Jun 0 8 1993
Total Page:16
File Type:pdf, Size:1020Kb

Load more
Recommended publications
-
Geologic Maps of the Eastern Alaska Range, Alaska, (44 Quadrangles, 1:63360 Scale)
Report of Investigations 2015-6 GEOLOGIC MAPS OF THE EASTERN ALASKA RANGE, ALASKA, (44 quadrangles, 1:63,360 scale) descriptions and interpretations of map units by Warren J. Nokleberg, John N. Aleinikoff, Gerard C. Bond, Oscar J. Ferrians, Jr., Paige L. Herzon, Ian M. Lange, Ronny T. Miyaoka, Donald H. Richter, Carl E. Schwab, Steven R. Silva, Thomas E. Smith, and Richard E. Zehner Southeastern Tanana Basin Southern Yukon–Tanana Upland and Terrane Delta River Granite Jarvis Mountain Aurora Peak Creek Terrane Hines Creek Fault Black Rapids Glacier Jarvis Creek Glacier Subterrane - Southern Yukon–Tanana Terrane Windy Terrane Denali Denali Fault Fault East Susitna Canwell Batholith Glacier Maclaren Glacier McCallum Creek- Metamorhic Belt Meteor Peak Slate Creek Thrust Broxson Gulch Fault Thrust Rainbow Mountain Slana River Subterrane, Wrangellia Terrane Phelan Delta Creek River Highway Slana River Subterrane, Wrangellia Terrane Published by STATE OF ALASKA DEPARTMENT OF NATURAL RESOURCES DIVISION OF GEOLOGICAL & GEOPHYSICAL SURVEYS 2015 GEOLOGIC MAPS OF THE EASTERN ALASKA RANGE, ALASKA, (44 quadrangles, 1:63,360 scale) descriptions and interpretations of map units Warren J. Nokleberg, John N. Aleinikoff, Gerard C. Bond, Oscar J. Ferrians, Jr., Paige L. Herzon, Ian M. Lange, Ronny T. Miyaoka, Donald H. Richter, Carl E. Schwab, Steven R. Silva, Thomas E. Smith, and Richard E. Zehner COVER: View toward the north across the eastern Alaska Range and into the southern Yukon–Tanana Upland highlighting geologic, structural, and geomorphic features. View is across the central Mount Hayes Quadrangle and is centered on the Delta River, Richardson Highway, and Trans-Alaska Pipeline System (TAPS). Major geologic features, from south to north, are: (1) the Slana River Subterrane, Wrangellia Terrane; (2) the Maclaren Terrane containing the Maclaren Glacier Metamorphic Belt to the south and the East Susitna Batholith to the north; (3) the Windy Terrane; (4) the Aurora Peak Terrane; and (5) the Jarvis Creek Glacier Subterrane of the Yukon–Tanana Terrane. -
P1616 Text-Only PDF File
A Geologic Guide to Wrangell–Saint Elias National Park and Preserve, Alaska A Tectonic Collage of Northbound Terranes By Gary R. Winkler1 With contributions by Edward M. MacKevett, Jr.,2 George Plafker,3 Donald H. Richter,4 Danny S. Rosenkrans,5 and Henry R. Schmoll1 Introduction region—his explorations of Malaspina Glacier and Mt. St. Elias—characterized the vast mountains and glaciers whose realms he invaded with a sense of astonishment. His descrip Wrangell–Saint Elias National Park and Preserve (fig. tions are filled with superlatives. In the ensuing 100+ years, 6), the largest unit in the U.S. National Park System, earth scientists have learned much more about the geologic encompasses nearly 13.2 million acres of geological won evolution of the parklands, but the possibility of astonishment derments. Furthermore, its geologic makeup is shared with still is with us as we unravel the results of continuing tectonic contiguous Tetlin National Wildlife Refuge in Alaska, Kluane processes along the south-central Alaska continental margin. National Park and Game Sanctuary in the Yukon Territory, the Russell’s superlatives are justified: Wrangell–Saint Elias Alsek-Tatshenshini Provincial Park in British Columbia, the is, indeed, an awesome collage of geologic terranes. Most Cordova district of Chugach National Forest and the Yakutat wonderful has been the continuing discovery that the disparate district of Tongass National Forest, and Glacier Bay National terranes are, like us, invaders of a sort with unique trajectories Park and Preserve at the north end of Alaska’s panhan and timelines marking their northward journeys to arrive in dle—shared landscapes of awesome dimensions and classic today’s parklands. -
Languages of the World--Native America
REPOR TRESUMES ED 010 352 46 LANGUAGES OF THE WORLD-NATIVE AMERICA FASCICLE ONE. BY- VOEGELIN, C. F. VOEGELIN, FLORENCE N. INDIANA UNIV., BLOOMINGTON REPORT NUMBER NDEA-VI-63-5 PUB DATE JUN64 CONTRACT MC-SAE-9486 EDRS PRICENF-$0.27 HC-C6.20 155P. ANTHROPOLOGICAL LINGUISTICS, 6(6)/1-149, JUNE 1964 DESCRIPTORS- *AMERICAN INDIAN LANGUAGES, *LANGUAGES, BLOOMINGTON, INDIANA, ARCHIVES OF LANGUAGES OF THE WORLD THE NATIVE LANGUAGES AND DIALECTS OF THE NEW WORLD"ARE DISCUSSED.PROVIDED ARE COMPREHENSIVE LISTINGS AND DESCRIPTIONS OF THE LANGUAGES OF AMERICAN INDIANSNORTH OF MEXICO ANDOF THOSE ABORIGINAL TO LATIN AMERICA..(THIS REPOR4 IS PART OF A SEkIES, ED 010 350 TO ED 010 367.)(JK) $. DEPARTMENT OF HEALTH,EDUCATION nib Office ofEduc.442n MD WELNicitt weenment Lasbeenreproduced a l l e a l O exactly r o n o odianeting es receivromed f the Sabi donot rfrocestarity it. Pondsof viewor position raimentofficial opinions or pritcy. Offkce ofEducation rithrppologicalLinguistics Volume 6 Number 6 ,Tune 1964 LANGUAGES OF TEM'WORLD: NATIVE AMER/CAFASCICLEN. A Publication of this ARC IVES OF LANGUAGESor 111-E w oRLD Anthropology Doparignont Indiana, University ANTHROPOLOGICAL LINGUISTICS is designed primarily, butnot exclusively, for the immediate publication of data-oriented papers for which attestation is available in the form oftape recordings on deposit in the Archives of Languages of the World. This does not imply that contributors will bere- stricted to scholars working in the Archives at Indiana University; in fact,one motivation for the publication -
Central and South America Report (1.8
United States NHEERL Environmental Protection Western Ecology Division May 1998 Agency Corvallis OR 97333 ` Research and Development EPA ECOLOGICAL CLASSIFICATION OF THE WESTERN HEMISPHERE ECOLOGICAL CLASSIFICATION OF THE WESTERN HEMISPHERE Glenn E. Griffith1, James M. Omernik2, and Sandra H. Azevedo3 May 29, 1998 1 U.S. Department of Agriculture, Natural Resources Conservation Service 200 SW 35th St., Corvallis, OR 97333 phone: 541-754-4465; email: [email protected] 2 Project Officer, U.S. Environmental Protection Agency 200 SW 35th St., Corvallis, OR 97333 phone: 541-754-4458; email: [email protected] 3 OAO Corporation 200 SW 35th St., Corvallis, OR 97333 phone: 541-754-4361; email: [email protected] A Report to Thomas R. Loveland, Project Manager EROS Data Center, U.S. Geological Survey, Sioux Falls, SD WESTERN ECOLOGY DIVISION NATIONAL HEALTH AND ENVIRONMENTAL EFFECTS RESEARCH LABORATORY OFFICE OF RESEARCH AND DEVELOPMENT U.S. ENVIRONMENTAL PROTECTION AGENCY CORVALLIS, OREGON 97333 1 ABSTRACT Many geographical classifications of the world’s continents can be found that depict their climate, landforms, soils, vegetation, and other ecological phenomena. Using some or many of these mapped phenomena, classifications of natural regions, biomes, biotic provinces, biogeographical regions, life zones, or ecological regions have been developed by various researchers. Some ecological frameworks do not appear to address “the whole ecosystem”, but instead are based on specific aspects of ecosystems or particular processes that affect ecosystems. Many regional ecological frameworks rely primarily on climatic and “natural” vegetative input elements, with little acknowledgement of other biotic, abiotic, or human geographic patterns that comprise and influence ecosystems. -
Description and Interpretation of Geologic Materials from Shotholes Drilled for the Trans-Alaska Crustal Transect Project, Copper River Basin, Alaska, May 1985
DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY Description and Interpretation of Geologic Materials from Shotholes Drilled for the Trans-Alaska Crustal Transect Project, Copper River Basin, Alaska, May 1985 By Jack K. Odum 1 , Lynn A. Yehle 1 , Henry R. Schmoll 1 , and Chuck Gilbert 2 Open-File Report 86-408 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature. Any use of trade names is for descriptive purposes only and does not imply endorsement by the USGS. U.S. Geological Survey HJ.S. Geological Survey Denver, Colorado Menlo Park, California 1986 CONTENTS Page Introduction....................................................... 1 Drilling operations and sampling................................... 1 Interpretation of materials........................................ 4 Description of drill sites and geologic materials from drill holes................................................. 4 CRB 85-23a and b............................................... 4 CRB 85-24...................................................... 6 CRB 85-25...................................................... 10 CRB 85-26...................................................... 12 CRB 85-27...................................................... 14 CRB 85-28...................................................... 14 References cited................................................... 17 ILLUSTRATIONS Figure 1. Location map showing the U.S. Geological Survey shotholes CRB -
Guide to Theecological Systemsof Puerto Rico
United States Department of Agriculture Guide to the Forest Service Ecological Systems International Institute of Tropical Forestry of Puerto Rico General Technical Report IITF-GTR-35 June 2009 Gary L. Miller and Ariel E. Lugo The Forest Service of the U.S. Department of Agriculture is dedicated to the principle of multiple use management of the Nation’s forest resources for sustained yields of wood, water, forage, wildlife, and recreation. Through forestry research, cooperation with the States and private forest owners, and management of the National Forests and national grasslands, it strives—as directed by Congress—to provide increasingly greater service to a growing Nation. The U.S. Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, age, disability, and where applicable sex, marital status, familial status, parental status, religion, sexual orientation genetic information, political beliefs, reprisal, or because all or part of an individual’s income is derived from any public assistance program. (Not all prohibited bases apply to all programs.) Persons with disabilities who require alternative means for communication of program information (Braille, large print, audiotape, etc.) should contact USDA’s TARGET Center at (202) 720-2600 (voice and TDD).To file a complaint of discrimination, write USDA, Director, Office of Civil Rights, 1400 Independence Avenue, S.W. Washington, DC 20250-9410 or call (800) 795-3272 (voice) or (202) 720-6382 (TDD). USDA is an equal opportunity provider and employer. Authors Gary L. Miller is a professor, University of North Carolina, Environmental Studies, One University Heights, Asheville, NC 28804-3299. -
UNITED STATES GEOLOGICAL SURVEY by Open-File Report 85
DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY Generalized Interpretation of Geologic Materials from Shot Roles Drilled for the Trans-Alaska Crustal Transect Project, Copper River Basin and Adjacent Regions, Alaska, by-June 1984 BY 1 Lynn A. yeh1e1, Jack K. Odum , and David Reneau 2 Open-File Report 85-582 This report is preliminary and has not been reviewed for confo~tywith U.S. Geological Survey editorial standards and stratigraphic nomenclature. Any use of trade names is for descriptive purposes only and docs not imply endorsement by the USGS. 'USGS , Denver, Colorado 2~~~~,kalo park, ~alifornia Page introduction^^.^; ................................................. 1 Drilling operations and samplingm.mmmm~~~.mwe~oI~................. Interpretation of materials..mDo~Doo~.o.......................... Description of drill sites and halesweeee........................ W3 84-la. b. and cow.......m...............mm.mm.m.......... CRB 84-2 ...m...m.mm.m..mm.......................oo........... CRB 84-3m.momoommmmmmmmmmmww.~eoo.ooe.oeo ......m...........m. CRB 84-4eoneee ..................m.m.mm..m.mmmmmmmm.mmmmmmm.mm CRB 84.5ereeeee.ee.oeeee.e ................................... CRB 84-6eomoe.eememeee.eeeoeoooomeooooomo ..*oo..ooo*mmmm.mo.. CRB 84.78. b. and cmeeemee................................... CRB 84-8o.emoewo.eeeoe.w ......................m.o........ CRB 84-9eoeomeemwwoowweoeeooeoeoeoo.eeo~ee.oe.eeeoo.oeo~ ..ooe CRB 84-10.. ......................mm.........o.mmm.....m.... .. CRB 84-11 ................................................... -
Assessment of the Vulnerability of Forest Ecosystems to Climate Change in Mexico
CLIMATE RESEARCH Vol. 9: 87-93, 1997 Published December 29 Clim Res Assessment of the vulnerability of forest ecosystems to climate change in Mexico Lourdes Villers-Ruiz*, Irma Trejo-Vazquez Instituto de Geografia, Universidad Nacional Autonoma de Mexico, Apartado Postal 20850, 04510 Mexico. D.F. Mexico ABSTRACT. An assessment of the vulnerability of forest ecosystems in Mexico to climate change is car- ried out on the basis of the scenarios projected by 3 climate models. A vegetation classification was per- formed according to 2 models, the Holdridge Life Zone Classification and the so-called Mexican Clas- sification (a climate-vegetation classification based on typologies developed for Mexico). Projections of climate models were based on a doubled CO2 concentration condition. The models used were: the CCCM, which estimates an average increase in temperature for the country of 2.8"C and a decrease in annual precipitation of 7 %; the GFDL-R30, which estimates an increase in both parameters by 3.2"C and 20% respectively; and a sensitivity model in which a homogeneous increase of 2°C in temperature and a 10% decrease in precipitation are applied throughout the country. In general, the cool temperate and warm temperate ecosystems were the most affected and tended to disappear under the conditions of the 3 scenarios In contrast, the dry and very dry tropical forests and the warm thorn woodlands tended to occupy larger areas than at present, particularly under the conditions projected by the CCCM model. However, under the GFDL-derived scenario an increase in the distribution of moist and wet forests, which would be favoured by an increase in precipitation, was predicted. -
West Copper River Delta Landscape Assessment Cordova Ranger District Chugach National Forest 03/18/2003 Updated 04/19/2007
West Copper River Delta Landscape Assessment Cordova Ranger District Chugach National Forest 03/18/2003 updated 04/19/2007 Copper River Delta – circa 1932 – photo courtesy of Perry Davis Team: Susan Kesti - Team Leader, writer-editor, vegetation Milo Burcham – Wildlife resources, Subsistence Bruce Campbell – Lands, Special Uses Dean Davidson – Soils, Geology Rob DeVelice – Succession, Ecology Carol Huber – Minerals, Geology, Mining Tim Joyce – Fish subsistence Dirk Lang – Fisheries Bill MacFarlane – Hydrology, Water Quality Dixon Sherman – Recreation Linda Yarborough – Heritage Resources Table of Contents Executive Summary...........................................................................................vi Chapter 1 – Introduction ....................................................................................1 Purpose.............................................................................................................1 The Analysis Area .............................................................................................1 Legislative History .............................................................................................3 Relationship to the revised Chugach Land and Resource Management Plan...4 Chapter 2 – Analysis Area Description .............................................................7 Physical Characteristics ....................................................................................7 Location .........................................................................................................7 -
Department of the Interior United States Geological Survey
DEPARTMENT OF THE INTERIOR UNITED STATES GEOLOGICAL SURVEY Description and Interpretation of Geologic Materi a1 s from Shothol es Dri 11ed for the Trans-Alaska Crustal Transect Project, Copper River Elasin. Alaska, May 1985 Jack K. ~ul,Lynn A. lehlel, Henry R. Schmoll 1 and Chuck ~ilbert2 Open-Fi le Report 86-408 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey edi toria1 standards and stratigraphic nomenclature. Any use of trade names is for descriptive purposes only and does not imply endorsement by the USGS. ~u.s. Geological Survey US. Geological Survey Denver, Colorado Menlo Park, Cal ifornia CONTENTS Page Introduction....................................................... 1 Drilling operations and sampling ................................... 1 Interpretation of materials ........................................ 4 Description of drill sites and geologic materials from drill holes ................................................ 4 CRB 85-23a and b ..e............................................ 4 CRB 85.24 .................................... 6 CRB 85.25 ...................................................... 10 CRB 85.26 ...................................................... 12 CRB 85-27 ......................................................14 CRB 85.28 ..............................~........... 14 References cited................................................. -17 ILLUSTRATIONS Figure 1. Location map showing the U.S. Geological Survey shotholes CRB 85.23a ................................. -
Changes of Major Terrestrial Ecosystems in China Since 1960
Global and Planetary Change 48 (2005) 287–302 www.elsevier.com/locate/gloplacha Changes of major terrestrial ecosystems in China since 1960 Tian Xiang YueT, Ze Meng Fan, Ji Yuan Liu Institute of Geographical Sciences and Natural Resources Research, Chinese Academy of Sciences, Jia No. 11, Datun, Anwai, 100101 Beijing, China Abstract Daily temperature and precipitation data since 1960 are selected from 735 weather stations that are scattered over China. After comparatively analyzing relative interpolation methods, gradient-plus-inverse distance squared (GIDS) is selected to create temperature surfaces and Kriging interpolation method is selected to create precipitation surfaces. Digital elevation model of China is combined into Holdridge Life Zone (HLZ) model on the basis of simulating relationships between temperature and elevation in different regions of China. HLZ model is operated on the created temperature and precipitation surfaces in ARC/ INFO environment. Spatial pattern of major terrestrial ecosystems in China and its change in the four decades of 1960s, 1970s, 1980s and 1990s are analyzed in terms of results from operating HLZ model. The results show that HLZ spatial pattern in China has had a great change since 1960. For instance, nival area and subtropical thorn woodland had a rapid decrease on an average and they might disappear in 159 years and 96 years, respectively, if their areas would decrease at present rate. Alpine dry tundra and cool temperate scrub continuously increased in the four decades and the decadal increase rates are, respectively, 13.1% and 3.4%. HLZ patch connectivity has a continuous increase trend and HLZ diversity has a continuous decrease trend on the average. -
Climatic Traits on Daily Clearness and Cloudiness Indices
Climatic traits on daily clearness and cloudiness indices Estefanía Muñoz1 and Andrés Ochoa1 1Universidad Nacional de Colombia, Medellín Correspondence: Estefanía Muñoz ([email protected]) Abstract. Solar radiation has a crucial role in photosynthesis, evapotranspiration and other biogeochemical processes. The amount of solar radiation reaching the Earth’s surface is a function of astronomical geometry and atmospheric optics. While the first is deterministic, the latter has a random behaviour caused by highly variable atmospheric components as water and aerosols. In this study, we use daily radiation data (1978-2014) from 37 FLUXNET sites distributed across the globe to inspect 5 for climatic traits in the shape of the probability density function (PDF) of the clear-day (c) and the clearness (k) indices. The analysis was made for shortwave radiation (SW) at all sites and for photosynthetically active radiation (PAR) at 28 sites. We identified three types of PDF, unimodal with low dispersion (ULD), unimodal with high dispersion (UHD) and bimodal (B), with no difference in the PDF type between c and k at each site. Looking for regional patterns in the PDF type we found that latitude, global climate zone and Köppen climate type have a weak and the Holdridge life a stronger relation with c and k 10 PDF types. The existence and relevance of a second mode in the PDF can be explained by the frequency and meteorological mechanisms of rainy days. These results are a frame to develop solar radiation stochastic models for biogeochemical and ecohydrological modeling. 1 Introduction Solar radiation drives most physical, chemical and biological processes at the earth’s surface.