Internationale Überstchten 645 1 . 3 Bodenerhebungen(Berge) Berg Höhe') Gebirge Land Bzw.Gebiet Berg Europa Montblanc(Mont B

Total Page:16

File Type:pdf, Size:1020Kb

Internationale Überstchten 645 1 . 3 Bodenerhebungen(Berge) Berg Höhe') Gebirge Land Bzw.Gebiet Berg Europa Montblanc(Mont B Internationale Überstchten 645 1 . 3 Bodenerhebungen(Berge) Berg Höhe’) Gebirge Land bzw.Gebiet Berg Europa Mittelame n ka Montblanc(Mont Blanc) ....4 807 Montblancgruppe Frankreich/Italien Voicän de Tajumulco^) . Dufourspitze(Monte Rosa) . .4 634 Walliser Alpen Schweiz/Italien Cerro Chirripö Grande.... Dom(Mischabel ) .4 545 Walliser Alpen Schweiz Voicän Barü^) . Weißhorn .4 506 Walliser Alpen Schweiz Pico Duarte . Matterhorn .4 478 Walliser Alpen Schweiz/Italien Cerro de Culmi. Finsteraarhorn.4 274 Berner Alpen Schweiz Blue Mountain Peak. Jungfrau. .4 158 Berner Alpen Schweiz Pico Turqumo . Barre des Écrins .4 103 Frankreich Gran Paradiso .4 061 PelvouxgruppeGrajische Alpen Italien Südamerika Piz Bernina .4 049 Berninagruppe Schweiz Cerro Aconcagua. Ortler.3 899 Ortlergruppe Italien Nevado de lllimani. Monte Vise .3 841 Cottische Alpen Italien Nevado Ojos del Salado.... Großglockner .3 797 Hohe Tauern Österreich Cerro Tupungato . Wildspitze .3 774 Ötztaler Alpen Österreich Cerro Mercedario. Großvenediger .3 674 Hohe Tauern Österreich Nevado Huascarän. Dammastock .3 630 Urner Alpen Schweiz Cerro de Tocorpun. Tödi .3 614 Glarner Alpen Schweiz Nevado de Ancohuma. Monte Adamello .3 554 Adameilogruppe Italien Nevado Coropuna. Mulhacén .3 478 Sierra Nevada Spanien Chimborazo^). Pico de Aneto.3 404 Pyrenäen Spanien Cumbre de Mejicana . Monte Perdido .3 355 Pyrenäen Spanien Pico Cnstöbal Colön. Marmolada .3 343 Dolomiten Italien Parseierspitze.3 036 Lechtaler Alpen Österreich Nevado del Huila^) . Hoher Dachstein.2 995 Dachsteingruppe Österreich Pico Bolivar . Zugspitze .2 962 Wettersteingebirge Cerro San Valentin . BundesrepÖsterreich.Deutschi./ Pico da Neblina. Musala.2 925 Rila Bulgarien Corno Grande.2 914 Abruzzen Italien Asien Olymp .2 911 Pieria Ori Griechenland Tschomolungma. Triglav.2 863 [ulische Alpen Jugoslawien (S^armatha.Mount Everestl Titov Vrv.2 747 Sar plania Jugoslawien К 2(Ischogori ,Godwin Austen ) jezercë .2 692 Prokletije Albanien Kantschmdschunga. Gerlachovsky 5tft .2 654 Hohe Tatra Tschechoslowakei Makalu . Almanzor .2 592 Sierra de Gredos Spanien Dhaulagiri . Moldoveanul .2 543 Südkaimaten Rumänien Nanga Parbat. Rysy .2 499 Hohe Tatra Polen Annapurna . Galdhopigg .2 469 Jotunheimen Norwegen Ullug Mustag. Kebnekajse .2 123 Skanden Schweden Hvannadalshnukur^) .2 119 Öraefajökull Island Tiritsch Mir. Estrêla .1 991 Serra da Estrêla Portugal Minyag Gongkar(Gongga Schan) Narodnaja.1 894 Ural Sowjetunion Mustag Ata . Puy de Sancy.1 886 Mont Dore Frankreich Kuiha Gangri . Ben Nevis.1 343 Schottisches Hochland Großbr.u.Nordirl. Pik Kommunisma. Pik Pobedy . Afrika Kibo2) . Gaurisankar. Mawensi^) . Pik Lenma. Mount Kenya(Batian)^) . , Schule Schan. Margherita. Hkakabo Razi . Meru^). Elbrus. Ras Daschen . Demawend^) . Karisimbi . Kuh-e Fuladi . Taio . Großer Ararat^). Mount Elgon^) . Belucha. Batu . Najrambal Uul. Guna. Kuh-e Dinar. Dschebel Tubkal . Kinabalu . Ol Doinyo Lesatima. Otgon Tenger Uul . Dschebel Ayachi . Yu Shan. Pico de Teide^) .. Erciyes dagi(Erdschias) .... Thabana Ntlenyana. Fuji-san(Fudschijama)^) .... 3 776 Japan(Honschu) Injasuti . Hadur Schuaib. 3 760 Jemen Emi Koussi. Gunung Leuser . 3 381 Indonesien(Sumatra) Dschebel Kinyeti . Pobeda. 3 147 Tscherskigebirge Sowjetunion Piton des Neiges^). Fan Si Pan. 3 143 Hoang Lien Son Vietnam Tahat. Jabal Suqah . 3 133 AsTr Saudi-Arabien Sapitwa. Qornet es Saouda . 3 083 Jebel Liban Libanon Maromokotro . Apo^). 2 954 Philippinen(Mindanao) Amerika Australien und Ozeanien Nordamerika Puncak Jaya(Carstenszspitze) 5 029 Maokegebirge Indonesien(Westinan) Mount McKinley.6 1 98 Alaska Range Verein.Staaten(Alaska) Mount Wilhelm . 4 694 Bismarckgebirge Papua-Neuguinea Mount Logan.5 951 Samt Elias Mountains Kanada Mauna Kea^). 4 206 Ver.Staaten(Hawaii) Citlaltepetl (Pik v.Orizaba)^)5 700 Sierra Madre Oriental Mexiko Mount Victoria . 4 073 Owen Stanley Gebirge Papua-Neugumea Mount Samt Elias.5 489 Samt Elias Mountains Alaska/Kanada Mount Cook. 3 764 Neuseeländische Alpen Neuseeland(Südmsel) Voicän PopocatépetP) .5 452 Anähuac Mexiko Mount Earnslaw. 2 823 Neuseeländische Alpen Neuseeland(Südinsel ) Mount Blackburn.4 996 Wrangell Mountains Mount Kosciusko . 2 230 Australische Alpen Australien Mount Whitney.4 421 Sierra Nevada Vf«'"1}(AlaskaKal.forn) .) (Neusüdwales) Mount Elbert .4 402 Rocky Mountains Staaten j(Colorado) Mauga Silisili^). 1 858 Samoa(Savai 'i ) Nevado de Toluca .4 392 Cordillera Volcânica Mexiko Mount Ossa. 1 617 Australien(Tasmanien) Mount Rainier^).4 392 Verein. (Washingt.^ Windom Peak .4 294 SanKaskadengebirgeJuan Mountains Staaten /(Colorado) Antarktis Mount Robson .3 954 Rocky Mountains Kanada Mount Vinson . 5 140 Marie-Byrd-Land Gunnbjörn Fjeld .3 700 Grönland(Ostgrönl.) Mount Kirkpatrick . 4 530 SentinelgebirgeKönigin-Älexandra-Kette Victorialand Mount Doonerak.3 060 Brooks Range Verein. \ (Alaska) Mount Jackson. 4 190 Eternity Range Palmerland Mount Mitchell .2 039 Blue Ridge Staaten /(Nordkarol.) Mount Sabine . 3 850 Admiralitäts-Berge Victorialand ’)Höhe in m über Meeresspiegel. ^)In geologisch jüngster Zeit(Quartär)noch tätiger Vulkan..
Recommended publications
  • Project of Strategic Interest NEXTDATA
    Project of Strategic Interest NEXTDATA WP 1.2 - GAW-WMO climate observatories Deliverable D1.2.5 Report on the upgrade of GAW-WMO stations with Italian management and related to the SHARE project. WP Coordinator: Angela Marinoni CNR-ISAC Partners: CNR-ISAC, URT Ev-K2-CNR 1 Report on upgrade carried out at GAW Global Stations “O. Vittori” at Monte Cimone and Nepal Climate Observatory Pyramid in the Himalayas 1. “O. Vittori” at Monte Cimone (2165 m, Northern Appenines) The upgrades carried out at Monte Cimone station concern aerosol, gases and radiation measurements. In particular the following measurement programs have been upgraded: - Aerosol size distribution from 10 nm to 800 nm has been completely renewed according to GAW/ACTRIS recommendations. - Aerosol scattering coefficient measured since 2007 at 525 nm has been upgraded with measurement in two additional wave lengths: 450 and 700 nm. Moreover, the following measurement programs have been newly started: - The aerosol size distribution from 500 nm to 20 µm based on time of flight was set up in July 2013. - Radiation measurement program (feasibility study). - Continuous nitrogen oxides (NOx), nitric oxide (NO) and nitrogen dioxide (NO2) measurements suitable for remote high-mountain stations (on test at Bologna laboratories). - Continuous of (SO2) sulfur dioxide measurements is on test in Bologna laboratories, ready for installation at CMN station. - Observations of aerosol vertical profiles have been carried out at Mt. Cimone. After a test installation in October 2012, several improvements were carried out in order to guarantee continuous observations also during winter season. I. Aerosol size distribution from 10 nm to 800 nm The number size distribution of atmospheric aerosol particles is a basic, but essential parameter required in calculations of the effects of aerosols on climate, human health, and eco-systems.
    [Show full text]
  • Climate Signals in a Multispecies Tree-Ring Network from Central And
    Clim. Past Discuss., doi:10.5194/cp-2017-48, 2017 Manuscript under review for journal Clim. Past Discussion started: 17 March 2017 c Author(s) 2017. CC-BY 3.0 License. 1 Climate signals in a multispecies tree-ring network from central and 2 southern Italy and reconstruction of the late summer temperatures 3 since the early 1700s 4 5 Giovanni Leonelli1, Anna Coppola2, Maria Cristina Salvatore2, Carlo Baroni2,3, Giovanna Battipaglia4,5, 6 Tiziana Gentilesca6, Francesco Ripullone6, Marco Borghetti6, Emanuele Conte7, Roberto Tognetti7, Marco 7 Marchetti7, Fabio Lombardi8, Michele Brunetti9, Maurizio Maugeri9,10, Manuela Pelfini11, Paolo 8 Cherubini12, Antonello Provenzale3, Valter Maggi1,3 9 10 1 Università degli Studi di Milano–Bicocca — Dept. of Earth and Environmental Science 11 2 Università degli Studi di Pisa — Dept. of Earth Science 12 3 Istituto di Geoscienze e Georisorse, Consiglio Nazionale delle Ricerche, Pisa 13 4 Università della Campania — Dept. DiSTABiF 14 5 University of Montpellier 2 (France) — PALECO EPHE 15 6 Università degli Studi della Basilicata — School of Agricultural, Forestry, Food and Environmental Sciences, Potenza 16 7 Università degli Studi del Molise — Dept. of Bioscience and Territory 17 8 Università Mediterranea di Reggio Calabria — Dept. of Agronomy 18 9 Istituto di Scienze dell’Atmosfera e del Clima, Consiglio Nazionale delle Ricerche, Bologna 19 10 Università degli Studi di Milano — Dept. of Physics 20 11 Università degli Studi di Milano — Dept. of Earth Science 21 12 Swiss Federal Institute for Forest, Snow and Landscape Research WSL (Switzerland) 22 Correspondence to: Giovanni Leonelli ([email protected]) 23 Abstract. A first assessment of the main climatic drivers that modulate the tree-ring width (RW) and maximum latewood 24 density (MXD) along the Italian Peninsula and northeastern Sicily was performed using 27 forest sites, which include conifers 25 (RW and MXD) and broadleaves (only RW).
    [Show full text]
  • Moüjmtaiim Operations
    L f\f¿ áfó b^i,. ‘<& t¿ ytn) ¿L0d àw 1 /1 ^ / / /This publication contains copyright material. *FM 90-6 FieW Manual HEADQUARTERS No We DEPARTMENT OF THE ARMY Washington, DC, 30 June 1980 MOÜJMTAIIM OPERATIONS PREFACE he purpose of this rUanual is to describe how US Army forces fight in mountain regions. Conditions will be encountered in mountains that have a significant effect on. military operations. Mountain operations require, among other things^ special equipment, special training and acclimatization, and a high decree of self-discipline if operations are to succeed. Mountains of military significance are generally characterized by rugged compartmented terrain witn\steep slopes and few natural or manmade lines of communication. Weather in these mountains is seasonal and reaches across the entireSspectrum from extreme cold, with ice and snow in most regions during me winter, to extreme heat in some regions during the summer. AlthoughNthese extremes of weather are important planning considerations, the variability of weather over a short period of time—and from locality to locahty within the confines of a small area—also significantly influences tactical operations. Historically, the focal point of mountain operations has been the battle to control the heights. Changes in weaponry and equipment have not altered this fact. In all but the most extreme conditions of terrain and weather, infantry, with its light equipment and mobility, remains the basic maneuver force in the mountains. With proper equipment and training, it is ideally suited for fighting the close-in battfe commonly associated with mountain warfare. Mechanized infantry can\also enter the mountain battle, but it must be prepared to dismount and conduct operations on foot.
    [Show full text]
  • Zur Verbreitung Von Permafrost Am Dachstein (Nördliche Kalkalpen, Steiermark)
    ZOBODAT - www.zobodat.at Zoologisch-Botanische Datenbank/Zoological-Botanical Database Digitale Literatur/Digital Literature Zeitschrift/Journal: Mitteilungen des naturwissenschaftlichen Vereins für Steiermark Jahr/Year: 1991 Band/Volume: 121 Autor(en)/Author(s): Lieb Gerhard Karl, Schopper Andreas Artikel/Article: Zur Verbreitung von Permafrost am Dachstein (Nördliche Kalkalpen, Steiermark). 149-163 © Naturwissenschaftlicher Verein für Steiermark; download unter www.biologiezentrum.at Mitt, naturwiss. Ver. Steiermark Band 121 S. 149-163 Graz 1991 Zur Verbreitung von Permafrost am Dachstein (Nördliche Kalkalpen, Steiermark) Von Gerhard Karl LlEB und Andreas SCHÖPFER Mit 8 Abbildungen und 3 Tabellen (im Text) Eingelangt am 3. Januar 1991 Angenommen am 10. Januar 1991 Zusammenfassung: Nach einführenden Bemerkungen über den alpinen Permafrost und einer kurzen Präsentation des Untersuchungsgebietes mit seiner Vergletscherung werden Ergebnisse von Grabungen, Quelltemperaturmessungen und Basistemperaturmessungen der winterlichen Schneedecke (BTS) diskutiert. Hiermit wird die Existenz von Permafrost erst- mals für den Dachstein nachgewiesen und, vor allem mit Hilfe der BTS-Meßergebnisse, erst- mals dessen Verbreitung für ein wenn auch kleines Areal der Nordalpen flächenhaft darge- stellt. Die Untergrenze des diskontinuierlichen Permafrosts liegt in N-Exposition bei rund 2300 m und steigt zu den Zentralalpen hin an. Summary: The distribution of permafrost in the Dachstein massive (Northern Lime- stone Alps, Styria, Austria). After some comments on alpine permafrost a short presentation of the investigated area including its glaciation is given. Then results of digging, temperature measuring of springs as well as measurements of the basical temperature of the winter snow cover are discussed. Thus the existence of permafrost in the Dachstein massive is proved for the first time. Also for the first time a map of permafrost distribution for a small area of the Northern Alps can be drawn.
    [Show full text]
  • We Make It Easier for You to Sell
    We Make it Easier For You to Sell Travel Agent Reference Guide TABLE OF CONTENTS ITEM PAGE ITEM PAGE Accommodations .................. 11-18 Hotels & Facilities .................. 11-18 Air Service – Charter & Scheduled ....... 6-7 Houses of Worship ................... .19 Animals (entry of) ..................... .1 Jamaica Tourist Board Offices . .Back Cover Apartment Accommodations ........... .19 Kingston ............................ .3 Airports............................. .1 Land, History and the People ............ .2 Attractions........................ 20-21 Latitude & Longitude.................. .25 Banking............................. .1 Major Cities......................... 3-5 Car Rental Companies ................. .8 Map............................. 12-13 Charter Air Service ................... 6-7 Marriage, General Information .......... .19 Churches .......................... .19 Medical Facilities ..................... .1 Climate ............................. .1 Meet The People...................... .1 Clothing ............................ .1 Mileage Chart ....................... .25 Communications...................... .1 Montego Bay......................... .3 Computer Access Code ................ 6 Montego Bay Convention Center . .5 Credit Cards ......................... .1 Museums .......................... .24 Cruise Ships ......................... .7 National Symbols .................... .18 Currency............................ .1 Negril .............................. .5 Customs ............................ .1 Ocho
    [Show full text]
  • The Pirin Mountains, Bulgaria) in the Last Ten Years
    STUDIA GEOMORPHOLOGICA CARPATHO-BALCANICA VOL. XLV, 2011: 47–68 PL ISSN 0081-6434 EMIL GACHEV (BLAGOEVGRAD) INTER-ANNUAL SIZE VARIATIONS OF SNEZHNIKA GLACIERET (THE PIRIN MOUNTAINS, BULGARIA) IN THE LAST TEN YEARS Abstract: Glacierets, which are in fact embryonic forms of recent glaciation, can serve as important indicators of contemporary climate dynamics in areas where classical glaciers do not exist, such as the high mountains in Southeastern Europe. Two glacierets are located in Bulgaria’s Pirin Mountains: Snezhnika and Banski Suhodol. Snezhnika has been relatively well studied for the last 50 years, and in particular since 1994, when annual size measurements on a regular basis started. The present study focuses on the recent variations in the size of Snezhnika i.e. in the last ten years. Data about the area of the glacieret at the end of the ablation season (in autumn), which was obtained for each year by field measurements and analytical calculations, show that temperature can be considered as a major factor that drives glacieret fluctuations. At the current stage precipitation factor can not be evaluated properly due to the deficit of accurate climate information. Key words: the Pirin Mountains, glacierets, size variation, climate change, climatic factors INTRODUCTION Although small in size and volume, in many mountain areas glacierets are natu- ral features of sufficient value for studies of the dynamics of environmental proc- esses, climatic variations and change. Glacierets are small bodies of perennial ice, which are smaller than glaciers but bigger and more persistent than snow patches. Glacierets are typified by a density of close-to-bottom ice of about 0.6 to 0.8 g cm–3, presence of annual layers in the vertical cross-section, and long- term persistence — decades to centuries (G r u n e w a l d et al.
    [Show full text]
  • THE NORDEND of MONTE ROSA. T. Graham Brown
    THE • VOL. LIII NOVEMBER I 942 NO. 265 THE NORDEND OF MONTE ROSA BY T. GRAHAM BROWN Substance of a lecture delivered before the Alpine Club, December g, 1941. T is curious to reflect that the ascent of the N ordend might have been one of the most popular in the Alps had the Dufourspitze been but 83 ft. lower. As things are, the mountain is relatively neglected. The usual route to its graceful summit lies off the beaten track, and more .often than not the N ordend is omitted during traverses of the Monte Rosa peaks ; parties from the Marinelli hut seem almost invariably to take the easier but more dangerous route to the Dufour­ spitze in preference to the more difficult ascent of the N ordend by its stupendous Macugnaga face ; the sensational Frontier arete, 1 which plunges to the Jagerjoch in vertical steps, has rarely been visited ; and (to the best of my knowledge) the wide and steep Weisstor (or N.E.) face of the N ordend has so far received attention from but a single climbing party. To these striking neglects may be added a fifth: on only one former occasion, and that was nearly thirty years ago, has the Nordend been the subject of a paper read before the Club.2 The event deserves to be recalled, because it was then that E. A. Broome described his expedition of 191 I, when, in the course of the day, he ascended the Macugnaga face from the Marinelli hut and descended by the ordinary route to the Riffelhaus the memorable achievement of a great climber who was in his sixty-seventh year at the time of the ascent.
    [Show full text]
  • Los Cien Montes Más Prominentes Del Planeta D
    LOS CIEN MONTES MÁS PROMINENTES DEL PLANETA D. Metzler, E. Jurgalski, J. de Ferranti, A. Maizlish Nº Nombre Alt. Prom. Situación Lat. Long. Collado de referencia Alt. Lat. Long. 1 MOUNT EVEREST 8848 8848 Nepal/Tibet (China) 27°59'18" 86°55'27" 0 2 ACONCAGUA 6962 6962 Argentina -32°39'12" -70°00'39" 0 3 DENALI / MOUNT McKINLEY 6194 6144 Alaska (USA) 63°04'12" -151°00'15" SSW of Rivas (Nicaragua) 50 11°23'03" -85°51'11" 4 KILIMANJARO (KIBO) 5895 5885 Tanzania -3°04'33" 37°21'06" near Suez Canal 10 30°33'21" 32°07'04" 5 COLON/BOLIVAR * 5775 5584 Colombia 10°50'21" -73°41'09" local 191 10°43'51" -72°57'37" 6 MOUNT LOGAN 5959 5250 Yukon (Canada) 60°34'00" -140°24’14“ Mentasta Pass 709 62°55'19" -143°40’08“ 7 PICO DE ORIZABA / CITLALTÉPETL 5636 4922 Mexico 19°01'48" -97°16'15" Champagne Pass 714 60°47'26" -136°25'15" 8 VINSON MASSIF 4892 4892 Antarctica -78°31’32“ -85°37’02“ 0 New Guinea (Indonesia, Irian 9 PUNCAK JAYA / CARSTENSZ PYRAMID 4884 4884 -4°03'48" 137°11'09" 0 Jaya) 10 EL'BRUS 5642 4741 Russia 43°21'12" 42°26'21" West Pakistan 901 26°33'39" 63°39'17" 11 MONT BLANC 4808 4695 France 45°49'57" 06°51'52" near Ozero Kubenskoye 113 60°42'12" c.37°07'46" 12 DAMAVAND 5610 4667 Iran 35°57'18" 52°06'36" South of Kaukasus 943 42°01'27" 43°29'54" 13 KLYUCHEVSKAYA 4750 4649 Kamchatka (Russia) 56°03'15" 160°38'27" 101 60°23'27" 163°53'09" 14 NANGA PARBAT 8125 4608 Pakistan 35°14'21" 74°35'27" Zoji La 3517 34°16'39" 75°28'16" 15 MAUNA KEA 4205 4205 Hawaii (USA) 19°49'14" -155°28’05“ 0 16 JENGISH CHOKUSU 7435 4144 Kyrghysztan/China 42°02'15" 80°07'30"
    [Show full text]
  • A Hydrographic Approach to the Alps
    • • 330 A HYDROGRAPHIC APPROACH TO THE ALPS A HYDROGRAPHIC APPROACH TO THE ALPS • • • PART III BY E. CODDINGTON SUB-SYSTEMS OF (ADRIATIC .W. NORTH SEA] BASIC SYSTEM ' • HIS is the only Basic System whose watershed does not penetrate beyond the Alps, so it is immaterial whether it be traced·from W. to E. as [Adriatic .w. North Sea], or from E. toW. as [North Sea . w. Adriatic]. The Basic Watershed, which also answers to the title [Po ~ w. Rhine], is short arid for purposes of practical convenience scarcely requires subdivision, but the distinction between the Aar basin (actually Reuss, and Limmat) and that of the Rhine itself, is of too great significance to be overlooked, to say nothing of the magnitude and importance of the Major Branch System involved. This gives two Basic Sections of very unequal dimensions, but the ., Alps being of natural origin cannot be expected to fall into more or less equal com­ partments. Two rather less unbalanced sections could be obtained by differentiating Ticino.- and Adda-drainage on the Po-side, but this would exhibit both hydrographic and Alpine inferiority. (1) BASIC SECTION SYSTEM (Po .W. AAR]. This System happens to be synonymous with (Po .w. Reuss] and with [Ticino .w. Reuss]. · The Watershed From .Wyttenwasserstock (E) the Basic Watershed runs generally E.N.E. to the Hiihnerstock, Passo Cavanna, Pizzo Luceridro, St. Gotthard Pass, and Pizzo Centrale; thence S.E. to the Giubing and Unteralp Pass, and finally E.N.E., to end in the otherwise not very notable Piz Alv .1 Offshoot in the Po ( Ticino) basin A spur runs W.S.W.
    [Show full text]
  • When Christopher Columbus Came Ashore in 1492, He Wrote in His Diary
    When Christopher Columbus came ashore in 1492, he wrote in his diary, “This is the most beautiful land that human eyes have seen.” He would leave members of his family behind to colonize the island and would return to it after venturing throughout the Caribbean. In his will, he asked to be buried in Santo Domingo, Dominican Republic. It was to this island a group of 22, mostly graduate nursing students and faculty from University of San Diego (www.sandiego.edu) , along with one dentist, would travel as a mission endeavor, to improve the health of school children of a rural school. Excitement ran high as the emails & gmails flashed back and forth, final arranges were gelling into a final plan. Were we actually going to the Caribbean? Over six months in the planning, and after 8 prior visits to La Republica Dominicana (Dominican Republic in English, indigenous Taino Indians called it Quisqueya), the trip was finally coming to fruition. It was decided that now was the time to include dental care in the overall plan to help the needy families far into the mountainous area near the international border with Haiti. Destination, El Cercado, to work at the school, Fe y Alegria (“Faith and Gladness”); the goal, examine students and their families in health screening as well as undertake a couple of research projects, one having to do with new techniques for diagnosing diabetes compared to traditional methods. But after having seen the severe need in oral disease, this was the year to begin inclusion of emergency dental care.
    [Show full text]
  • Alpine Adventures 2019 68
    RYDER WALKER THE GLOBAL TREKKING SPECIALISTS ALPINE ADVENTURES 2019 68 50 RYDER WALKER ALPINE ADVENTURES CONTENTS 70 Be the first to know. Scan this code, or text HIKING to 22828 and receive our e-newsletter. We’ll send you special offers, new trip info, RW happenings and more. 2 RYDERWALKER.COM | 888.586.8365 CONTENTS 4 Celebrating 35 years of Outdoor Adventure 5 Meet Our Team 6 Change and the Elephant in the Room 8 Why Hiking is Important – Watching Nature 10 Choosing the Right Trip for You 11 RW Guide to Selecting Your Next Adventure 12 Inspired Cuisine 13 First Class Accommodations 14 Taking a Closer Look at Huts 15 Five Reasons Why You Should Book a Guided Trek 16 Self-Guided Travel 17 Guided Travel & Private Guided Travel EASY TO MODERATE HIKING 18 Highlights of Switzerland: Engadine, Lago Maggiore, Zermatt 20 England: The Cotswolds 22 Isola di Capri: The Jewel of Southern Italy NEW 24 French Alps, Tarentaise Mountains: Bourg Saint Maurice, Sainte Foy, Val d’Isère 26 Sedona, Arches & Canyonlands 28 Croatia: The Dalmatian Coast 28 30 Engadine Trek 32 Scotland: Rob Roy Way 34 Montenegro: From the Durmitor Mountain Range to the Bay of Kotor 36 New Mexico: Land of Enchantment, Santa Fe to Taos NEW 38 Slovakia: Discover the Remote High Tatras Mountains NEW MODERATE TO CHALLENGING HIKING 40 Heart of Austria 42 Italian Dolomites Trek 44 High Peaks of the Bavarian Tyrol NEW 46 Sicily: The Aeolian Islands 48 Rocky Mountain High Life: Aspen to Telluride 50 New Brunswick, Canada: Bay of Fundy 52 Via Ladinia: Italian Dolomites 54 Dolomiti di
    [Show full text]
  • O-1 the Epithelial-To-Mesenchymal Transition Protein Periostin Is
    Virchows Arch (2008) 452 (Suppl 1):S1–S286 DOI 10.1007/s00428-008-0613-x O-1 O-2 The epithelial-to-mesenchymal transition protein Squamous cell carcinoma of the lung: polysomy periostin is associated with higher tumour stage of chromosome 7 and wild type of exon 19 and 21 and grade in non-small cell lung cancer were defined for the EGFR gene Alex Soltermann; Laura Morra; Stefanie Arbogast; Vitor Sousa; Maria Silva; Ana Alarcão; Patrícia Peter Wild; Holger Moch, Glen Kristiansen Couceiro; Ana Gomes; Lina Carvalho Institute for Surgical Pathology Zürich, Switzerland Instituto de Anatomia Patológica - Faculdade de Medicina da Universidade de Coimbra, Portugal Background: The epithelial-to-mesenchymal transition (EMT) is vital for morphogenesis and has been implicated BACKGROUND: The use of tyrosine kinase inhibitors in cancer invasion. EMT of carcinoma cells can be defined after first line chemotherapy, induced several studies to by morphological trans-differentiation, accompanied by determine molecular characteristics in non-small-cell lung permanent cytosolic overexpression of mesenchymal pro- cancer to predict the response to those drugs. teins, which are normally expressed in the peritumoural The present study was delineated to clarify the status of stroma. We aimed for correlating the expression levels of EGFR gene by Fluorescence in situ Hibridization(FISH), the EMT indicator proteins periostin and vimentin with Polimerase Chain Reaction (PCR) and Immunohistochem- clinico-pathological parameters of non-small cell lung ical protein expression in 60 cases of squamous cell cancer (NSCLC). Method: 538 consecutive patients with carcinoma of the lung after surgical resection of tumours surgically resected NSCLC were enrolled in the study and a in stages IIb/IIIa.
    [Show full text]