World Heritage Nomination - Iucn Technical Evaluation
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Rain Shadows
WEB TUTORIAL 24.2 Rain Shadows Text Sections Section 24.4 Earth's Physical Environment, p. 428 Introduction Atmospheric circulation patterns strongly influence the Earth's climate. Although there are distinct global patterns, local variations can be explained by factors such as the presence of absence of mountain ranges. In this tutorial we will examine the effects on climate of a mountain range like the Andes of South America. Learning Objectives • Understand the effects that topography can have on climate. • Know what a rain shadow is. Narration Rain Shadows Why might the communities at a certain latitude in South America differ from those at a similar latitude in Africa? For example, how does the distribution of deserts on the western side of South America differ from the distribution seen in Africa? What might account for this difference? Unlike the deserts of Africa, the Atacama Desert in Chile is a result of topography. The Andes mountain chain extends the length of South America and has a pro- nounced influence on climate, disrupting the tidy latitudinal patterns that we see in Africa. Let's look at the effects on climate of a mountain range like the Andes. The prevailing winds—which, in the Andes, come from the southeast—reach the foot of the mountains carrying warm, moist air. As the air mass moves up the wind- ward side of the range, it expands because of the reduced pressure of the column of air above it. The rising air mass cools and can no longer hold as much water vapor. The water vapor condenses into clouds and results in precipitation in the form of rain and snow, which fall on the windward slope. -
Amit Wasnik & Shubham Jain
- Amit Wasnik & Shubham Jain What is a Biome? A biome is a geographic area characterized by specific kinds of plants and animals. Deserts, tropical rainforests, and tundra are all types of biomes. In the desert biome many organisms have learned to adapt to the hot climate and lack of supplements. Deserts are formed by mountains blocking the path of precipitation . Deserts can be hot or cold but they are always dry. They receive less than 25 cm of precipitation annually. They cover 22 million km2 or 1/5 of the earth’s surface. Hot Desert eg. Thar, in Rajasthan, India Rub-ab-khali, Saudi Arab . Cold Desert eg. Gobi desert, Mangolia Ica desert, Peru A Desert’s CharacteristicsCharacteristics Climate Seasons Animals Adaptations Plants Significance to humans ClimateClimate The desert is the hottest biome on Earth. It also has its extremes. It can be over 50 degrees during the day and below 32 degrees at night. Less than 25 cm or rainfall every year. The amount of rainfall varies, but when it rains…it POURS!!!! After a storm, the desert may not see any rain for weeks or months. The animals include snakes, owls, mice, armadillo lizards, fennec foxes, gila monsters, bats, and vultures. EndangeredEndangered AnimalsAnimals Black Rhino The major causes of endangered animals Grevy’s in the desert are Zebra mainly poachers and unexpected drought. King Cheetah PlantPlant LifeLife ofof DesertsDeserts There are several plants that are able to survive in the desert. Most plants survive by their long roots to reach underground water sources. A Variety of cactuses Prickly Pear Dragon Tree Octillo Plant Desert Spoon Boojum i. -
Baja California's Sonoran Desert
Baja California’s Sonoran Desert By Debra Valov What is a Desert? It would be difficult to find any one description that scarce and sporadic, with an would fit all of the twenty or so deserts found on our annual average of 12-30 cm (4.7- planet because each one is a unique landscape. 12 inches). There are two rainy seasons, December- While an expanse of scorching hot sand dunes with March and July-September, with the northern the occasional palm oasis is the image that often peninsula dominated by winter rains and the south comes to mind for the word desert, in fact, only by summer rains. Some areas experience both about 10% of the world’s deserts are covered by seasons, while in other areas, such as parts of the sand dunes. The other 90% comprise a wide variety Gulf coast region, rain may fail for years on end. of landscapes, among these cactus covered plains, Permanent above-ground water reserves are scarce foggy coastal slopes, barren salt flats, and high- throughout most of the peninsula but ephemeral, altitude, snow-covered plateaus. However, one seasonal pools and rivers do appear after winter characteristic that all deserts share is aridity—any storms in the north or summer storms (hurricanes place that receives less than 10 inches (25 and thunderstorms—chubascos) in the south. There centimeters) of rain per year is generally considered are also a number of permanent oases, most often to be a desert and the world’s driest deserts average formed where aquifers (subterranean water) rise to less than 10 mm (3/8 in.) annually. -
Download the Dossier
THE LATIN AMERICA TRAVEL COMPANY TAILOR MADE ARGENTINA SELF DRIVE, MENDOZA TO SALTA ITINERARY ▶ CONTENTS, ABOUT US & TRIP SUMMARY CONTENTS OF THIS DOSSIER TRIP SUMMARY 2 ..... Contents, about us & trip summary DAY 1: Meet & greet at airport, private transfer to hotel 3 ….. Testimonials DAY 2: A city tour of the highlights of Buenos Aires 4 ..... Guide price and inclusions DAY 3: Fly to Mendoza, transfer to vineyard & asado dinner 5 ..... Detailed day by day itinerary DAY 4: A day of wine tasting at high end wineries & lunch 19 ... Recommended reading list DAY 5: Start driving north, stopping in Villa Unión 20 ... Booking conditions DAY 6: 4X4 excursion to the high Andean Puna DAY 7: Talampaya national park & a scenic drive to Belen ABOUT OUR COMPANY DAY 8: Drive to the wine town of Cafayate DAY 9: A day at leisure to visit wineries & enjoy the scenery As one of the UK’s leading, independent and family owned Latin DAY 10: Drive past the most stunning landscapes to Cachi America tour specialists our focus is on well thought through private and tailor made adventures. Our emphasis is very much on DAY 11: Continue past Los Cardones to Salta creating the right trip for you and we work closely with you in order DAY 12: A day at leisure or optional horse riding to achieve this. We use our experience and knowledge to ensure DAY 13: Return to Salta airport & fly back to Buenos Aires your trip to Latin America is a trip of a lifetime! DAY 14: Private transfer to the airport for departure ALL TOURS ARE FINANCIALLY PROTECTED SPEAK TO SOMEONE WHO HAS BEEN TO ARGENTINA THE LATIN AMERICA TRAVEL COMPANY We are members of ABTA (Y1699) and our tours are ATOL protected ■ www.thelatinamericatravelcompany.com (license 10287) giving you full peace of mind when booking with us ■ [email protected] both for monies paid to us as well as the code of conduct and high ☎ standards that membership of these organisations require. -
Living in the Desert Desert World Activity
desert World Activity Living in the desert desert World Activity Living in the desert In this activity your students will be looking at what makes a desert a desert. They will look at hot deserts (like the Arabian Desert) and cold deserts (like the Patagonian desert) and compare and contrast some of the animals that live there. Based on what they have learned they can then design their own fantasy desert animal! In this activity you and your students will: ▶ Learn about the definition of a desert. ▶ Learn about the evolutionary adaptations that ▶ Learn about hot and cold deserts. the animals have made to live in these different desert environments. ▶ Design their own fantasy desert animal. Objectives Carrying out this activity will help students learn about deserts and some of the animals that call them home. They will also learn about how animals cope with the heat and the cold and how this affects the way they look and behave. You can also ask your class to design their own fantasy desert animal showcasing the special adaptations that they have learned about. These can be displayed in the classroom and uploaded to the Roots & Shoots UAE website to share with the world. What do I need to make it work? You do not need anything special for the first part of this activity (which can be done in the classroom), just an internet connection to carry out some background reading, view pictures and watch some video segments. To design their own fantasy desert animal your students can use paper and coloured pens/pencils, or why not incorporate craft materials to make the designs more exciting, or even make a 3-dimensional creature! What things will my students create? ▶ Drawings and/or models of a fantasy desert animal. -
Narratives of Patagonian Exploration Mark W
University of Richmond UR Scholarship Repository Master's Theses Student Research Fall 8-2001 Going to nowhere : narratives of Patagonian exploration Mark W. Bell Follow this and additional works at: http://scholarship.richmond.edu/masters-theses Part of the English Language and Literature Commons Recommended Citation Bell, Mark W., "Going to nowhere : narratives of Patagonian exploration" (2001). Master's Theses. Paper 1143. This Thesis is brought to you for free and open access by the Student Research at UR Scholarship Repository. It has been accepted for inclusion in Master's Theses by an authorized administrator of UR Scholarship Repository. For more information, please contact [email protected]. Abstract Since its discovery on Magellan's circumnavigation, Patagonia has been treated differently than any other region in the world. Effectively, Patagonia has been left empty or vacated by the North. But this emptiness and blankness have compulsively attracted curious travel writers who have filled the emptiness of Patagonia with self-reflexive projections. From Charles Darwin and W.H. Hudson to Bruce Chatwin and Paul Theroux, Northern commentators have found in Patagonia a landscape that accommodates their desire for self-reflexivity and self-consciousness. Thus, Patagonia has been simultaneously filled and evacuated by the Northern mind. As a result, Patagonia has become increasingly about the self and less about the physical place to the point where Patagonia as a concept has been abstracted and made into a trope or condition. This paper examines the history of Patagonia in literature in English and analyzes how Patagonia has evolved into its modem signification. I certify that I have read this thesis and find that, in scope and quality, it satisfies the requirements for the degree of Master of Arts. -
Dry Lands and Desertification - Willy Verheye
LAND USE, LAND COVER AND SOIL SCIENCES – Vol. V – Dry Lands and Desertification - Willy Verheye DRY LANDS AND DESERTIFICATION Willy Verheye National Science Foundation Flanders/Belgium, and Geography Department, University of Gent, Belgium Keywords: Aerosols, aridity, crop adaptation, desertification, dust storms, fuel wood, irrigation, land degradation, over-grazing, rangeland, water harvesting, wildfires, and xerophytes Contents 1. Introduction 2. Extension of Dry Lands 3. Definition of Dry Lands and Aridity 3.1. Climate-based Definitions 3.2. Non Climate-based Definitions 4. Main Features of Desert Environments 4.1. Rainfall 4.2. Temperature 4.3. Wind 4.4. Vegetation and Biological Activity 4.5. Soils 4.6. Salinity 4.7. Impact of Man 5. Use and Management of Dry Lands 5.1. Surface Water Management and Water Harvesting 5.2. Groundwater Exploitation and Recharge 5.3. Irrigation and Drainage 5.4. Crop Adaptation 5.5 Soil Fertility Management 5.6. Extensive Grazing 6. Desertification 6.1. Introduction 6.2. Causes ofUNESCO Desertification – EOLSS 6.3. Indicators and Classification of Desertification 6.4 Combating Desertification Glossary Bibliography SAMPLE CHAPTERS Biographical Sketch Summary Dry lands are areas which have no water available to mesophytic plants. Aridity can have a climatic or a plant-physiological basis. Desertification is the process which leads to aridity, either because of a deteriorating rainfall regime or due to a degradation of the environment by human activities. Dry lands extend over approximately 35 % of the ©Encyclopedia of Life Support Systems (EOLSS) LAND USE, LAND COVER AND SOIL SCIENCES – Vol. V – Dry Lands and Desertification - Willy Verheye global land surface. -
Chemical Properties of Continental Aerosol Transported Over the Southern Ocean: Patagonian and Namibian Sources
Chemical properties of continental aerosol transported over the Southern Ocean : Patagonian and Namibian sources Zihan Qu To cite this version: Zihan Qu. Chemical properties of continental aerosol transported over the Southern Ocean : Patago- nian and Namibian sources. Geochemistry. Université Pierre et Marie Curie - Paris VI, 2016. English. NNT : 2016PA066002. tel-01349197 HAL Id: tel-01349197 https://tel.archives-ouvertes.fr/tel-01349197 Submitted on 27 Jul 2016 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. 8QLYHUVLWp3LHUUHHW0DULH&XULH (FROHGRFWRUDOH±6FLHQFHVGHO¶HQYLURQQHPHQWGHO¶,OHGH)UDQFH /DERUDWRLUH,QWHUXQLYHUVLWDLUHGHV6\VWqPHV$WPRVSKpULTXHV /,6$ 805 &15683'83(& &KHPLFDOSURSHUWLHVRIFRQWLQHQWDODHURVRO WUDQVSRUWHGRYHUWKH6RXWKHUQ2FHDQ3DWDJRQLDQ DQG1DPLELDQVRXUFHV 3DU=LKDQ48 7KqVHGHGRFWRUDWGH*pRFKLPLH 'LULJpHSDU5pPL/2612HWePLOLH-2851(7 3UpVHQWpHHWVRXWHQXHSXEOLTXHPHQWOH-DQYLHU 'HYDQWXQMXU\FRPSRVpGH 3UpVLGHQW'DPLHQ&$5',1$/3URIHVVHXU830&/2&($1 5DSSRUWHXU$OR\V%25<0DvWUHGH&RQIpUHQFHV8QLY/LOOH/2* 5DSSRUWHXU*DsO/(528;&KDUJpGHUHFKHUFKH&156(FR/DE ([DPLQDWHXU*LOOHV%(5*$0(77,'LUHFWHXUGHUHFKHUFKH&156/,6$ ([DPLQDWHXU-pU{PH*$,//$5'(73URIHVVHXU83',3*3 'LUHFWHXUGHWKqVH5pPL/26123URIHVVHXU83',3*3 &RGLUHFWULFHGHWKqVHePLOLH-2851(70DvWUHGHFRQIpUHQFHV83(&/,6$ I II III Remerciements J’adresse mes premiers remerciements à Rémi LOSNO et Émilie JOURNET pour la direction de ma thèse pendant trois ans. Rémi LOSNO montre toujours sa confiance pendant les travaux de recherche, sa tolérance à nos arguments et parfois mes caprices, sa patience et ses encouragements pendant la direction rigoureuse. -
Supplementary Information
SUPPLEMENTARY INFORMATION The oldest known communal latrines provide evidence of gregarism in Triassic megaherbivores Lucas E. Fiorelli*, Martín D. Ezcurra, E. Martín Hechenleitner, Eloisa Argañaraz, Jeremías R. A. Taborda, M. Jimena Trotteyn, M. Belén von Baczko & Julia B. Desojo *To whom correspondence should be addressed. E-mail: [email protected] 1. Provenance, authenticity, geological setting and stratigraphy of the communal latrines of the Chañares Formation 2. Depositional setting 3. Taphonomy 4. Statistics 5. Age of the Chañares Formation 6. Fossil tetrapods from the Chañares Formation 7. Dinodontosaurus body size 8. Dinodontosaurus as a gregarious megaherbivore 9. References 1. Provenance, authenticity, geological setting and stratigraphy of the communal latrines of the Chañares Formation. Several communal latrines were found in successive palaeontological field works conducted in 2011 and 2012 in outcrops of the Chañares Formation situated in the Talampaya National Park, La Rioja Province, northwestern Argentina (Supplementary Figure 1a). The Chañares Formation 1 crops out as part of the Ischigualasto-Villa Unión Basin, which represents a succession of continental deposits composed of 4,000 metres of alluvial, fluvial and lacustrine sediments 2,3 . The basin contains the reddish Talampaya and Tarjados formations as its lower- most units and corresponds to the Synrift 1 tectonic phase. The Talampaya Formation is dated as Induan/Olenekian (Early Triassic) and the Tarjados Formation as Anisian (early Middle Triassic) according to some authors 3,4 . The lower section of the Talampaya Formation is represented by alluvian fan deposits followed by fluvial and playa lake deposits in the middle and upper sections 4. The Tarjados Formation has aerealy extensive outcrops in the Talampaya National Park but at the moment no significant fossil vertebrate remains were reported. -
The Precise Temporal Calibration of Dinosaur Origins SEE COMMENTARY
The precise temporal calibration of dinosaur origins SEE COMMENTARY Claudia A. Marsicanoa, Randall B. Irmisb,c,1, Adriana C. Mancusod, Roland Mundile, and Farid Chemalef aDepartamento de Ciencias Geológicas, Instituto de Estudios Andinos-Consejo Nacional de Investigaciones Científicas y Técnicas, Universidad de Buenos Aires, Ciudad Autónoma de Buenos Aires C1428EHA, Argentina; bNatural History Museum of Utah, University of Utah, Salt Lake City, UT 84108-1214; cDepartment of Geology & Geophysics, University of Utah, Salt Lake City, UT 84112-0102; dInstituto Argentino de Nivología, Glaciología y Ciencias Ambientales, Centro Científico y Tecnológico-Consejo Nacional de Investigaciones Científicas y Técnicas-Mendoza, Mendoza CC330, Argentina; eBerkeley Geochronology Center, Berkeley, CA 94709; and fInstituto de Geociências, Universidade de Brasília, Brasília-DF 70864-050, Brazil Edited by Paul E. Olsen, Columbia University, Palisades, NY, and approved November 6, 2015 (received for review June 25, 2015) Dinosaurs have been major components of ecosystems for over 200 composition across Pangea appears to be particularly heteroge- million years. Although different macroevolutionary scenarios exist neous (11–13). Without precise independent age control (other to explain the Triassic origin and subsequent rise to dominance of than vertebrate biostratigraphic correlations), it is impossible to dinosaurs and their closest relatives (dinosauromorphs), all lack critical determine if these faunal differences vary across time, space, or a support from a precise biostratigraphically independent temporal combination of both. framework. The absence of robust geochronologic age control for Among the many uncertainties regarding dinosaur evolution is comparing alternative scenarios makes it impossible to determine if the timing of the origin and subsequent radiation of this clade and observed faunal differences vary across time, space, or a combination their closest relatives (early dinosauromorphs). -
Argentina Dario Podestá Dario
100 reasons to visit ARGENTINA DARIO PODESTÁ DARIO An amazing variety of landscapes and habitats... an impressive diversity of birds. Red-tailed Comet Picaflor cometa | Sappho sparganura Argentina comprises an amazing diversity of landscapes and habitats: from subtropical rainforests in the north to dry steppes and deserts in the south N and west; and from the highest peaks of the western SE N E J hemisphere in the Andes range, to the flatlowlands of ER LL the Pampas and Chaco. And everything in between. O For this reason there is an impressive diversity of MÓN M RA birds, with over 1000 species. In this brochure you will find a selection of Argentina’s bird fauna, with species significant for their uniqueness, rarity, or endemic status. They represent some of the species most sought-after by birdwatchers who visit this part of the globe. Credits. Idea and text: Marcelo Gavensky and Francisco González Taboas (Aves Argentinas). Edition and graphic design: Mariano Masariche. Colaboration: Roberto Güller. Technical revision: Alejandro Di Giacomo. Fotos: Roberto Güller; Adrián Aspiroz; Francisco Erize; Andrés Terán; Ramón Moller Jensen; Alec Earnshaw; Alejandro Ronchetti; Fernando Bernasconi; Francisco Lucero; Carlos Cuñado; Carlos Cáceres; Alberto Gurni and Luis Piovani. Ruddy-headed Goose Cauquén colorado | Chloephaga rubidiceps CISCO ERIZE CISCO N FRA ARGENTINA Bolivia JUJUY North Argentina’s SALTA 1 4 1 - Laguna de los Pozuelos Natural Monument TUCUMÁN 3 JUJUY CATAMARCA 2 - Calilegua National Park Chile 2 tourism SANTIAGO DEL 3 - Baritú -
Rock Art of Latin America & the Caribbean
World Heritage Convention ROCK ART OF LATIN AMERICA & THE CARIBBEAN Thematic study June 2006 49-51 rue de la Fédération – 75015 Paris Tel +33 (0)1 45 67 67 70 – Fax +33 (0)1 45 66 06 22 www.icomos.org – [email protected] THEMATIC STUDY OF ROCK ART: LATIN AMERICA & THE CARIBBEAN ÉTUDE THÉMATIQUE DE L’ART RUPESTRE : AMÉRIQUE LATINE ET LES CARAÏBES Foreword Avant-propos ICOMOS Regional Thematic Studies on Études thématiques régionales de l’art Rock Art rupestre par l’ICOMOS ICOMOS is preparing a series of Regional L’ICOMOS prépare une série d’études Thematic Studies on Rock Art of which Latin thématiques régionales de l’art rupestre, dont America and the Caribbean is the first. These la première porte sur la région Amérique latine will amass data on regional characteristics in et Caraïbes. Ces études accumuleront des order to begin to link more strongly rock art données sur les caractéristiques régionales de images to social and economic circumstances, manière à préciser les liens qui existent entre and strong regional or local traits, particularly les images de l’art rupestre, les conditions religious or cultural traditions and beliefs. sociales et économiques et les caractéristiques régionales ou locales marquées, en particulier Rock art needs to be anchored as far as les croyances et les traditions religieuses et possible in a geo-cultural context. Its images culturelles. may be outstanding from an aesthetic point of view: more often their full significance is L’art rupestre doit être replacé autant que related to their links with the societies that possible dans son contexte géoculturel.