematite, manganese oxide, various copper minerals, fluorite, barite, natrolite, and the chromium- rich smectite clay mineral, volkonskoite. This report provides a broad overview of woods fossilized with these minerals, describing specimens from world-wide locations comprising a diverse variety of mineral assemblages. Data from previously-undescribed fossil woods are also presented. The result is a paper that has a somewhat unconventional format, being a combination of literature review and original research. In an attempt for clarity, the information is organized based on mineral composition, rather than in the format of a hypothesis-driven research report.