The Flora of Prince Albert National Park (An Annotated Catalogue of the Vascular Plants Recorded Within the Park Boundaries)
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Willows of Interior Alaska
1 Willows of Interior Alaska Dominique M. Collet US Fish and Wildlife Service 2004 2 Willows of Interior Alaska Acknowledgements The development of this willow guide has been made possible thanks to funding from the U.S. Fish and Wildlife Service- Yukon Flats National Wildlife Refuge - order 70181-12-M692. Funding for printing was made available through a collaborative partnership of Natural Resources, U.S. Army Alaska, Department of Defense; Pacific North- west Research Station, U.S. Forest Service, Department of Agriculture; National Park Service, and Fairbanks Fish and Wildlife Field Office, U.S. Fish and Wildlife Service, Department of the Interior; and Bonanza Creek Long Term Ecological Research Program, University of Alaska Fairbanks. The data for the distribution maps were provided by George Argus, Al Batten, Garry Davies, Rob deVelice, and Carolyn Parker. Carol Griswold, George Argus, Les Viereck and Delia Person provided much improvement to the manuscript by their careful editing and suggestions. I want to thank Delia Person, of the Yukon Flats National Wildlife Refuge, for initiating and following through with the development and printing of this guide. Most of all, I am especially grateful to Pamela Houston whose support made the writing of this guide possible. Any errors or omissions are solely the responsibility of the author. Disclaimer This publication is designed to provide accurate information on willows from interior Alaska. If expert knowledge is required, services of an experienced botanist should be sought. Contents -
East and Central Farming and Forest Region and Atlantic Basin Diversified Farming Region: 12 Lrrs N and S
East and Central Farming and Forest Region and Atlantic Basin Diversified Farming Region: 12 LRRs N and S Brad D. Lee and John M. Kabrick 12.1 Introduction snowfall occurs annually in the Ozark Highlands, the Springfield Plateau, and the St. Francois Knobs and Basins The central, unglaciated US east of the Great Plains to the MLRAs. In the southern half of the region, snowfall is Atlantic coast corresponds to the area covered by LRR N uncommon. (East and Central Farming and Forest Region) and S (Atlantic Basin Diversified Farming Region). These regions roughly correspond to the Interior Highlands, Interior Plains, 12.2.2 Physiography Appalachian Highlands, and the Northern Coastal Plains. The topography of this region ranges from broad, gently rolling plains to steep mountains. In the northern portion of 12.2 The Interior Highlands this region, much of the Springfield Plateau and the Ozark Highlands is a dissected plateau that includes gently rolling The Interior Highlands occur within the western portion of plains to steeply sloping hills with narrow valleys. Karst LRR N and includes seven MLRAs including the Ozark topography is common and the region has numerous sink- Highlands (116A), the Springfield Plateau (116B), the St. holes, caves, dry stream valleys, and springs. The region also Francois Knobs and Basins (116C), the Boston Mountains includes many scenic spring-fed rivers and streams con- (117), Arkansas Valley and Ridges (118A and 118B), and taining clear, cold water (Fig. 12.2). The elevation ranges the Ouachita Mountains (119). This region comprises from 90 m in the southeastern side of the region and rises to 176,000 km2 in southern Missouri, northern and western over 520 m on the Springfield Plateau in the western portion Arkansas, and eastern Oklahoma (Fig. -
Physical Geography of the United States and Canada: a Land of Contrasts S
Chapter 5 Guided Notes _________________________________________________________________________________________ NAME Physical Geography of the United States and Canada: A Land of Contrasts s North America’s vast and varied landscape and abundant resources have attracted immigrants and shaped the development of the United States and Canada. Section 1: Landforms and Resources The United States and Canada have vast lands and abundant resources. These two countries share many of the same landforms. Landscape Influenced Development U.S., Canada: former British colonies, most people speak English Strong economic and political ties with one another Vast Lands Canada second largest country in the world by area; U.S. third Together they cover one-eighth of the earth’s land surface Abundant Resources Landmass and natural resources attract immigrants to both countries U.S. and Canada have developed into global economic powers Many and Varied Landforms All major landforms are found in U.S. and Canada; The two countries share mountain chains and interior plains The Appalachian Highlands Appalachian Mountains run 1,600 miles from Newfoundland to Alabama; More than 400 million years old o include Green and Catskill mountains in the north; Blue Ridge and Great Smoky mountains in the south Erosion has created gentle slopes, peaks from 1,200–2,400 feet The Appalachian Trail is a scenic hiking path along the chain The Interior Lowlands Great Plains extend from Missouri River to Rocky Mountains; Interior Plains extend from Appalachians -
Landforms and Resources
Name _____________________________ Class _________________ Date __________________ Physical Geography of the United States and Canada Section 1 Landforms and Resources Terms and Names Appalachian Mountains major mountain chain in the eastern United States and Canada Great Plains largely treeless area in the interior lowlands Canadian Shield rocky, flat area that surrounds Hudson Bay Rocky Mountains mountain chain in the western United States and Canada Continental Divide line of the highest points in the Rockies that marks the separation between rivers flowing to the east and to the west Great Lakes five large lakes found in the central United States and Canada Mackenzie River Canada’s longest river Before You Read In the last chapter, you read about human geography–the way humans in general relate to their environment. In this section, you will learn about the physical features and resources of the United States and Canada. As You Read Use a graphic organizer to take notes about the landforms and resources of the United States and Canada. LANDSCAPE INFLUENCED The United States and Canada are rich DEVELOPMENT (Page 117) in natural resources. They have much How vast are these countries? fertile soil and water and many forests and The United States and Canada occupy the minerals. This geographic richness has central and northern four-fifths of the attracted immigrants from around the continent of North America. Culturally, the world for centuries. region is known as Anglo America. This is 1. What binds Canada and the United because both countries were colonies of States together? Great Britain at one time and because most of _______________________________ the people speak English. -
Alberta Wetland Classification System – June 1, 2015
Alberta Wetland Classification System June 1, 2015 ISBN 978-1-4601-2257-0 (Print) ISBN: 978-1-4601-2258-7 (PDF) Title: Alberta Wetland Classification System Guide Number: ESRD, Water Conservation, 2015, No. 3 Program Name: Water Policy Branch Effective Date: June 1, 2015 This document was updated on: April 13, 2015 Citation: Alberta Environment and Sustainable Resource Development (ESRD). 2015. Alberta Wetland Classification System. Water Policy Branch, Policy and Planning Division, Edmonton, AB. Any comments, questions, or suggestions regarding the content of this document may be directed to: Water Policy Branch Alberta Environment and Sustainable Resource Development 7th Floor, Oxbridge Place 9820 – 106th Street Edmonton, Alberta T5K 2J6 Phone: 780-644-4959 Email: [email protected] Additional copies of this document may be obtained by contacting: Alberta Environment and Sustainable Resource Development Information Centre Main Floor, Great West Life Building 9920 108 Street Edmonton Alberta Canada T5K 2M4 Call Toll Free Alberta: 310-ESRD (3773) Toll Free: 1-877-944-0313 Fax: 780-427-4407 Email: [email protected] Website: http://esrd.alberta.ca Alberta Wetland Classification System Contributors: Matthew Wilson Environment and Sustainable Resource Development Thorsten Hebben Environment and Sustainable Resource Development Danielle Cobbaert Alberta Energy Regulator Linda Halsey Stantec Linda Kershaw Arctic and Alpine Environmental Consulting Nick Decarlo Stantec Environment and Sustainable Resource Development would also -
Botanical Survey at Reed River Hot Springs, Gates of the Arctic National Park and Preserve (GAAR)
National Park Service U.S. Department of the Interior Natural Resource Stewardship and Science Botanical Survey at Reed River Hot Springs, Gates of the Arctic National Park and Preserve (GAAR) Natural Resource Report NPS/GAAR/NRR—2016/1136 ON THIS PAGE Photograph of two hot water outlets in the uppermost part of the A field. The hot springs are surrounded by azonal, lush fern vegetation. The central part of the A field consisted mainly of broken sinter material and very sparse vegetation. Photograph courtesy of Lisa Strecker ON THE COVER Photograph of A field of the Reed River Hot Springs and the Reed River as seen from the slope above the hot springs. The bright green vegetation of the hot springs area contrasts starkly with plant cover on the other side of the Reed River which is characteristic for the area. Photograph courtesy of Lisa Strecker Botanical Survey at Reed River Hot Springs, Gates of the Arctic National Park and Preserve (GAAR) Natural Resource Report NPS/GAAR/NRR—2016/1136 Lisa Strecker Gates of the Arctic National Park and Preserve 4175 Geist Road Fairbanks, AK 99709 February 2016 U.S. Department of the Interior National Park Service Natural Resource Stewardship and Science Fort Collins, Colorado The National Park Service, Natural Resource Stewardship and Science office in Fort Collins, Colorado, publishes a range of reports that address natural resource topics. These reports are of interest and applicability to a broad audience in the National Park Service and others in natural resource management, including scientists, conservation and environmental constituencies, and the public. -
Laurentide Ice Sheet Retreat Around 8000 Years Ago Occurred Over Western Quebec (700-900 Meters/Year)
The retreat chronology of the Laurentide Ice Sheet during the last 10,000 years and implications for deglacial sea-level rise David Ullman University of Wisconsin-Madison, Department of Geoscience Author Profile Shortcut URL: https://serc.carleton.edu/59463 Location Continent: North America Country: Canada State/Province:Quebec, Labrador City/Town: UTM coordinates and datum: none Setting Climate Setting: Tectonic setting: Type: Chronology Show caption Show caption Show caption Description Much of the world's population is located along the coasts. In a world of changing climate, the rate of sea level rise will determine the ability of these communities to adapt to sea level rise. Perhaps the greatest uncertainty in sea level rise prediction has to do with amount of water melting off of Earth's major ice sheets. Recent decades have seen an accelerated loss of ice from Greenland and Antarctica. These bodies of ice may be prone to change more rapid than expected. Greenland and Antarctica contain enough frozen water, which, if melted could raise sea level by 70 m, but predictions on the rate at which this sea level rise could occur depend on scientists' understanding of the complex physics of ice flow (and on future climate scenarios). Paleoclimate researchers study past climates in hopes of developing a better understanding of our current and future climates. Similarly, understanding past ice sheets will aid in future prediction of ice sheet change. At the end of the Last Glacial Maximum, roughly 20,000 years ago, much of Earth in the northern hemisphere was covered in vast ice sheets. -
A Guide to the Identification of Salix (Willows) in Alberta
A Guide to the identification of Salix (willows) in Alberta George W. Argus 2008 Devonian Botanical Garden Workshop on willow identification Jasper National Park, Alberta 2 Available from: George W. Argus 310 Haskins Rd, Merrickville R3, Ontario, Canada K0G 1N0 email: [email protected] http://aknhp.uaa.alaska.edu/willow/index.html 3 CONTENTS Preface............................................................................................................................... 5 Salicaceae ...........…………………...........……........................................……..........…. 8 Classification ..........……………….…..….................................................….............…. 9 Some Useful Morphological Characters .......................................................….............. 11 Key to the Species.............................................................................................................13 Taxonomic Treatment .........................................................…..……….………............ 18 Glossary .....………………………………………....…..................………...........….... 61 Cited and Selected References ......................................................................................... 64 Salix Web Sites ...................……..................................……..................……............…. 68 Distribution Maps ............................................................................................................ 69 TABLES Table 1. Comparison of Salix athabascensis and Salix pedicellaris .............................. -
Rare Plant Survey of San Juan Public Lands, Colorado
Rare Plant Survey of San Juan Public Lands, Colorado 2005 Prepared by Colorado Natural Heritage Program 254 General Services Building Colorado State University Fort Collins CO 80523 Rare Plant Survey of San Juan Public Lands, Colorado 2005 Prepared by Peggy Lyon and Julia Hanson Colorado Natural Heritage Program 254 General Services Building Colorado State University Fort Collins CO 80523 December 2005 Cover: Imperiled (G1 and G2) plants of the San Juan Public Lands, top left to bottom right: Lesquerella pruinosa, Draba graminea, Cryptantha gypsophila, Machaeranthera coloradoensis, Astragalus naturitensis, Physaria pulvinata, Ipomopsis polyantha, Townsendia glabella, Townsendia rothrockii. Executive Summary This survey was a continuation of several years of rare plant survey on San Juan Public Lands. Funding for the project was provided by San Juan National Forest and the San Juan Resource Area of the Bureau of Land Management. Previous rare plant surveys on San Juan Public Lands by CNHP were conducted in conjunction with county wide surveys of La Plata, Archuleta, San Juan and San Miguel counties, with partial funding from Great Outdoors Colorado (GOCO); and in 2004, public lands only in Dolores and Montezuma counties, funded entirely by the San Juan Public Lands. Funding for 2005 was again provided by San Juan Public Lands. The primary emphases for field work in 2005 were: 1. revisit and update information on rare plant occurrences of agency sensitive species in the Colorado Natural Heritage Program (CNHP) database that were last observed prior to 2000, in order to have the most current information available for informing the revision of the Resource Management Plan for the San Juan Public Lands (BLM and San Juan National Forest); 2. -
Soil Ecoregions in Latin America 5
Chapter 1 Soil EcoregionsSoil Ecoregions in Latin Latin America America Boris Volkoff Martial Bernoux INTRODUCTION Large soil units generally reflect bioclimatic environments (the concept of zonal soils). Soil maps thus represent summary documents that integrate all environmental factors involved. The characteristics of soils represent the environmental factors that control the dynamics of soil organic matter (SOM) and determine both their accumulation and degradation. Soil maps thus rep- resent a basis for quantitative studies on the accumulation processes of soil organic carbon (SOC) in soils in different spatial scales. From this point of view, however, and in particular if one is interested in general scales (large semicontinental regions), soil maps have several disadvantages. First, most soil maps take into account the intrinsic factors of the soils, thus the end results of the formation processes, rather than the processes themselves. These processes are the factors that are directly related to envi- ronmental conditions, whereas the characteristics of the soils can be inher- ited (paleosols and paleoalterations) and might no longer be in equilibrium with the present environment. Second, soils seldom are homogenous spatial entities. The soil cover is in reality a juxtaposition of several distinct soils that might differ to various degrees (from similar to highly contrasted), and might be either genetically linked or entirely disconnected. This spatial heterogeneity reflects the con- ditions in which the soils were formed and is expressed differently accord- ing to the substrates and the topography. The heterogeneity also depends on the duration of evolution of soils and the geomorphologic history, either re- gional or local, as well as on climatic gradients, which are particularly obvi- ous in mountain areas. -
Part 2 – Fruticose Species
Appendix 5.2-1 Vegetation Technical Appendix APPENDIX 5.2‐1 Vegetation Technical Appendix Contents Section Page Ecological Land Classification ............................................................................................................ A5.2‐1‐1 Geodatabase Development .............................................................................................. A5.2‐1‐1 Vegetation Community Mapping ..................................................................................... A5.2‐1‐1 Quality Assurance and Quality Control ............................................................................ A5.2‐1‐3 Limitations of Ecological Land Classification .................................................................... A5.2‐1‐3 Field Data Collection ......................................................................................................... A5.2‐1‐3 Supplementary Results ..................................................................................................... A5.2‐1‐4 Rare Vegetation Species and Rare Ecological Communities ........................................................... A5.2‐1‐10 Supplementary Desktop Results ..................................................................................... A5.2‐1‐10 Field Methods ................................................................................................................. A5.2‐1‐16 Supplementary Results ................................................................................................... A5.2‐1‐17 Weed Species -
Overwintering Hosts for the Exotic Leafroller
Overwintering Hosts for the Exotic Leafroller Parasitoid, Colpoclypeus florus: Implications for Habitat Manipulation to Augment Biological Control of Leafrollers in Pome Fruits Author(s): R. S. Pfannenstiel, T. R. Unruh and J. F. Brunner Source: Journal of Insect Science, 10(75):1-13. 2010. Published By: Entomological Society of America DOI: http://dx.doi.org/10.1673/031.010.7501 URL: http://www.bioone.org/doi/full/10.1673/031.010.7501 BioOne (www.bioone.org) is a nonprofit, online aggregation of core research in the biological, ecological, and environmental sciences. BioOne provides a sustainable online platform for over 170 journals and books published by nonprofit societies, associations, museums, institutions, and presses. Your use of this PDF, the BioOne Web site, and all posted and associated content indicates your acceptance of BioOne’s Terms of Use, available at www.bioone.org/page/terms_of_use. Usage of BioOne content is strictly limited to personal, educational, and non-commercial use. Commercial inquiries or rights and permissions requests should be directed to the individual publisher as copyright holder. BioOne sees sustainable scholarly publishing as an inherently collaborative enterprise connecting authors, nonprofit publishers, academic institutions, research libraries, and research funders in the common goal of maximizing access to critical research. Journal of Insect Science: Vol. 10 | Article 75 Pfannenstiel et al. Overwintering hosts for the exotic leafroller parasitoid, Colpoclypeus florus: Implications for habitat manipulation to augment biological control of leafrollers in pome fruits R. S. Pfannenstiel1,2,3a, T. R. Unruh2, and J. F. Brunner1 1Tree Fruit Research and Extension Center, Washington State University, 1100 N.