MNP Rapport 500102001 Scientific Assessment of Solar Induced
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Geologic Map of the Long Valley Caldera, Mono-Inyo Craters
DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP 1-1933 US. GEOLOGICAL SURVEY GEOLOGIC MAP OF LONG VALLEY CALDERA, MONO-INYO CRATERS VOLCANIC CHAIN, AND VICINITY, EASTERN CALIFORNIA By Roy A. Bailey GEOLOGIC SETTING VOLCANISM Long Valley caldera and the Mono-Inyo Craters Long Valley caldera volcanic chain compose a late Tertiary to Quaternary Volcanism in the Long Valley area (Bailey and others, volcanic complex on the west edge of the Basin and 1976; Bailey, 1982b) began about 3.6 Ma with Range Province at the base of the Sierra Nevada frontal widespread eruption of trachybasaltic-trachyandesitic fault escarpment. The caldera, an east-west-elongate, lavas on a moderately well dissected upland surface oval depression 17 by 32 km, is located just northwest (Huber, 1981).Erosional remnants of these mafic lavas of the northern end of the Owens Valley rift and forms are scattered over a 4,000-km2 area extending from the a reentrant or offset in the Sierran escarpment, Adobe Hills (5-10 km notheast of the map area), commonly referred to as the "Mammoth embayment.'? around the periphery of Long Valley caldera, and The Mono-Inyo Craters volcanic chain forms a north- southwestward into the High Sierra. Although these trending zone of volcanic vents extending 45 km from lavas never formed a continuous cover over this region, the west moat of the caldera to Mono Lake. The their wide distribution suggests an extensive mantle prevolcanic basement in the area is mainly Mesozoic source for these initial mafic eruptions. Between 3.0 granitic rock of the Sierra Nevada batholith and and 2.5 Ma quartz-latite domes and flows erupted near Paleozoic metasedimentary and Mesozoic metavolcanic the north and northwest rims of the present caldera, at rocks of the Mount Morrisen, Gull Lake, and Ritter and near Bald Mountain and on San Joaquin Ridge Range roof pendants (map A). -
NSF Current Newsletter Highlights Research and Education Efforts Supported by the National Science Foundation
March 2012 Each month, the NSF Current newsletter highlights research and education efforts supported by the National Science Foundation. If you would like to automatically receive notifications by e-mail or RSS when future editions of NSF Current are available, please use the links below: Subscribe to NSF Current by e-mail | What is RSS? | Print this page | Return to NSF Current Archive Robotic Surgery Systems Shipped to Medical Research Centers A set of seven identical advanced robotic-surgery systems produced with NSF support were shipped last month to major U.S. medical research laboratories, creating a network of systems using a common platform. The network is designed to make it easy for researchers to share software, replicate experiments and collaborate in other ways. Robotic surgery has the potential to enable new surgical procedures that are less invasive than existing techniques. The developers of the Raven II system made the decision to share it as the best way to move the field forward--though it meant giving competing laboratories tools that had taken them years to develop. "We decided to follow an open-source model, because if all of these labs have a common research platform for doing robotic surgery, the whole field will be able to advance more quickly," said Jacob Rosen, Students with components associate professor of computer engineering at the University of of the Raven II surgical California-Santa Cruz. Rosen and Blake Hannaford, director of the robotics systems. Credit: University of Washington Biorobotics Laboratory, led the team that Carolyn Lagattuta built the Raven system, initially with a U.S. -
Natural & Unnatural Disasters
Lesson 20: Disasters February 22, 2006 ENVIR 202: Lesson No. 20 Natural & Unnatural Disasters February 22, 2006 Gail Sandlin University of Washington Program on the Environment ENVIR 202: Lesson 20 1 Natural Disaster A natural disaster is the consequence or effect of a natural phenomenon becoming enmeshed with human activities. “Disasters occur when hazards meet vulnerability” So is it Mother Nature or Human Nature? ENVIR 202: Lesson 20 2 Natural Phenomena Tornadoes Drought Floods Hurricanes Tsunami Wild Fires Volcanoes Landslides Avalanche Earthquakes ENVIR 202: Lesson 20 3 ENVIR 202: Population & Health 1 Lesson 20: Disasters February 22, 2006 Naturals Hazards Why do Populations Live near Natural Hazards? High voluntary individual risk Low involuntary societal risk Element of probability Benefits outweigh risk Economical Social & cultural Few alternatives Concept of resilience; operationalized through policies or systems ENVIR 202: Lesson 20 4 Tornado Alley http://www.spc.noaa.gov/climo/torn/2005deadlytorn.html ENVIR 202: Lesson 20 5 Oklahoma City, May 1999 319 mph (near F6) 44 died, 795 injured 3,000 homes and 150 businesses destroyed ENVIR 202: Lesson 20 6 ENVIR 202: Population & Health 2 Lesson 20: Disasters February 22, 2006 World’s Deadliest Tornado April 26, 1989 1300 died 12,000 injured 80,000 homeless Two towns leveled Where? ENVIR 202: Lesson 20 7 Bangladesh ENVIR 202: Lesson 20 8 Hurricanes, Typhoons & Cyclones winds over 74 mph regional location 500,000 Bhola cyclone, 1970, Bangladesh 229,000 Typhoon Nina, 1975, China 138,000 Bangladesh cyclone, 1991 ENVIR 202: Lesson 20 9 ENVIR 202: Population & Health 3 Lesson 20: Disasters February 22, 2006 U.S. -
Yosemite, Lake Tahoe & the Eastern Sierra
Emerald Bay, Lake Tahoe PCC EXTENSION YOSEMITE, LAKE TAHOE & THE EASTERN SIERRA FEATURING THE ALABAMA HILLS - MAMMOTH LAKES - MONO LAKE - TIOGA PASS - TUOLUMNE MEADOWS - YOSEMITE VALLEY AUGUST 8-12, 2021 ~ 5 DAY TOUR TOUR HIGHLIGHTS w Travel the length of geologic-rich Highway 395 in the shadow of the Sierra Nevada with sightseeing to include the Alabama Hills, the June Lake Loop, and the Museum of Lone Pine Film History w Visit the Mono Lake Visitors Center and Alabama Hills Mono Lake enjoy an included picnic and time to admire the tufa towers on the shores of Mono Lake w Stay two nights in South Lake Tahoe in an upscale, all- suites hotel within walking distance of the casino hotels, with sightseeing to include a driving tour around the north side of Lake Tahoe and a narrated lunch cruise on Lake Tahoe to the spectacular Emerald Bay w Travel over Tioga Pass and into Yosemite Yosemite Valley Tuolumne Meadows National Park with sightseeing to include Tuolumne Meadows, Tenaya Lake, Olmstead ITINERARY Point and sights in the Yosemite Valley including El Capitan, Half Dome and Embark on a unique adventure to discover the majesty of the Sierra Nevada. Born of fire and ice, the Yosemite Village granite peaks, valleys and lakes of the High Sierra have been sculpted by glaciers, wind and weather into some of nature’s most glorious works. From the eroded rocks of the Alabama Hills, to the glacier-formed w Enjoy an overnight stay at a Yosemite-area June Lake Loop, to the incredible beauty of Lake Tahoe and Yosemite National Park, this tour features lodge with a private balcony overlooking the Mother Nature at her best. -
Consequences of Drying Lake Systems Around the World
Consequences of Drying Lake Systems around the World Prepared for: State of Utah Great Salt Lake Advisory Council Prepared by: AECOM February 15, 2019 Consequences of Drying Lake Systems around the World Table of Contents EXECUTIVE SUMMARY ..................................................................... 5 I. INTRODUCTION ...................................................................... 13 II. CONTEXT ................................................................................. 13 III. APPROACH ............................................................................. 16 IV. CASE STUDIES OF DRYING LAKE SYSTEMS ...................... 17 1. LAKE URMIA ..................................................................................................... 17 a) Overview of Lake Characteristics .................................................................... 18 b) Economic Consequences ............................................................................... 19 c) Social Consequences ..................................................................................... 20 d) Environmental Consequences ........................................................................ 21 e) Relevance to Great Salt Lake ......................................................................... 21 2. ARAL SEA ........................................................................................................ 22 a) Overview of Lake Characteristics .................................................................... 22 b) Economic -
An Archaeological Inventory of Alamance County, North Carolina
AN ARCHAEOLOGICAL INVENTORY OF ALAMANCE COUNTY, NORTH CAROLINA Alamance County Historic Properties Commission August, 2019 AN ARCHAEOLOGICAL INVENTORY OF ALAMANCE COUNTY, NORTH CAROLINA A SPECIAL PROJECT OF THE ALAMANCE COUNTY HISTORIC PROPERTIES COMMISSION August 5, 2019 This inventory is an update of the Alamance County Archaeological Survey Project, published by the Research Laboratories of Anthropology, UNC-Chapel Hill in 1986 (McManus and Long 1986). The survey project collected information on 65 archaeological sites. A total of 177 archaeological sites had been recorded prior to the 1986 project making a total of 242 sites on file at the end of the survey work. Since that time, other archaeological sites have been added to the North Carolina site files at the Office of State Archaeology, Department of Natural and Cultural Resources in Raleigh. The updated inventory presented here includes 410 sites across the county and serves to make the information current. Most of the information in this document is from the original survey and site forms on file at the Office of State Archaeology and may not reflect the current conditions of some of the sites. This updated inventory was undertaken as a Special Project by members of the Alamance County Historic Properties Commission (HPC) and published in-house by the Alamance County Planning Department. The goals of this project are three-fold and include: 1) to make the archaeological and cultural heritage of the county more accessible to its citizens; 2) to serve as a planning tool for the Alamance County Planning Department and provide aid in preservation and conservation efforts by the county planners; and 3) to serve as a research tool for scholars studying the prehistory and history of Alamance County. -
A Guide to Space Law Terms: Spi, Gwu, & Swf
A GUIDE TO SPACE LAW TERMS: SPI, GWU, & SWF A Guide to Space Law Terms Space Policy Institute (SPI), George Washington University and Secure World Foundation (SWF) Editor: Professor Henry R. Hertzfeld, Esq. Research: Liana X. Yung, Esq. Daniel V. Osborne, Esq. December 2012 Page i I. INTRODUCTION This document is a step to developing an accurate and usable guide to space law words, terms, and phrases. The project developed from misunderstandings and difficulties that graduate students in our classes encountered listening to lectures and reading technical articles on topics related to space law. The difficulties are compounded when students are not native English speakers. Because there is no standard definition for many of the terms and because some terms are used in many different ways, we have created seven categories of definitions. They are: I. A simple definition written in easy to understand English II. Definitions found in treaties, statutes, and formal regulations III. Definitions from legal dictionaries IV. Definitions from standard English dictionaries V. Definitions found in government publications (mostly technical glossaries and dictionaries) VI. Definitions found in journal articles, books, and other unofficial sources VII. Definitions that may have different interpretations in languages other than English The source of each definition that is used is provided so that the reader can understand the context in which it is used. The Simple Definitions are meant to capture the essence of how the term is used in space law. Where possible we have used a definition from one of our sources for this purpose. When we found no concise definition, we have drafted the definition based on the more complex definitions from other sources. -
UN Specialized Agencies and Governance for Global Risks
13 UN Specialized Agencies and Governance for Global Risks For the first time in human history, we have reached a level of scientific knowledge that allows us to develop an enlightened relationship to risks of catastrophic magnitude. Not only can we foresee many of the challenges ahead, but we are in a position to identify what needs to be done in order to mitigate or even eliminate some of those risks. Our enlightened status, however, also requires that we ... collectively commit to reducing them. 1 Allan Dafoe and Anders Sandberg The United Nations has grown far beyond the institutions directly provided for in the UN Charter. This chapter and those immediately following review a number of global issues and risks that have emerged largely since 1945 and the responses through the UN family of specialized agencies, programs and convention secretar- iats. We consider the efforts of the UN to develop more strategic and integrated approaches to the range of interrelated problems in sustainable development facing the world today. We then consider examples of reform in the economic, environ- mental and social dimensions, without attempting to be comprehensive. We first look at governance for the global economy, especially to address the major chal- lenges of growing inequality and the need for a level playing field for business. For the risks of instability in the financial system, we propose reinforcing the role of the International Monetary Fund (IMF) for enhanced financial governance. We then review global environmental governance, including climate change, as well as population and migration as significant global social issues. -
Relation Between Sunspots and Covid19 – a Proof for Panspermia
International Research Journal of Engineering and Technology (IRJET) e-ISSN: 2395-0056 Volume: 07 Issue: 11 | Nov 2020 www.irjet.net p-ISSN: 2395-0072 RELATION BETWEEN SUNSPOTS AND COVID19 – A PROOF FOR PANSPERMIA Janani T1 1Department of Biotechnology, Kumaraguru College of Technology, Coimbatore, Tamilnadu, India ---------------------------------------------------------------------***---------------------------------------------------------------------- Abstract - The novel viral or the bacterial pandemics and epidemics are not new to this earth. Often these disease-causing pathogens are of unknown origin and often identified as an infection which is transmitted from other animals. They are frequently found as the mutated form of the original strain or completely a newly developed strain. The causes for this mutation are many which comprises of both natural and artificial sources. The time of occurrence of these pandemic and epidemic astonishingly coincides with the sun spot extremum (often minimum). It is observed that whenever there is a sun spot extremum there was a novel microbial pandemic or epidemic. The current COVID19 pandemic is also suggested to be due to such sunspot extremum as the sun cycle is currently at its sun spot minimum. This review aims at providing the facts of relation between sunspots and the novel corona virus pandemic and there by stating this occurrence as a proof for panspermia. Key Words: Pandemic, Epidemic, COVID19, Sunspot, Solar Cycle, Solar minimum, Panspermia 1. INTRODUCTION 1.1 SUNSPOTS: Sunspots are the dark regions in the sun’s surface due to the concentration of magnetic field in that region. These regions are relatively colder to the other regions of the sun’s surface. Hotter region emits more light than the colder region hence these regions appear to be darker and called the spots of the sun. -
Introducing Terminal Lakes Joe Eilers and Ron Larson
Terminal Lakes Introducing Terminal Lakes Joe Eilers and Ron Larson Study Lakes akes tend to be among the more ephemeral features of the landscape Land generally are formed and disappear rapidly on a geological time frame. However, to see groups of lakes disappear within a lifetime is typically not a natural phenomenon. Here in Oregon, we’ve witnessed the desiccation of what was formerly a 16-mile-long lake in a little over a decade. Endorehic lakes, commonly referred to as terminal lakes because they lack an outlet, are among the most vulnerable of lakes to human intervention. Because terminal lakes are usually located in arid environments where water is extremely valuable, they are the first to lose among the competing forces for water. But that doesn’t have to be the case. In some respects, terminal lakes are far easier to restore than eutrophic/hypereutrophic systems. No expensive alum treatments, no dredging, no chemicals . just add water and life returns: but as those in West know, “Whiskey is for drinking; water is for fighting over.” And fight we must. In this issue of LakeLine, we describe a series of terminal lakes in the western United States starting with the least saline lake among the group, Walker Lake, and ending with Lake Winnemucca, which was desiccated in the 20th century (Figure 1). Like all lakes, each of these has a unique story to relate with different Figure 1. Terminal lakes in the western United States described in this issue. chemistry and biota. The loss of Lake Winnemucca is an informative tale, but it a wider audience and reach a solution migration when the birds replenish fat is not necessarily the inevitable outcome that ensures adequate water to save the reserves. -
Oxygen Isotope Evidence for Paleoclimate Change During The
PALEOCLIMATE RECONSTRUCTION IN NORTHWEST SCOTLAND AND SOUTHWEST FLORIDA DURING THE LATE HOLOCENE Ting Wang A dissertation submitted to the faculty of the University of North Carolina at Chapel Hill in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the Department of Geological Sciences. Chapel Hill 2011 Approved by: Dr. Donna M. Surge Dr. Joseph G. Carter Dr. Jose A. Rial Dr. Justin B. Ries Dr. Karen J. Walker © 2011 Ting Wang ALL RIGHTS RESERVED ii ABSTRACT TING WANG: Paleoclimate Reconstruction in Northwest Scotland and Southwest Florida during the Late Holocene (Under the direction of Dr. Donna M. Surge) The study reconstructed seasonal climate change in mid-latitude northwest Scotland during the climate episodes Neoglacial (~3300-2500 BP) and Roman Warm Period (RWP; ~2500-1600 BP) and in subtropical southwest Florida during the latter part of RWP (1-550 AD) based on archaeological shell accumulations in two study areas. In northwest Scotland, seasonal sea surface temperature (SST) during the Neoglacial and RWP was estimated from high-resolution oxygen isotope ratios (δ18O) of radiocarbon-dated limpet (Patella vulgata) shells accumulated in a cave dwelling on the Isle of Mull. The SST results revealed a cooling transition from the Neoglacial to RWP, which is supported by earlier studies of pine pollen in Scotland and European glacial events and also coincident with the abrupt climate deterioration at 2800-2700 BP. The cooling transition might have been driven by decreased solar radiation and weakened North Atlantic Oscillation (NAO) conditions. In southwest Florida, seasonal-scale climate conditions for the latter part of RWP were reconstructed by using high-resolution δ18O of archaeological shells (Mercenaria campechiensis) and otoliths (Ariopsis felis). -
Open-File/Color For
Questions about Lake Manly’s age, extent, and source Michael N. Machette, Ralph E. Klinger, and Jeffrey R. Knott ABSTRACT extent to form more than a shallow n this paper, we grapple with the timing of Lake Manly, an inconstant lake. A search for traces of any ancient lake that inundated Death Valley in the Pleistocene upper lines [shorelines] around the slopes Iepoch. The pluvial lake(s) of Death Valley are known col- leading into Death Valley has failed to lectively as Lake Manly (Hooke, 1999), just as the term Lake reveal evidence that any considerable lake Bonneville is used for the recurring deep-water Pleistocene lake has ever existed there.” (Gale, 1914, p. in northern Utah. As with other closed basins in the western 401, as cited in Hunt and Mabey, 1966, U.S., Death Valley may have been occupied by a shallow to p. A69.) deep lake during marine oxygen-isotope stages II (Tioga glacia- So, almost 20 years after Russell’s inference of tion), IV (Tenaya glaciation), and/or VI (Tahoe glaciation), as a lake in Death Valley, the pot was just start- well as other times earlier in the Quaternary. Geomorphic ing to simmer. C arguments and uranium-series disequilibrium dating of lacus- trine tufas suggest that most prominent high-level features of RECOGNITION AND NAMING OF Lake Manly, such as shorelines, strandlines, spits, bars, and tufa LAKE MANLY H deposits, are related to marine oxygen-isotope stage VI (OIS6, In 1924, Levi Noble—who would go on to 128-180 ka), whereas other geomorphic arguments and limited have a long and distinguished career in Death radiocarbon and luminescence age determinations suggest a Valley—discovered the first evidence for a younger lake phase (OIS 2 or 4).