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Palawan ‘CAN ’ Palawan is 1,780 islands of pristine white beaches, dramatic rock A nature lover ’s paradise and an formations, secret coves and underground mysteries. An untamed CULTURE . The island province of Palawan land, a nature lover’s paradise and an adventurer’s dream: Palawan adventurer ’s dream has much to offer to those who want to get to certainly lives up to its image as the last frontier. LAOAG the heart and soul of the Philippines. The more Getting there adventurous traveller can visit one of Palawan’s The island province has been declared a nature sanctuary of the world Palawan Banaue Major Airport Gateways: indigenous people, the Batak, whose settlements and for good reason. It is wrapped in a mantel of rainforests, outstanding Luzon dive sites, majestic mountains, primeval caves and shimmering beaches. Puerto Princesa, El Nido, Sandoval, Busuanga and PHILIPPINE SEA are on the slope of Cleopatra’s Needle. The Tabon Cuyo. Distance from Manila to Puerto Princesa is and Palawan Museums with their displays of It bursts with exotic flora and fauna and is surrounded by a coral shelf 306 nautical miles MANILAMMAMANMANIMANIL prehistoric artifacts from the Tabon caves and that abounds with varied and colourful marine life. Air Transport: items from the Spanish era bring the areas’ local Mindoro The long narrow strip of the main island, located southwest of Manila, Various domestic carriers fly to Palawan's major history to life and are well worth exploring. gateways from Manila (20+ flights daily), Cebu Busuanga Boracay Samar is around 425 kilometres long and 40 kilometres at its widest. -
Cruising Guide to the Philippines
Cruising Guide to the Philippines For Yachtsmen By Conant M. Webb Draft of 06/16/09 Webb - Cruising Guide to the Phillippines Page 2 INTRODUCTION The Philippines is the second largest archipelago in the world after Indonesia, with around 7,000 islands. Relatively few yachts cruise here, but there seem to be more every year. In most areas it is still rare to run across another yacht. There are pristine coral reefs, turquoise bays and snug anchorages, as well as more metropolitan delights. The Filipino people are very friendly and sometimes embarrassingly hospitable. Their culture is a unique mixture of indigenous, Spanish, Asian and American. Philippine charts are inexpensive and reasonably good. English is widely (although not universally) spoken. The cost of living is very reasonable. This book is intended to meet the particular needs of the cruising yachtsman with a boat in the 10-20 meter range. It supplements (but is not intended to replace) conventional navigational materials, a discussion of which can be found below on page 16. I have tried to make this book accurate, but responsibility for the safety of your vessel and its crew must remain yours alone. CONVENTIONS IN THIS BOOK Coordinates are given for various features to help you find them on a chart, not for uncritical use with GPS. In most cases the position is approximate, and is only given to the nearest whole minute. Where coordinates are expressed more exactly, in decimal minutes or minutes and seconds, the relevant chart is mentioned or WGS 84 is the datum used. See the References section (page 157) for specific details of the chart edition used. -
Rock Stratigraphy of the Silurian System in Northeastern and Northwestern Illinois
2UJ?. *& "1 479 S 14.GS: CIR479 STATE OF ILLINOIS c. 1 DEPARTMENT OF REGISTRATION AND EDUCATION Rock Stratigraphy of the Silurian System in Northeastern and Northwestern Illinois H. B. Willman GEOLOGICAL ILLINOIS ""SURVEY * 10RM* APR 3H986 ILLINOIS STATE GEOLOGICAL SURVEY John C. Frye, Chief Urbano, IL 61801 CIRCULAR 479 1973 CONTENTS Page Abstract 1 Introduction 1 Time-stratigraphic classification 3 Alexandrian Series 5 Niagaran Series 5 Cayugan Series 6 Regional correlations 6 Northeastern Illinois 6 Development of the classification 9 Wilhelmi Formation 12 Schweizer Member 13 Birds Member 13 Elwood Formation 14 Kankakee Formation 15 Drummond Member 17 Offerman Member 17 Troutman Member 18 Plaines Member 18 Joliet Formation 19 Brandon Bridge Member 20 Markgraf Member 21 Romeo Member 22 Sugar Run Formation . „ 22 Racine Formation 24 Northwestern Illinois 26 Development of the classification 29 Mosalem Formation 31 Tete des Morts Formation 33 Blanding Formation 35 Sweeney Formation 36 Marcus Formation 3 7 Racine Formation 39 References 40 GEOLOGIC SECTIONS Northeastern Illinois 45 Northwestern Illinois 52 FIGURES Figure 1 - Distribution of Silurian rocks in Illinois 2 2 - Classification of Silurian rocks in northeastern and northwestern Illinois 4 3 - Correlation of the Silurian formations in Illinois and adjacent states 7 - CM 4 Distribution of Silurian rocks in northeastern Illinois (modified from State Geologic Map) 8 - lis. 5 Silurian strata in northeastern Illinois 10 ^- 6 - Development of the classification of the Silurian System in |§ northeastern Illinois 11 7 - Distribution of Silurian rocks in northwestern Illinois (modified ;0 from State Geologic Map) 2 7 8 - Silurian strata in northwestern Illinois 28 o 9 - Development of the classification of the Silurian System in CO northwestern Illinois 30 10 - Index to stratigraphic units described in the geologic sections • • 46 ROCK STRATIGRAPHY OF THE SILURIAN SYSTEM IN NORTHEASTERN AND NORTHWESTERN ILLINOIS H. -
As Pessoas Interessadas Em Receber Nossa Newsletter Via Mail, Podem Escrever Para [email protected] Pedindo Sua Adesão
***As pessoas interessadas em receber nossa newsletter via mail, podem escrever para [email protected] pedindo sua adesão. LIVROS http://eu.wiley.com/WileyCDA/Section/id-350717.html ÍNDICE DE NOTÍCIAS JORNAL DA CIÊNCIA Edição 4638 - Notícias de C&T - Serviço da SBPC 1. Para SBPC, Brasil precisa de Educação e CT&I para manter seu crescimento econômico 2. Senadora atende pleito da SBPC e ABC e adia votação do PL sobre revalidação de diplomas estrangeiros 3. Congresso tem até 13 de março para votar MP dos royalties 4. Sem bons professores não há futuro, artigo de Mozart Neves Ramos 5. Mercosul terá programa de mobilidade estudantil semelhante ao Ciência sem Fronteitas 6. Contra o conteudismo escolar e seus testes, artigo de Roberto Franklin de Leão 7. Pronatec atende mais de 2,5 milhões de jovens e será ampliado em 2013 8. Cristovam propõe sistema único de educação 9. A segurança alimentar e a desinformação do consumidor, artigo de Flávio Finardi Filho 10. Marco legal precisa amparar interação público-privada, defende ministro 11. Futuro tecnológico da geração elétrica nuclear, artigo de Leonam dos Santos Guimarães 12. Adeus a Oscar Niemeyer 13. Excesso de neurônio é tão ruim como falta, diz pesquisa da UFRJ 14. "Feijão verde": astrônomos descobrem novo tipo de galáxia 15. Homenagem a Renato Archer, com inauguração de Espaço Galeria, lançamento de Livro e selo comemorativo dos 30 anos do CTI Renato Archer 16. Ciência Hoje On-line: Terra partida 17. Campus Sorocaba da UFSCar realiza concurso para professores até 7 de dezembro 18. UFABC abre oportunidade de pós-doutorado em Microbiologia e Biologia Molecular 19. -
Lancaster County Geology
LancasterLancaster CountyCounty GeologyGeology gfgh µ OverOver TopographicTopographic ReliefRelief Om Miles Í897 0 10 hg Lebanon County Adamstown ¦¨§76 ! Berks County Oha ! Oo Denver ab322 Ephrata Csc Í501 ! Í72 TRh 272 TRn Oco Lititz Í ! Akron Elizabethtown Manheim ! Dauphin County! ! TRhc Cr TRs c Os Rn ! T Terre Hill TRg Trd 322 772 ab 10 Í 222 625 Í ab Í897 Í Í283 Ohm Í230 Oan Í241 East New Holland Oe 722 Petersburg Í Cbs ! Mount Joy ! ! Czc Cch Í23 Cm gga fl R 743 T Í Csb gg pg ggd Í441 Ck Cl 772 72 Í 23 Í ! Í Ca Marietta Ch Lancaster Mountville ! 340 ! Í Columbia 30 ! ! ba Í462 Í462 ab30 Í999 Millersville Ccc Strasburg ! ! Cv Í741 Í741 Í272 41 Í County Chester 896 222 Í gn Christiana ba mg ! oct Cah Í372 S u sq u e h a n n a R iv e r Y o rk C o u n ty gqm LEGEND COUNTY BOUNDARIES Í324 Source: Lancaster County GIS, Copyright (c) 2019 MAJOR ROADS This map to be used for reference or illustrative purposes only. This map FAULT is not a legally recorded plan, survey, or engineering schematic Quarryville and it is not intended to be used as such. For complete disclaimer see: RIVERS AND STREAMS ! http://www.co.lancaster.pa.us/gisdisclaimer DIKE wc ORDOVICIAN Í472 Oan, ANNVILLE FORMATION LIMESTONE TRIASSIC 372 Oco, COCALICO FORMATION DARK GRAY SHALE TRfl, LIMESTONE FANGLOMERATE Í TRg, GETTYSBURG FORMATION SHALE-SANDSTONE Oe, EPLER FORMATION LIMESTONE TRh, HAMMER CREEK FORMATION SANDSTONE-SHALE Oha, ANNVILLE, HERSHEY, AND MYERSTOWN FORMATION TRhc, HAMMER CREEK QUARTZ-CONGLOMERATE Ohm, HERSHEY AND MYERSTOWN FORMATION LIMESTONE 272 TRn, NEW -
USNMP-76 2806 1929.Pdf
NEW LOWER AND MIDDLE CAJ^IBRIAN CRUSTACEA By Charles E, Resser Associate Curator of Stratigraphic Paleontology INTRODUCTION Among the numerous Cambrian fossils that have been accumulating in the United States National Museum during the last 15 years, there are many undescribed species and some of the specimens are remarkable for the preservation of thin tests or of soft body parts. In order to stimulate further search for the rarer fossils, and par- ticularly for preservations of the softer parts of animals or of delicate plant tissues, it is planned to publish more or less related groups of these animals from time to time. Accordingly, in this paper I have assembled a group of species that centers mainly around the pre- viously described genus Tuzoia, but which also includes several unre- lated forms that were secured from the same localities as the others. This paper thus adds several new species preserving more than ordinarily thin tests of Crustacea and a few with the still softer fleshy parts. Some are from the well known Burgess shale that has already furnished so many interesting animals and plants, but other formations, some of which have not previously been known to yield such fossils, are also represented. This paper also contains information of interest aside from that naturally attaching to any description of the softer parts of such ancient animals, by presenting certain important stratigraphic facts in addition to further data regarding the geographic distribution and origin of the faunas to which these species belong. Acknowledgment.—In the preparation of this paper I was kindly assisted by Dr. -
Annual Report 2008
godišnje izvješće annual report 2008 Sachsova 2, HR-10000 Zagreb Hrvatska (Croatia) Tel.: (+385 1) 6160-749 Fax.: (+385 1) 6144-718 www.hgi-cgs.hr ISBN 978-953-6907-19-9 ISSN 1846-629X Avanić Radovan +385 1 6160 708 [email protected] Zavod za geologiju Badnjević Edin +385 1 6160 754 Stručne službe Bakrač Koraljka +385 1 6160 706 [email protected] Zavod za geologiju Banović Jarmila +385 1 6160 744 [email protected] Zavod za mineralne sirovine NAKLADNIK – PUBLISHER: Hrvatski geološki institut – Croatian Geological Survey Bastalić Nada +385 1 6160 712 [email protected] Zavod za hidrogeologiju i inženjersku geologiju Belak Mirko +385 1 6160 722 [email protected] Zavod za geologiju Sachsova 2, HR-10000 Zagreb, Hrvatska (Croatia) Bergant Stanislav +385 1 6160 732 [email protected] Zavod za geologiju Brkić Željka +385 1 6160 700 [email protected] Zavod za hidrogeologiju i inženjersku geologiju Buljan Renato +385 1 6160 806 [email protected] Zavod za hidrogeologiju i inženjersku geologiju Colussi Kristijan +385 1 6160 754 Stručne službe ZA NAKLADNIKA – FOR THE PUBLISHER: Crnogaj Stjepan +385 1 6160 751 [email protected] Zavod za mineralne sirovine Ravnatelj (Director) Josip HALAMIĆ Dedić Željko +385 1 6160 746 [email protected] Zavod za mineralne sirovine Devčić Zorka +385 1 6160 742 Stručne službe Dmitrović Aco +385 1 6160 800 [email protected] Stručne službe Dolić Stjepan +385 1 6160 704 [email protected] Zavod za hidrogeologiju i inženjersku geologiju -
Water-Quality Data Collected at Lake Anne, Reston, Virginia, 1997-1999
Water-Quality Data Collected at Lake Anne, Reston, Virginia, 1997-1999 Kathryn M. Conko, Margaret M. Kennedy, and Karen C. Rice U.S. GEOLOGICAL SURVEY Open-File Report 00-481 Reston, Virginia 2000 Contents ABSTRACT ..............................^^ INTRODUCTION.............................................................................................................^ FIELD DATA COLLECTION METHODS.................................................................................... 3 Precipitation................................................................................................................................. 3 Streams and Lake Water.............................................................................................................. 5 LABORATORY ANALYTICAL METHODS................................................................................ 9 Sample Analysis Trace Elements............................................................................................... 9 Precipitation.............................................................................................................................. 9 Streams and Lake Water......................................................................................................... 11 Sample Analysis Major Cations and Anions........................................................................... 12 Quality Assurance...................................................................................................................... 14 Field Collection..................................................................................................................... -
Exhibit 5 Town of Barton Geology and Seismicity Report Sections
GEOLOGY AND SEISMICITY REPORT SNYDER E1-A WELL TOWN OF BARTON TIOGA COUNTY, NEW YORK Prepared for: Couch White, LLP 540 Broadway P.O. Box 22222 Albany, New York 12201 Prepared by: Continental Placer Inc. II Winners Circle Albany, New York 12205 July 25, 2017 Table of Contents 1.0 EXECUTIVE SUMMARY............................................................................................................. 1 2.0 INTRODUCTION ........................................................................................................................... 2 2.1 Depositional Sequences and General Stratigraphic Sequence ................................................ 2 2.1.1 Upper Devonian Lithologies ........................................................................................................ 4 2.1.2 Marcellus-Hamilton ..................................................................................................................... 4 2.1.3 Tristates-Onondaga ...................................................................................................................... 4 2.1.4 Helderberg .................................................................................................................................... 4 2.1.5 Oneida-Clinton-Salina ................................................................................................................. 4 2.1.6 Black River-Trenton-Utica-Frankfort .......................................................................................... 5 2.1.7 Potsdam-Beekmantown .............................................................................................................. -
Geologic Cross Section C–C' Through the Appalachian Basin from Erie
Geologic Cross Section C–C’ Through the Appalachian Basin From Erie County, North-Central Ohio, to the Valley and Ridge Province, Bedford County, South-Central Pennsylvania By Robert T. Ryder, Michael H. Trippi, Christopher S. Swezey, Robert D. Crangle, Jr., Rebecca S. Hope, Elisabeth L. Rowan, and Erika E. Lentz Scientific Investigations Map 3172 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2012 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1–888–ASK–USGS. For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. Suggested citation: Ryder, R.T., Trippi, M.H., Swezey, C.S. Crangle, R.D., Jr., Hope, R.S., Rowan, E.L., and Lentz, E.E., 2012, Geologic cross section C–C’ through the Appalachian basin from Erie County, north-central Ohio, to the Valley and Ridge province, Bedford County, south-central Pennsylvania: U.S. Geological Survey Scientific Investigations Map 3172, 2 sheets, 70-p. -
Get Outside and Thrive
GET OUTSIDE AND THRIVE THE MENTAL HEALTH BENEFITS OF SPENDING TIME OUTSIDE, NATURE AND MOVEMENT WHY DOES GETTING OUTSIDE MATTER? ¡ Researchers at Harvard Medical School have found that time spent in nature can drastically impact mental health ¡ Ecotherapy has shown a strong connection between time spent in nature and reduced stress, anxiety, and depression. ¡ Walking has been proven effective in reducing anxiety and depression, and there is further evidence that walking in nature improves those results even further. That’s because different parts of our brain activate in nature. Our mind calms, leading to physical changes including a reduction in heart rate and blood pressure and a drop is cortisol levels ¡ Nature Walks have been described as the easiest self help strategy available to support mental health. HOW MUCH TIME OUTSIDE IS NEEDED TO MAKE A DIFFERENCE? ¡ 20 minutes 3 times a week is enough to show a consistent reduction in stress as measured by cortisol levels. ¡ Any natural environment should help – the goal is to get away from the high stimulation levels of urban environments ¡ Find a time and space that works for you ¡ Consider making this a (safe) social time with family members or your support pod – evidence suggests the greatest mental health benefits come from group nature walks ¡ Any outdoor activity can help – a gentle walk, brisk hike, bike ride or run all help reduce stress levels ¡ Any green space will have a positive impact if “escape to the country” isn’t an option. WHERE CAN I GET OUTSIDE? ¡ For local walks our Lemon Road neighbourhoods are blessed with options – there are short and long trails along Pimmit Run at the back of the school property, multiple green spaces and parks in Pimmit Hills and behind the library and the High School allows walkers to use the trails around the school property and across the fields. -
Overview of the Strategic and Structural Evolution of the Talladega Slate Belt, Alabama Appalachians
fl d029-08 1st pgs page 1 The Geological Society of America Field Guide 29 2012 Overview of the stratigraphic and structural evolution of the Talladega slate belt, Alabama Appalachians James F. Tull* Department of Earth, Ocean, and Atmospheric Science, Florida State University Clinton I. Barineau* Department of Earth and Space Sciences, Columbus State University ABSTRACT The allochthonous Talladega belt of eastern-northeastern Alabama and north- western Georgia is a northeast striking, fault bounded block of lower greenschist facies metasedimentary and metaigneous rocks that formed along the margin of Lau- rentia at or outboard of the seaward edge of the Alabama promontory. Bounded by metamorphic rocks of the higher grade Neoproterozoic(?) to Carboniferous eastern Blue Ridge on the southeast and unmetamorphosed to anchimetamorphic Paleozoic rocks of the Appalachian foreland on the northwest, the Talladega belt includes shelf facies rocks of the latest Neoproterozoic/earliest Cambrian Kahatchee Mountain Group, Cambrian-Ordovician Sylacauga Marble Group, and the latest Silurian(?) to uppermost Devonian/earliest Mississippian Talladega Group. Along the southeast- ern fl ank of these metasedimentary sequences, a Middle Ordovician back-arc terrane (Hillabee Greenstone) was tectonically emplaced along a cryptic pre-metamorphic thrust fault (Hillabee thrust) and subsequently dismembered with units of the upper Talladega Group along the post-metamorphic Hollins Line fault system. Importantly, strata within the Talladega belt are critical for understanding the tectonic evolution of the southern Appalachian orogen when coupled with the geologic history of adjacent terranes. Rocks of the lower Talladega Group, the Lay Dam Formation, suggest latest Silurian-earliest Devonian tectonism that is only now being recognized in other areas of the southern Appalachians.