Summer Monsoon Convection in the Himalayan Region: Terrain and Land Cover Effects†
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CEMOZOIC DEPOSITS in the SOUTHERN FOOTHILLS of the SANTA CATALINA MOUNTAINS NEAR TUCSON, ARIZONA Ty Klaus Voelger a Thesis Submi
Cenozoic deposits in the southern foothills of the Santa Catalina Mountains near Tucson, Arizona Item Type text; Thesis-Reproduction (electronic) Authors Voelger, Klaus, 1926- Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 25/09/2021 10:53:10 Link to Item http://hdl.handle.net/10150/551218 CEMOZOIC DEPOSITS IN THE SOUTHERN FOOTHILLS OF THE SANTA CATALINA MOUNTAINS NEAR TUCSON, ARIZONA ty Klaus Voelger A Thesis submitted to the faculty of the Department of Geology in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE in the Graduate College, University of Arizona 1953 Approved; , / 9S~J Director of Thesis ^5ate Univ. of Arizona Library The research on which this thesis is based was com pleted by Mr. Klaus Voelger of Berlin, Germany, while he was studying at the University of Arizona under the program of the Institute of International Education. The final draft was written after Mr. Voelgerf s return to his home in the Russian-occupied zone of Berlin. Difficulties such as a shortage of typing paper of uniform grade and the impossibility of adequate supervision and advice on matters of terminology, punctuation, and English usage account for certain details in which this thesis may depart from stand ards of the Graduate College of the University of Arizona. These details are largely mechanical, and it is felt that they do not detract appreciably from the quality of the research nor the clarity of presentation of the results. -
General Features and Fisheries Potential of Palk Bay, Palk Strait and Its Environs
J. Natn.Sci.Foundation Sri Lanka 2005 33(4): 225-232 FEATURE ARTICLE GENERAL FEATURES AND FISHERIES POTENTIAL OF PALK BAY, PALK STRAIT AND ITS ENVIRONS S. SIVALINGAM* 18, Pamankade Lane, Colombo 6. Abstract: The issue of possible social and environmental serving in the former Department of Fisheries, impacts of the shipping canal proposed for the Palk Bay and Colombo (now Ministry of Fisheries and Aquatic Palk Strait area is a much debated topic. Therefore it is Resources) and also recently when consultation necessary to explore the general features of the said area to assess such impacts when formulating the development and assignments were done in these areas. Other management programmes relevant to the area. This paper available data have also been brought together discussed the general features of the area, its environmental and a comprehensive picture of the general and ecological condition and the fisheries potential in detail features and fisheries potential of the areas so as to give some insight to the reader on this important under study is presented below. topic. This article is based on the data collected from earlier field visits and other published information relevant to the subject. GENERAL FEATURES INTRODUCTION Palk Bay and Palk Strait together (also called Sethusamudram), consist of an area of about Considerable interest has been created in the 17,000km2. This is an almost enclosed shallow water Palk Bay, Palk Strait and its environs recently as body that separates Sri Lanka from the a result of the Indian project to construct a mainland India and opens on the east into the shipping canal to connect Gulf of Mannar BOB ( Figure 1 ). -
Cultural Heritage the Mountains and Foothills of North Carolina Have Over Many Centuries Fostered a Rich Mosaic of Cultural Heritage
Western North Carolina Vitality Index Cultural Heritage www.wncvitalityindex.org The mountains and foothills of North Carolina have over many centuries fostered a rich mosaic of cultural heritage. The birthplace of the Cherokee’s advanced early civilization, the region is home today to the Eastern Band of Cherokee Indians, which continues to preserve many facets of traditional Cherokee culture. Beginning in the eighteenth century, European and African settlers moved into the mountains. The relative isolation of mountain life helped these settlers refine and preserve many traditions, most notably handmade crafts, traditional music, and local agricultural practices. Today, these distinctive cultural legacies are celebrated as living traditions, providing employment to master artists and tradition bearers and drawing tourists from across the globe to experience the region’s craft galleries, music halls, festivals, museums, farms, and local cuisine. photo courtesy of Blue Ridge National this project has been funded by Heritage Area a project of Blue Ridge National Heritage Area Designation A National Heritage Area is a place designated by the United States Congress where natural, cultural, historic, and recreational resources combine to form a cohesive, nationally distinctive landscape arising from patterns of human activity shaped by geography. Currently, there are 49 National Heritage Areas across the United States, where each area shares how their people, resources, and histories come together to provide experiences that “tell America’s story” and to encourage the community to join together around a common theme and promote the cultural, natural, and recreational benefits of the area. In November 2003, Western North Carolina (WNC) was designated the Blue Ridge National Heritage Area in recognition of the region’s agriculture, craft heritage, traditional music, the distinctive living traditions of Cherokee culture, and rich natural heritage, and their significance to the country. -
Ecoregions of New England Forested Land Cover, Nutrient-Poor Frigid and Cryic Soils (Mostly Spodosols), and Numerous High-Gradient Streams and Glacial Lakes
58. Northeastern Highlands The Northeastern Highlands ecoregion covers most of the northern and mountainous parts of New England as well as the Adirondacks in New York. It is a relatively sparsely populated region compared to adjacent regions, and is characterized by hills and mountains, a mostly Ecoregions of New England forested land cover, nutrient-poor frigid and cryic soils (mostly Spodosols), and numerous high-gradient streams and glacial lakes. Forest vegetation is somewhat transitional between the boreal regions to the north in Canada and the broadleaf deciduous forests to the south. Typical forest types include northern hardwoods (maple-beech-birch), northern hardwoods/spruce, and northeastern spruce-fir forests. Recreation, tourism, and forestry are primary land uses. Farm-to-forest conversion began in the 19th century and continues today. In spite of this trend, Ecoregions denote areas of general similarity in ecosystems and in the type, quality, and 5 level III ecoregions and 40 level IV ecoregions in the New England states and many Commission for Environmental Cooperation Working Group, 1997, Ecological regions of North America – toward a common perspective: Montreal, Commission for Environmental Cooperation, 71 p. alluvial valleys, glacial lake basins, and areas of limestone-derived soils are still farmed for dairy products, forage crops, apples, and potatoes. In addition to the timber industry, recreational homes and associated lodging and services sustain the forested regions economically, but quantity of environmental resources; they are designed to serve as a spatial framework for continue into ecologically similar parts of adjacent states or provinces. they also create development pressure that threatens to change the pastoral character of the region. -
Adits, Caves, Karizi-Qanats, and Tunnels in Afghanistan: an Annotated Bibliography by R
Adits, Caves, Karizi-Qanats, and Tunnels in Afghanistan: An Annotated Bibliography by R. Lee Hadden Topographic Engineering Center November 2005 US Army Corps of Engineers 7701 Telegraph Road Alexandria, VA 22315-3864 Adits, Caves, Karizi-Qanats, and Tunnels In Afghanistan Form Approved REPORT DOCUMENTATION PAGE OMB No. 0704-0188 Public reporting burden for this collection of information is estimated to average 1 hour per response, including the time for reviewing instructions, searching existing data sources, gathering and maintaining the data needed, and completing and reviewing this collection of information. Send comments regarding this burden estimate or any other aspect of this collection of information, including suggestions for reducing this burden to Department of Defense, Washington Headquarters Services, Directorate for Information Operations and Reports (0704-0188), 1215 Jefferson Davis Highway, Suite 1204, Arlington, VA 22202-4302. Respondents should be aware that notwithstanding any other provision of law, no person shall be subject to any penalty for failing to comply with a collection of information if it does not display a currently valid OMB control number. PLEASE DO NOT RETURN YOUR FORM TO THE ABOVE ADDRESS. 1. REPORT DATE 30-11- 2. REPORT TYPE Bibliography 3. DATES COVERED 1830-2005 2005 4. TITLE AND SUBTITLE 5a. CONTRACT NUMBER “Adits, Caves, Karizi-Qanats and Tunnels 5b. GRANT NUMBER In Afghanistan: An Annotated Bibliography” 5c. PROGRAM ELEMENT NUMBER 6. AUTHOR(S) 5d. PROJECT NUMBER HADDEN, Robert Lee 5e. TASK NUMBER 5f. WORK UNIT NUMBER 7. PERFORMING ORGANIZATION NAME(S) AND ADDRESS(ES) 8. PERFORMING ORGANIZATION REPORT US Army Corps of Engineers 7701 Telegraph Road Topographic Alexandria, VA 22315- Engineering Center 3864 9.ATTN SPONSORING CEERD / MONITORINGTO I AGENCY NAME(S) AND ADDRESS(ES) 10. -
Geologic Framework of the Catalina Foothills, Outskirts of Tucson (Pima County, Arizona)
GEOLOGIC FRAMEWORK OF THE CATALINA FOOTHILLS, OUTSKIRTS OF TUCSON (PIMA COUNTY, ARIZONA) W.R. DICKINSON Emeritus, Dept. of Geosciences University of Arizona ARIZONA GEOLOGICAL SURVEY CONTRIBUTED MAP CM-99-B MAY 1999 31 p., scale 1 :24,000 TIus report is preliminary and has not been edited or reviewed for confonnity with Arizona Geological Survey standards. ARIZONA GEOLOGICAL SURVEY CONTRIBUTED MAP CM-99-B (31 pp., 1 Plate) Geologic Framework of the Catalina Foothills, Outskirts of Tucson (Pima County, Arizona) [Text and Legend to Accompany 1:24,000 Map] William R. Dickinson, Department of Geosciences, University of Arizona May 1999 Introduction and Purpose Past geologic maps and accounts of the sedimentary, geomorphic, and structural geology of the piedmont of the Santa Catalina Mountains in the outskirts of Tucson by Voelger (1953), Pashley (1966), Davidson (1973), Creasey and Theodore (1975), Banks (1976), Anderson (1987), Pearthree et al. (1988), McKittrick (1988), and Jackson (1989) raised questions about the sedimentary evolution of the foothills belt that were left open or unresolved. Multiple dissected alluvial fans and pediments overlie much older faulted and tilted strata to form Cenozoic sedimentary assemblages of considerable stratigraphic and structural complexity. As a contribution to improved understanding of urban geology in the Tucson metropolitan area, systematic geologic mapping of the piedmont belt was undertaken to establish the overall geologic framework of the Catalina foothills (~ 175 2 km ) at a common scale (1 :24,000). The area studied extends from Oracle Road on the west to the vicinity of Rinconado Road on the east, and from the Rillito River and Tanque Verde Wash northward to the limit of bedrock exposures at the base of the Santa Catalina Mountains. -
The Kingdom of Afghanistan: a Historical Sketch George Passman Tate
University of Nebraska Omaha DigitalCommons@UNO Books in English Digitized Books 1-1-1911 The kingdom of Afghanistan: a historical sketch George Passman Tate Follow this and additional works at: http://digitalcommons.unomaha.edu/afghanuno Part of the History Commons, and the International and Area Studies Commons Recommended Citation Tate, George Passman The kingdom of Afghanistan: a historical sketch, with an introductory note by Sir Henry Mortimer Durand. Bombay: "Times of India" Offices, 1911. 224 p., maps This Monograph is brought to you for free and open access by the Digitized Books at DigitalCommons@UNO. It has been accepted for inclusion in Books in English by an authorized administrator of DigitalCommons@UNO. For more information, please contact [email protected]. Tate, G,P. The kfn&ean sf Af&mistan, DATE DUE I Mil 7 (7'8 DEDICATED, BY PERMISSION, HIS EXCELLENCY BARON HARDINGE OF PENSHURST. VICEROY AND GOVERNOR-GENERAL OF INDIA, .a- . (/. BY m HIS OBEDIENT, SERVANT THE AUTHOR. il.IEmtev 01 the Asiniic Society, Be?zg-nl, S?~rueyof I~din. dafhor of 'I Seisinqz : A Menzoir on the FJisio~y,Topo~rcrphj~, A7zliquiiies, (112d Peo$Ie of the Cozi?zt~y''; The F/.o?zlic7,.~ of Baluchisia'nn : Travels on ihe Border.? of Pe~szk n?zd Akhnnistnn " ; " ICalnf : A lMe??zoir on t7ze Cozl7~try and Fnrrzily of the Ahntadsai Khn7zs of Iinlnt" ; 4 ec. \ViTkI AN INrPR<dl>kJCTOl2Y NO'FE PRINTED BY BENNETT COLEMAN & Co., Xc. PUBLISHED AT THE " TIMES OF INDIA" OFFTCES, BOMBAY & C.1LCUTT-4, LONDON AGENCY : gg, SI-IOE LANE, E.C. -
Arabian Sea and the Gulf of Oman by Global Ocean Associates Prepared for Office of Naval Research – Code 322 PO
An Atlas of Oceanic Internal Solitary Waves (February 2004) Arabian Sea and the Gulf of Oman by Global Ocean Associates Prepared for Office of Naval Research – Code 322 PO Arabian Sea and the Gulf of Oman Overview The Arabian Sea is located in the northwest Indian Ocean. It is bounded by India (to the east), Iran (to the north) and the Arabian Peninsula (in the west)(Figure 1). The Gulf of Oman is located in the northwest corner of the Arabian Sea. The continental shelf in the region is widest off the northwest coast of India, which also experiences wind-induced upwelling. [LME, 2004]. The circulation in the Arabian Sea is affected by the Northeast (March-April) and Southwest (September -October) Monsoon seasons [Tomczak et al. 2003]. Figure 1. Bathymetry of Arabian Sea [Smith and Sandwell, 1997]. 501 An Atlas of Oceanic Internal Solitary Waves (February 2004) Arabian Sea and the Gulf of Oman by Global Ocean Associates Prepared for Office of Naval Research – Code 322 PO Observations There has been some scientific study of internal waves in the Arabian Sea and Gulf of Oman through the use of satellite imagery [Zheng et al., 1998; Small and Martin, 2002]. The imagery shows evidence of fine scale internal wave signatures along the continental shelf around the entire region. Table 1 shows the months of the year when internal wave observations have been made. Table 1 - Months when internal waves have been observed in the Arabian Sea and Gulf of Oman (Numbers indicate unique dates in that month when waves have been noted) Jan Feb Mar Apr May Jun Jul Aug Sept Oct Nov Dec 2 552 1251 Small and Martin [2002] reported on internal wave signatures observed in ERS SAR images of the Gulf of Oman. -
It Is Well Known That the Upwelling Along the West Coast of India Is
Results (modifications) It is well known that the upwelling along the west coast of India is influenced by local winds as well as remotely forcing (Yu et al., 1991; McCreary et al., 1993; Shankar and Shetye, 1997; Shankar et al., 2002). A modelling study by Suresh et al. (2016) has shown that winds near Sri Lanka drive 60% of seasonal sea level of Indian west coast where as the contribution from Bay of Bengal wind forcing is only 20%. They also pointed out that sea level signals forced by the winds near Sri Lanka extend westward into the eastern Arabian Sea with more than 50% contribution in the Lakshadweep high/low region. Negative seasonal sea level anomaly and associated thermocline shoaling in the southeastern Arabian Sea (Lakshdweep low region) during the summer monsoon brings nutrients near the surface causes phytoplankton bloom, and thus influences the food chain with a direct impact on the local fisheries (Madhupratap et al., 2001). A recent study by Suresh et al. (2018) showed that during positive IOD events downwelling Kelvin waves induce a positive sea level anomaly and a deep thermocline along the west coast of India very quickly (within days) during fall. Also, the equatorial easterlies force upwelling Kelvin waves that travel through the Bay of Bengal coastal waveguide to the west coast of India very slowly finally resulting in negative sea level anomaly in winter. The sea level anomaly along the west coast thus shifts from positive in fall to negative in winter during positive IOD events. Our results have shown that chlorophyll concentration is low along the south west coast of India during positive IOD years when compared to neutral and negative IOD years (Fig. -
Northern Arabian Sea Circulation-Autonomous Research (Nascar): a Research Initiative Based on Autonomous Sensors
OceTHE OFFICIALa MAGAZINEn ogOF THE OCEANOGRAPHYra SOCIETYphy CITATION Centurioni, L.R., V. Hormann, L.D. Talley, I. Arzeno, L. Beal, M. Caruso, P. Conry, R. Echols, H.J.S. Fernando, S.N. Giddings, A. Gordon, H. Graber, R.R. Harcourt, S.R. Jayne, T.G. Jensen, C.M. Lee, P.F.J. Lermusiaux, P. L’Hegaret, A.J. Lucas, A. Mahadevan, J.L. McClean, G. Pawlak, L. Rainville, S.C. Riser, H. Seo, A.Y. Shcherbina, E. Skyllingstad, J. Sprintall, B. Subrahmanyam, E. Terrill, R.E. Todd, C. Trott, H.N. Ulloa, and H. Wang. 2017. Northern Arabian Sea Circulation-Autonomous Research (NASCar): A research initiative based on autonomous sensors. Oceanography 30(2):74–87, https://doi.org/10.5670/oceanog.2017.224. DOI https://doi.org/10.5670/oceanog.2017.224 COPYRIGHT This article has been published in Oceanography, Volume 30, Number 2, a quarterly journal of The Oceanography Society. Copyright 2017 by The Oceanography Society. All rights reserved. USAGE Permission is granted to copy this article for use in teaching and research. Republication, systematic reproduction, or collective redistribution of any portion of this article by photocopy machine, reposting, or other means is permitted only with the approval of The Oceanography Society. Send all correspondence to: [email protected] or The Oceanography Society, PO Box 1931, Rockville, MD 20849-1931, USA. DOWNLOADED FROM HTTP://TOS.ORG/OCEANOGRAPHY SPECIAL ISSUE ON AUTONOMOUS AND LAGRANGIAN PLATFORMS AND SENSORS (ALPS) Northern Arabian Sea Circulation- Autonomous Research (NASCar) A RESEARCH INITIATIVE BASED ON AUTONOMOUS SENSORS By Luca R. Centurioni, Verena Hormann, Lynne D. -
South Carolina Landform Regions (And Facts About Landforms) Earth Where Is South Carolina? North America United States of America SC
SCSouth Carolina Landform Regions (and facts about Landforms) Earth Where is South Carolina? North America United States of America SC Here we are! South Carolina borders the Atlantic Ocean. SC South Carolina Landform Regions Map Our state is divided into regions, starting at the mountains and going down to the coast. Can you name these? Blue Ridge Mountains Landform Regions SC The Blue Ridge Mountain Region is only 2% of the South Carolina land mass. Facts About the Blue Ridge Mountains . ◼ It is the smallest of the landform regions ◼ It includes the state’s highest point: Sassafras Mountain. ◼ The Blue Ridge Mountains are part of the Appalachian Mountain Range Facts About the Blue Ridge Mountains . ◼ The Blue Ridge Region is mountainous and has many hardwood forests, streams, and waterfalls. ◼ Many rivers flow out of the Blue Ridge. Blue Ridge Mountains, SC Greenville Spartanburg Union Greenwood Rock Hill Abbeville Piedmont Landform Regions SC If you could see the Piedmont Region from space and without the foliage, you would notice it is sort of a huge plateau. Facts About the Piedmont Region . ◼ The Piedmont is the largest region of South Carolina. ◼ The Piedmont is often called The Upstate. Facts About the Piedmont Region . ◼ It is the foothills of the mountains and includes rolling hills and many valleys. ◼ Piedmont means “foot of the mountains” ◼ Waterfalls and swift flowing rivers provided the water power for early mills and the textile industry. Facts About the Piedmont Region . ◼ The monadnocks are located in the Piedmont. ◼ Monadnocks – an isolated or single hill made of very hard rock. -
Arabian Peninsula from Wikipedia, the Free Encyclopedia Jump to Navigationjump to Search "Arabia" and "Arabian" Redirect Here
Arabian Peninsula From Wikipedia, the free encyclopedia Jump to navigationJump to search "Arabia" and "Arabian" redirect here. For other uses, see Arabia (disambiguation) and Arabian (disambiguation). Arabian Peninsula Area 3.2 million km2 (1.25 million mi²) Population 77,983,936 Demonym Arabian Countries Saudi Arabia Yemen Oman United Arab Emirates Kuwait Qatar Bahrain -shibhu l-jazīrati l ِش ْبهُ ا ْل َج ِزي َرةِ ا ْلعَ َربِيَّة :The Arabian Peninsula, or simply Arabia[1] (/əˈreɪbiə/; Arabic jazīratu l-ʿarab, 'Island of the Arabs'),[2] is َج ِزي َرةُ ا ْلعَ َرب ʿarabiyyah, 'Arabian peninsula' or a peninsula of Western Asia situated northeast of Africa on the Arabian plate. From a geographical perspective, it is considered a subcontinent of Asia.[3] It is the largest peninsula in the world, at 3,237,500 km2 (1,250,000 sq mi).[4][5][6][7][8] The peninsula consists of the countries Yemen, Oman, Qatar, Bahrain, Kuwait, Saudi Arabia and the United Arab Emirates.[9] The peninsula formed as a result of the rifting of the Red Sea between 56 and 23 million years ago, and is bordered by the Red Sea to the west and southwest, the Persian Gulf to the northeast, the Levant to the north and the Indian Ocean to the southeast. The peninsula plays a critical geopolitical role in the Arab world due to its vast reserves of oil and natural gas. The most populous cities on the Arabian Peninsula are Riyadh, Dubai, Jeddah, Abu Dhabi, Doha, Kuwait City, Sanaʽa, and Mecca. Before the modern era, it was divided into four distinct regions: Red Sea Coast (Tihamah), Central Plateau (Al-Yamama), Indian Ocean Coast (Hadhramaut) and Persian Gulf Coast (Al-Bahrain).