ADM ISSUE 13 Single Pages
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Coastal Circulation and Water-Column Properties in The
Coastal Circulation and Water-Column Properties in the War in the Pacific National Historical Park, Guam— Measurements and Modeling of Waves, Currents, Temperature, Salinity, and Turbidity, April–August 2012 Open-File Report 2014–1130 U.S. Department of the Interior U.S. Geological Survey FRONT COVER: Left: Photograph showing the impact of intentionally set wildfires on the land surface of War in the Pacific National Historical Park. Right: Underwater photograph of some of the healthy coral reefs in War in the Pacific National Historical Park. Coastal Circulation and Water-Column Properties in the War in the Pacific National Historical Park, Guam— Measurements and Modeling of Waves, Currents, Temperature, Salinity, and Turbidity, April–August 2012 By Curt D. Storlazzi, Olivia M. Cheriton, Jamie M.R. Lescinski, and Joshua B. Logan Open-File Report 2014–1130 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette M. Kimball, Acting Director U.S. Geological Survey, Reston, Virginia: 2014 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Suggested citation: Storlazzi, C.D., Cheriton, O.M., Lescinski, J.M.R., and Logan, J.B., 2014, Coastal circulation and water-column properties in the War in the Pacific National Historical Park, Guam—Measurements and modeling of waves, currents, temperature, salinity, and turbidity, April–August 2012: U.S. -
Download Transcript
SCIENTIFIC AMERICAN FRONTIERS PROGRAM #1503 "Going Deep" AIRDATE: February 2, 2005 ALAN ALDA Hello and welcome to Scientific American Frontiers. I'm Alan Alda. It's said that the oceans, which cover more than two thirds of the earth's surface, are less familiar to us than the surface of the moon. If you consider the volume of the oceans, it's actually more than ninety percent of the habitable part of the earth that we don't know too much about. The main reason for our relative ignorance is simply that the deep ocean is an absolutely forbidding environment. It's pitch dark, extremely cold and with pressures that are like having a 3,000-foot column of lead pressing down on every square inch -- which does sound pretty uncomfortable. In this program we're going to see how people finally made it to the ocean floor, and we'll find out about the scientific revolutions they brought back with them. We're going to go diving in the Alvin, the little submarine that did so much of the work. And we're going to glimpse the future, as Alvin's successor takes shape in a small seaside town on Cape Cod. That's coming up in tonight's episode, Going Deep. INTO THE DEEP ALAN ALDA (NARRATION) Woods Hole, Massachusetts. It's one of the picturesque seaside towns that draw the tourists to Cape Cod each year. But few seaside towns have what Woods Hole has. For 70 years it's been home to the Woods Hole Oceanographic Institution — an organization that does nothing but study the world's oceans. -
Excavations at Dzibilchaltun, Yucatan, Mexico
Linga-Bibliothek Linga B/951497 National Geographic Society-Tulane University Program of Research on the Yucatan Peninsula Excavations at Dzibilchaltun, Yucatan, Mexico E. WyllysjiAndrews IV and E. Wyllys Andrews V With an appendix on Vertebrate Faunal Remains by Elizabeth S. Wing and David Steadman Publication 48 Middle American Research Institute Tulane University New Orleans 1980 Contents List of Illustrations Structure 605 (Formative period) 25 List of Tables xvi Period 1 (Nabanche 1) 26 Preface xvii Phase A 26 Acknowledgments xix Phase B, subphase a 27 1. Introduction 1 Phase B, subphase b 27 The Natural Setting 1 Phase C 27 The Problem of Environmental Change 3 Phase D 27 Middle American Research Institute Archaeological Period 2 (Nabanche 2) 28 Investigations on the Yucatan Peninsula, Phase A 28 1955-77 4 Phase B 28 The National Geographic Society—Tulane Phase C 29 University Program of Research at Phase D, subphase a 30 Dzibilchaltun 4 Phase D, subphase b 30 Early Investigations 4 Phase E 30 The 1956-57 Season 5 Phase F 31 The 1957—58 Season 6 Phase G 31 The 1958—59 Season 6 Period 3 (Nabanche 2 and Komcl 31 The 1959—60 Season 7 Phase A 31 The 1960—61 Season 7 Phase B, subphase a 34 The 1961—62 Season 8 Phase B, subphase b 34 The 1962-63 Season 8 Phase B, subphase c 34 The 1963—64 Season 9 Phase B, subphase d 35 The 1964-65 and 1965--66 Seasons 9 Phase B, subphase e 35 Research in 1967 and 1968 9 Phase B, subphase f 35 The National Geographic Society—Tulane Phase B, subphase g 35 University Program of Research in Campeche, Phase -
Karst Features — Where and What Are They?
Karst Features — Where and What are They? This story was made with Esri's Story Map Journal. Read the interactive version on the web at https://arcg.is/jCmza. Iowa Geological and Water Survey Bureau completed a detailed mapping project of bedrock geologic units, key subsurface horizons, and surficial karst features in the Iowa portion of the Upper Iowa River Watershed in 2011. In the report, they note that “One of the primary goals of the study was to gain more thorough understanding of relationships between bedrock geology and karst features within the watershed.” Black River Falls photo courtesy of Larry Reis. Sinkholes Esri, HERE, Garmin, FAO, USGS, NGA, EPA, NPS According to the GIS data from the Iowa DNR, the UIR Watershed has 6,649 known sinkholes in the Iowa portion of the watershed. Although this number is very precise, sinkhole development is actually an active process in the UIR Watershed so the actual number of sinkholes changes over time as some are filled in through natural or human processes and others are formed. One of the most numerous karst features found in the UIR Watershed, sinkholes are formed when specific types of underlying bedrock are gradually dissolved, creating voids in the subsurface. When soils and other materials above these voids can no longer bridge the gap created in the bedrock, a collapse occurs. Photo Courtesy of USGS Sinkholes vary in size and shape and can and do occur in any type of land use in the UIR Watershed, from row crop to forest, and even in roads. According to the Iowa Geologic Survey, sinkholes are often connected to underground bedrock fractures and conduits, from minor fissures to enlarged caverns, which allow for rapid movement of water from sinkholes vertically and laterally through the subsurface. -
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. -
Underwater Speleology Journal of the Cave Diving Section of the National Speleological Society
Underwater Speleology Journal of the Cave Diving Section of the National Speleological Society INSIDE THIS ISSUE: Possible Explanations For The Lack Of Formations In Underwater Caves In FLA The Challenge At Challenge Cave Diving Science Visit with A Cave: Cannonball Cow Springs Clean Up Volume 41 Number 1 January/February/March 2014 Underwater Speleology NSS-CDS Volume 41 Number 1 BOARD OF DIRECTORS January/February/March 2014 CHAIRMAN contents Joe Citelli (954) 646-5446 [email protected] Featured Articles VICE CHAIRMAN Tony Flaris (904) 210-4550 Possible Explanations For The Lack Of Formations In Underwater Caves In FLA [email protected] By Dr. Jason Gulley and Dr. Jason Polk............................................................................6 TREASURER The Challenge At Challenge Terri Simpson By Jim Wyatt.................................................................................................................8 (954) 275-9787 [email protected] Cave Diving Science SECRETARY By Peter Buzzacott..........................................................................................................10 TJ Muller Visit With A Cave: Cannonball [email protected] By Doug Rorex.................................................................................................................16 PROGRAM DIRECTORS Book Review: Classic Darksite Diving: Cave Diving Sites of Britain and Europe David Jones By Bill Mixon..............................................................................................................24 -
NIKONOS Speedlighf
Nikon NIKONOS Speedlighf INSTRUCTION MANUAL NOMENCLATURE _______ CD Synchro socket index Joint collar @ Flash head positioning index @ Joint plate ® i ion mark @ i ion mark (@I (J) Sensor socket ® ro socket ® Synchro socket cover Joint @ @ Snp,erllinlht Arm@ ® Camera plug and locking ring Grip @ Sensor holder socket O-rings and lubricant @ @ Sensor holder positioning pin @ Bracket slot @ Bracket screw @Bracket Arm knob @ @ Buckle lock/release latch Battery chamber cap index @ Target -light holder @ @ calculation dial screw ® Exposure calculation dial Exposure calculation dial ® Distance scale scale mode selector ® @ Distance lines T-S switch ®> @ Non-TTL auto shooting aperture scale @ Non-TTL auto shooting aperture index Power switch ® scale 2 CONTENTS _________ NOMENCLATURE . 2 FOREWORD .. ... .. ...... ........ .. ..... 4 PREPARATION .......... ................... 4-6 Examining and lubricating the O-rings ... .. 5 The O-rings and their sealing method .... 6 TIPS ON SPEEDLIGHT CARE. .. 7 BASIC OPERATIONS . .. ..... ............... 8-16 CONTROLS IN DETAIL . ......... .... .. .... 17-30 Bracket ... .. ... .. .... .... ... .. .. ... ... 17 Arm .... .. ... ....... .. .. .. .. .. 17 Joint . ....... .... .. .. ... 18 Close-Up Shooting in the Non-TTL Automatic Mode . .. 18 Synchro Socket . .. 19 Sensor Socket . .. 19 Sensor Unit SU-101 (Optional). ... .. ... ... 20 Synchronization Speed . .. ....... ........ 20 Shooting Mode Selector. .. 21 Exposure Calculation Dial . ... ... .. 22 TTL Automatic Flash Control . .... 22-23 Non-TTL Automatic -
Nikon Report2017
Nikon 100th Anniversary Special Feature A Look Back at Nikon’s 100-Year History of Value Creation Nikon celebrated the 100th anniversary of its founding on July 25, 2017. Nikon has evolved together with light-related technologies over the course of the past century. Driven by our abundant sense of curiosity and inquisitiveness, we have continued to unlock new possibilities that have shined light on the path to a brighter future, creating revolutionary new products along the way. We pride ourselves on the contributions we have made to changing society. Seeking to make our hopes and dreams a reality, the Nikon Group will boldly pursue innovation over the next 100 years, striving to transform the impossible of yesterday into the normal of tomorrow. We will take a look back at Nikon’s 100-year history of value creation. 1917 Three of Japan’s leading optical 1946 Pointal ophthalmic lens manufacturers merge to form is marketed a comprehensive, fully integrated Nikon’s fi rst ophthalmic lens optical company known as Nikon brand name is adopted for Nippon Kogaku K.K. small-sized cameras Pointal Oi Dai-ichi Plant (now Oi Plant) Tilting Level E and Transit G 1918 is completed 1947 surveying instruments are marketed Nikon’s fi rst surveying instruments after World War II MIKRON 4x and 6x 1921 ultra-small-prism binoculars are marketed Nikon Model I small-sized 1948 camera is marketed The fi rst binoculars developed, designed and manufactured The fi rst Nikon camera and the by Nikon fi rst product to bear the MIKRON 6x “Nikon” name Nikon Model I Model -
Where America's Day Begins
Guam Where America’s Day Begins 1 Tumon Bay 2 Two Lovers Point 3 Local boy and mango 4 Where is Paradise? U.S. Territory located • RUSSIA in the Pacific Ocean, Moscow Vladivostok Beijing CHINA KOREA a true tropical island Seoul Osaka JAPAN KOREA Tokyo CHINA JAPAN Shanghai Commonwealth of the TAIWANNorthern Mariana Islands Situated approximately Hong Kong Taipei Saipan HONG KONG • Hanoi TAIWAN GUAM TERRITORY OF THE USA 900 miles north of the Manila PHILIPPINES PHILIPPINES Ho Chi Minh City equator VIETNAM • 32 miles long and ranges between 4 and 8 miles in width • Shaped like a footprint, Guam is the first step into Micronesia 5 Gateway to the Marianas and Micronesia The meaning of Micronesia: • COMMONWEALTH Saipan MICRONESIA OF NORTHERN Tinian MARIANA ISLANDS Rota “micro” – tiny Pacific Ocean Philippine Sea “nesia” – many GUAM TERRITORY OF U.S.A. REPUBLIC FEDERATED STATES REPUBLIC OF Micronesia – “many tiny OF PALAU OF MICRONESIA MARSHALL ISLANDS Pohnpei Kwajalein islands” Palau Yap Chuuk Kosrae Majuro • Largest and most populated island in the Marianas • Communications, transportation and financial hub in the Marianas 6 RUSSIA Getting Moscow Vladivostok Beijing CHINA KOREA Seoul Osaka JAPAN to Guam KOREA Tokyo CHINA JAPAN Shanghai Commonwealth of the TAIWANNorthern Mariana Islands From Hong Kong Taipei HONG KONG Hanoi TAIWAN GUAM TERRITORY OF THE USA Manila PHILIPPINES Vietnam PHILIPPINES Ho Chi Minh City VIETNAM Flight Time Hanoi to Guam via Korea 9 hrs via Taiwan 6 hrs 40 min via Tokyo 8 hrs 50 min Ho Chi Minh City via Hong Kong 10 hrs to Guam via Taiwan 7 hrs 15 min via Manila 6 hrs 30 min 7 Climate & Geography • Average 85ºF (29ºC) • Guam is on the edge of the Mariana Trench, the deepest trench in the world • Craggy limestone cliffs dominate in the North and rolling hills with spectacular views in the South 8 The People • 160,000 Residents • Population is 37% Chamorro, 26% Filipino and 11% other Pacific Islanders. -
Appendix 4-K Preliminary Assessment of Open Pit Slope Instability Due to the Mitchell Block Cave
APPENDIX 4-K PRELIMINARY ASSESSMENT OF OPEN PIT SLOPE INSTABILITY DUE TO THE MITCHELL BLOCK CAVE TM SEABRIDGE GOLD INC. KSM PRELIMINARY FEASIBILITY STUDY UPDATE PRELIMINARY ASSESSMENT OF OPEN PIT SLOPE INSTABILITY DUE TO THE MITCHELL BLOCK CAVE FINAL PROJECT NO: 0638-013-31 DISTRIBUTION: DATE: December 24, 2012 SEABRIDGE: 2 copies DOCUMENT NO: KSM12-26 BGC: 2 copies R.2.7.6 #500-1045 Howe Street Vancouver, B.C. Canada V6Z 2A9 Tel: 604.684.5900 Fax: 604.684.5909 December 24, 2012 Project No: 0638-013-31 Mr. T. Jim Smolik, Pre-Feasibility Study Manager Seabridge Gold Inc. 108 Front Street East Toronto, Ontario, M5A 1E1 Dear Mr. Smolik, Re: Preliminary Assessment of Open Pit Slope Instability due to the Mitchell Block Cave – FINAL Please find attached the above referenced report. Thank you for the opportunity to work on this interesting project. Should you have any questions or comments, please do not hesitate to contact the undersigned. Yours sincerely, BGC ENGINEERING INC. per: Derek Kinakin, M.Sc., P.Geo. (BC) Senior Engineering Geologist Seabridge Gold Inc., KSM Preliminary Feasibility Study Update December 24, 2012 Preliminary Assessment of Open Pit Slope Instability due to the Mitchell Block Cave FINAL Project No: 0638-013-31 EXECUTIVE SUMMARY The Mitchell Zone is the largest of the four exploration targets comprising Seabridge Gold Inc.’s KSM Project and is the only zone where a combination of open pit and block caving mining methods is proposed. The open pit will be mined with ultimate north and south wall heights reaching approximately 1,200 m. -
Airborne Microorganisms in Lascaux Cave (France) Pedro M
International Journal of Speleology 43 (3) 295-303 Tampa, FL (USA) September 2014 Available online at scholarcommons.usf.edu/ijs/ & www.ijs.speleo.it International Journal of Speleology Off icial Journal of Union Internationale de Spéléologie Airborne microorganisms in Lascaux Cave (France) Pedro M. Martin-Sanchez1, Valme Jurado1, Estefania Porca1, Fabiola Bastian2, Delphine Lacanette3, Claude Alabouvette2, and Cesareo Saiz-Jimenez1* 1Instituto de Recursos Naturales y Agrobiología de Sevilla, IRNAS-CSIC, Apartado 1052, 41080 Sevilla, Spain 2UMR INRA-Université de Bourgogne, Microbiologie du Sol et de l’Environnement, BP 86510, 21065 Dijon Cedex, France 3Université de Bordeaux, I2M, UMR 5295, 16 Avenue Pey-Berland, 33600 Pessac, France Abstract: Lascaux Cave in France contains valuable Palaeolithic paintings. The importance of the paintings, one of the finest examples of European rock art paintings, was recognized shortly after their discovery in 1940. In the 60’s of the past century the cave received a huge number of visitors and suffered a microbial crisis due to the impact of massive tourism and the previous adaptation works carried out to facilitate visits. In 1963, the cave was closed due to the damage produced by visitors’ breath, lighting and algal growth on the paintings. In 2001, an outbreak of the fungus Fusarium solani covered the walls and sediments. Later, black stains, produced by the growth of the fungus Ochroconis lascauxensis, appeared on the walls. In 2006, the extensive black stains constituted the third major microbial crisis. In an attempt to know the dispersion of microorganisms inside the cave, aerobiological and microclimate studies were carried out in two different seasons, when a climate system for preventing condensation of water vapor on the walls was active (September 2010) or inactive (February 2010). -
Archons (Commanders) [NOTICE: They Are NOT Anlien Parasites], and Then, in a Mirror Image of the Great Emanations of the Pleroma, Hundreds of Lesser Angels
A R C H O N S HIDDEN RULERS THROUGH THE AGES A R C H O N S HIDDEN RULERS THROUGH THE AGES WATCH THIS IMPORTANT VIDEO UFOs, Aliens, and the Question of Contact MUST-SEE THE OCCULT REASON FOR PSYCHOPATHY Organic Portals: Aliens and Psychopaths KNOWLEDGE THROUGH GNOSIS Boris Mouravieff - GNOSIS IN THE BEGINNING ...1 The Gnostic core belief was a strong dualism: that the world of matter was deadening and inferior to a remote nonphysical home, to which an interior divine spark in most humans aspired to return after death. This led them to an absorption with the Jewish creation myths in Genesis, which they obsessively reinterpreted to formulate allegorical explanations of how humans ended up trapped in the world of matter. The basic Gnostic story, which varied in details from teacher to teacher, was this: In the beginning there was an unknowable, immaterial, and invisible God, sometimes called the Father of All and sometimes by other names. “He” was neither male nor female, and was composed of an implicitly finite amount of a living nonphysical substance. Surrounding this God was a great empty region called the Pleroma (the fullness). Beyond the Pleroma lay empty space. The God acted to fill the Pleroma through a series of emanations, a squeezing off of small portions of his/its nonphysical energetic divine material. In most accounts there are thirty emanations in fifteen complementary pairs, each getting slightly less of the divine material and therefore being slightly weaker. The emanations are called Aeons (eternities) and are mostly named personifications in Greek of abstract ideas.