Lake Titicaca
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Urban Interrelation and Regional Patterning in the Department of Puno, Southern Peru Jean Morisset
Document généré le 30 sept. 2021 04:15 Cahiers de géographie du Québec Urban interrelation and regional patterning in the department of Puno, Southern Peru Jean Morisset Volume 20, numéro 49, 1976 Résumé de l'article Le département de Puno s'inscrit autour du lac Titicaca (3 800 m au-dessus du URI : https://id.erudit.org/iderudit/021311ar niveau de la mer) pour occuper un vaste plateau (l'altiplano) ainsi que les DOI : https://doi.org/10.7202/021311ar hautes chaînes andines (la puna) et; déborder au nord vers le bassin amazonien (la selva). Aller au sommaire du numéro En utilisant à la fois des informations recueillies lors d'enquêtes sur le terrain et des données de recensement (1940 et 1961), cet essai poursuit un double objectif: on a tenté d'analyser d'une part, l'évolution et l'interdépendance des Éditeur(s) principaux centres du département de Puno pour proposer, d'autre part, une régionalisation à partir des structures géo-spatiales et des organisations Département de géographie de l'Université Laval administratives. De plus, on a brièvement traité de la nature des agglomérations et on a réalisé une analyse quantitative ISSN regroupant 30 variables reportées sur les 85 districts du département. 0007-9766 (imprimé) L'auteur conclut en suggérant que toute planification est un processus qui doit 1708-8968 (numérique) aboutir à un compromis entre des composantes spatio-économiques (planificaciôn tecno-crética) et des composantes socio-culturelles (planificaciôn Découvrir la revue de base). Citer cet article Morisset, J. (1976). Urban interrelation and regional patterning in the department of Puno, Southern Peru. -
Salt Lakes and Pans
SCIENCE FOCUS: Salt Lakes and Pans Ancient Seas, Modern Images SeaWiFS image of the western United States. The features of interest that that will be discussed in this Science Focus! article are labeled on the large image on the next page. (Other features and landmarks are also labeled.) It should be no surprise to be informed that the Sea-viewing Wide Field-of-view Sensor (SeaWiFS) was designed to observe the oceans. Other articles in the Science Focus! series have discussed various oceanographic applications of SeaWiFS data. However, this article discusses geological features that indicate the presence of seas that existed in Earth's paleohistory which can be discerned in SeaWiFS imagery. SeaWiFS image of the western United States. Great Salt Lake and Lake Bonneville The Great Salt Lake is the remnant of ancient Lake Bonneville, which gave the Bonneville Salt Flats their name. Geologists estimate that Lake Bonneville existed between 23,000 and 12,000 years ago, during the last glacial period. Lake Bonneville's existence ended abruptly when the waters of the lake began to drain rapidly through Red Rock Pass in southern Idaho into the Snake River system (see "Lake Bonneville's Flood" link below). As the Earth's climate warmed and became drier, the remaining water in Lake Bonneville evaporated, leaving the highly saline waters of the Great Salt Lake. The reason for the high concentration of dissolved minerals in the Great Salt Lake is due to the fact that it is a "terminal basin" lake; water than enters the lake from streams and rivers can only leave by evaporation. -
Relación De Agencias Que Atenderán De Lunes a Viernes De 8:30 A. M. a 5:30 P
Relación de Agencias que atenderán de lunes a viernes de 8:30 a. m. a 5:30 p. m. y sábados de 9 a. m. a 1 p. m. (con excepción de la Ag. Desaguadero, que no atiende sábados) DPTO. PROVINCIA DISTRITO NOMBRE DIRECCIÓN Avenida Luzuriaga N° 669 - 673 Mz. A Conjunto Comercial Ancash Huaraz Huaraz Huaraz Lote 09 Ancash Santa Chimbote Chimbote Avenida José Gálvez N° 245-250 Arequipa Arequipa Arequipa Arequipa Calle Nicolás de Piérola N°110 -112 Arequipa Arequipa Arequipa Rivero Calle Rivero N° 107 Arequipa Arequipa Cayma Periférica Arequipa Avenida Cayma N° 618 Arequipa Arequipa José Luis Bustamante y Rivero Bustamante y Rivero Avenida Daniel Alcides Carrión N° 217A-217B Arequipa Arequipa Miraflores Miraflores Avenida Mariscal Castilla N° 618 Arequipa Camaná Camaná Camaná Jirón 28 de Julio N° 167 (Boulevard) Ayacucho Huamanga Ayacucho Ayacucho Jirón 28 de Julio N° 167 Cajamarca Cajamarca Cajamarca Cajamarca Jirón Pisagua N° 552 Cusco Cusco Cusco Cusco Esquina Avenida El Sol con Almagro s/n Cusco Cusco Wanchaq Wanchaq Avenida Tomasa Ttito Condemaita 1207 Huancavelica Huancavelica Huancavelica Huancavelica Jirón Francisco de Angulo 286 Huánuco Huánuco Huánuco Huánuco Jirón 28 de Julio N° 1061 Huánuco Leoncio Prado Rupa Rupa Tingo María Avenida Antonio Raymondi N° 179 Ica Chincha Chincha Alta Chincha Jirón Mariscal Sucre N° 141 Ica Ica Ica Ica Avenida Graú N° 161 Ica Pisco Pisco Pisco Calle San Francisco N° 155-161-167 Junín Huancayo Chilca Chilca Avenida 9 De Diciembre N° 590 Junín Huancayo El Tambo Huancayo Jirón Santiago Norero N° 462 Junín Huancayo Huancayo Periférica Huancayo Calle Real N° 517 La Libertad Trujillo Trujillo Trujillo Avenida Diego de Almagro N° 297 La Libertad Trujillo Trujillo Periférica Trujillo Avenida Manuel Vera Enríquez N° 476-480 Avenida Victor Larco Herrera N° 1243 Urbanización La La Libertad Trujillo Victor Larco Herrera Victor Larco Merced Lambayeque Chiclayo Chiclayo Chiclayo Esquina Elías Aguirre con L. -
Spjl-Juliaca
AIS - PERÚ AD2 SPJL 1 30 JAN 20 AEROPUERTO INTERNACIONAL INCA MANCO CÁPAC - JULIACA (SPJL) REGIÓN / DEPARTAMENTO / PROVINCIA / DISTRITO PUNO / PUNO / SAN ROMÁN / JULIACA SPJL INDICADOR DE LUGAR Y NOMBRE 1 AEROPUERTO INTERNACIONAL DEL AERÓDROMO INCA MANCO CÁPAC DATOS GEOGRÁFICOS Y ADMINISTRATIVOS DEL AERÓDROMO 1 ARP 15º28’00.69”S - 070°09’28.38”W 2100 m FM THR 30 2 Distancia y direccion desde la ciudad 5 km al NW Elevación del aeródromo 3826 m / 12552 ft 3 Temperatura 19°C (NOV) 4 Ondulación Geoidal NIL Declinación Magnética 6°W (JAN 2015) 5 Cambio anual 0°11' W 2 Administración AD Aeropuertos Andinos del Perú S.A. - AAP Dirección Av. Aviación S/N - Juliaca - Perú Teléfono (051) 328226 6 Fax NIL AFTN SPJLYDYX Email [email protected] 7 Tránsito Autorizado VFR/IFR 8 Observaciones NIL HORAS DE FUNCIONAMIENTO 1 Administración del AD: 1200 - 0000 Aduana: 1200 - 0000 2 Inmigración: O/R 3 Servicios médicos: 1200 - 0000 4 Oficina de notificación AIS: 1200 - 0000 5 Oficina de notificación ATS (ARO): 1200 - 0000 3 6 Oficina de notificación MET: 1200 - 0000 7 ATS: 1200 - 0000 8 Abastecimiento de combustible: NO AVBL 9 Servicios de despacho: 1200 - 0000 10 Seguridad: h24 11 Descongelamiento: NIL 12 Observaciones: COM 1100 - 0000. Fuera de estas horas: O/R CORPAC S.A. AIS - PERÚ AMDT 26/19 AD2 SPJL 2 AIS - PERÚ 30 JAN 20 AEROPUERTO INTERNACIONAL INCA MANCO CÁPAC - JULIACA (SPJL) INSTALACIONES Y SERVICIOS DE ESCALA 1 Instalaciones de manipuleo de carga: 01 Montacarga de 2 L Tipos de combustible: NIL 2 Tipos de lubricante: NO AVBL 4 NIL 3 Instalaciones -
The Endemic Gastropod Fauna of Lake Titicaca: Correlation Between
The endemic gastropod fauna of Lake Titicaca: correlation between molecular evolution and hydrographic history Oliver Kroll1, Robert Hershler2, Christian Albrecht1, Edmundo M. Terrazas3, Roberto Apaza4, Carmen Fuentealba5, Christian Wolff1 & Thomas Wilke1 1Department of Animal Ecology and Systematics, Justus Liebig University Giessen, Germany 2National Museum of Natural History, Smithsonian Institution, Washington, D.C. 3Facultad de Ciencias Biologicas, Universidad Nacional del Altiplano, Puno, Peru 4Instituto de Ecologıa,´ Universidad Mayor de San Andres, La Paz, Bolivia 5Departamento de Zoologia, Universidad de Concepcion, Chile Keywords Abstract Altiplano, Heleobia, molecular clock, phylogeography, species flock. Lake Titicaca, situated in the Altiplano high plateau, is the only ancient lake in South America. This 2- to 3-My-old (where My is million years) water body has had Correspondence a complex history that included at least five major hydrological phases during the Thomas Wilke, Department of Animal Ecology Pleistocene. It is generally assumed that these physical events helped shape the evo- and Systematics, Justus Liebig University lutionary history of the lake’s biota. Herein, we study an endemic species assemblage Giessen, Heinrich Buff Ring 26–32 (IFZ), 35392 in Lake Titicaca, composed of members of the microgastropod genus Heleobia,to Giessen, Germany. Tel: +49-641-99-35720; determine whether the lake has functioned as a reservoir of relic species or the site Fax: +49-641-99-35709; of local diversification, to evaluate congruence of the regional paleohydrology and E-mail: [email protected] the evolutionary history of this assemblage, and to assess whether the geographic distributions of endemic lineages are hierarchical. Our phylogenetic analyses in- Received: 17 February 2012; Revised: 19 April dicate that the Titicaca/Altiplano Heleobia fauna (together with few extralimital 2012; Accepted: 23 April 2012 taxa) forms a species flock. -
Phylogenomics of the Hyalella Amphipod Species-Flock of The
www.nature.com/scientificreports OPEN Phylogenomics of the Hyalella amphipod species‑fock of the Andean Altiplano Francesco Zapelloni1,3, Joan Pons2,3, José A. Jurado‑Rivera1, Damià Jaume2 & Carlos Juan1,2* Species diversifcation in ancient lakes has enabled essential insights into evolutionary theory as they embody an evolutionary microcosm compared to continental terrestrial habitats. We have studied the high‑altitude amphipods of the Andes Altiplano using mitogenomic, nuclear ribosomal and single‑ copy nuclear gene sequences obtained from 36 Hyalella genomic libraries, focusing on species of the Lake Titicaca and other water bodies of the Altiplano northern plateau. Results show that early Miocene South American lineages have recently (late Pliocene or early Pleistocene) diversifed in the Andes with a striking morphological convergence among lineages. This pattern is consistent with the ecological opportunities (access to unoccupied resources, initial relaxed selection on ecologically‑ signifcant traits and low competition) ofered by the lacustrine habitats established after the Andean uplift. Lakes with an uninterrupted history of more than 100,000 years (ancient lakes) may be considered as natural laboratories for evolutionary research as they constitute hotspots of aquatic animal speciation and phenotypic diversity1. Changes in lake size and episodes of desiccation are considered to be critical factors in the speciation and extinction of lake faunas, with the creation of new habitats afer lake expansions as the primary driver of intra-lake diversifcation2–4. For instance, cichlid radiations in the East African Lakes seem to have been trig- gered by lake expansions afer periods of intense desiccation, with the surviving species flling up empty niches afer lake reflling2. -
Lake Titicaca
Lake Basin Management Initiative Experience and Lessons Learned Brief Lake Titicaca Mario Francisco Revollo Vargas* Maximo Liberman Cruz Alberto Lescano Rivero 1. Description Drought and floods are the natural hazards that have the greatest environmental, social and eco- nomic impact on the Bolivian-Peruvian high plateau (altiplano) which includes the hydrological basin of Lake Titicaca, the Desaguadero River, Lake Poopo and the Salt Lake of Coipasa, collec- tively designated by the acronym TDPS. Through good management, the system can be regulated in benefit of the people who live in the region. Territorial Scope The project area (Figure 1) includes the hydrological basins of Lake Titicaca, the Desaguadero River, and lakes Poopo and Salar de Coipasa (TDPS system). The TDPS system is located in parts of Peru, Bolivia and Chile, spread between latitude 14° 03' to 20° 00' South and between longitude 66° 21' to 71° 07' West. The total area of the system is 143,900 km2 and includes the sub-region Puno in Peru and the departments of La Paz and Oruro in Bolivia. The basins included in the TDPS system have the following characteristics: Lake Titicaca This paper was presented at the Lake Basin Management Initiative 2 Regional Workshop for Europe, Central Asia and the Americas catchment area: 56,270 km 2 held at Saint Michaelʼs College in Vermont, USA, 18-21 June - average lake area: 8,400 km 2003. The workshop was organized by LakeNet in cooperation with SMC and the International Lake Environment Committee medium altitude: 3,810 m above sea level 3 with funding from the Global Environment Facility, U.S. -
Puntos De Recaudo Pagoefectivo En Agentes Kasnet - Provincia
Puntos de Recaudo PagoEfectivo en Agentes Kasnet - Provincia Departamento Provincia Distrito Localidad Nombre del Comercio Dirección Referencia AMAZONAS BAGUA COPALLIN COPALLIN BOTICA JC FARMA FRANCISCO BOLOGNESI 533 MEDIA CUADRA DEL MERCADO AMAZONAS BAGUA LA PECA BAGUA BAZAR LOCUTORIO ANGELICA JR. COMERCIO 524 FRENTE A PARQUE PRINCIPAL AMAZONAS BAGUA LA PECA BAGUA BOTICA SANIDAD J&S JR. RODRIGUEZ DE MENDOZA 442 ENTRE LA PLAZA PRINCIPAL Y EL BANCO DE LA NACION AMAZONAS BAGUA LA PECA LA PECA TELECOMUNICACIONES LURVI JR. LIMA PT. INT. 3 MERCADO LA PARADA AMAZONAS BONGARA FLORIDA FLORIDA MULTISERVICIOS J & G AV. MARGINAL S/N CD 2 FRENTE A CAJA PIURA Y A DOS CUADRAS DE COMISARIA AMAZONAS CHACHAPOYAS CHACHAPOYAS CHACHAPOYAS COSELVI JR. SALAMANCA 900 A CUADRA Y MEDIA DE LA PLAZA DE ARMAS AMAZONAS UTCUBAMBA BAGUA GRANDE BAGUA GRANDE LOCUTORIO MOVITEL PARADA MUNICIPAL PUESTO 14 FRENTE A FERRETERIA CHAVEZ AV MARIANO MELGAR AMAZONAS UTCUBAMBA BAGUA GRANDE BAGUA GRANDE MOTO REPUESTOS MENDOZA AV. CHACHAPOYAS N. 1688 FRENTE A LA UGEL BAGUA GRANDE AMAZONAS UTCUBAMBA BAGUA GRANDE BAGUA GRANDE TELECOMUNICACIONES & SERVICIOS SFA AV. CHACHAPOYAS 2294 COST. COOP. CRISTO DE BAGAZAN ANCASH CARHUAZ CARHUAZ CARHUAZ MULTISERTEL G Y M AV. PROGRESO 684 ESQUINA PLAZA DE ARMAS ANCASH CASMA CASMA CASMA JAVELI OFFICE SCHOOL AV. NEPEÑA MZ. B LT. 1 FRENTE AL BANCO DE LA NACION ANCASH HUARAZ HUARAZ HUARAZ COMPEX PERU AV. FITZCARRAL 304 ESQUINA CON JR. CARAZ ANCASH HUARAZ HUARAZ HUARAZ COMPUNET JR. JUAN DE LA CRUZ ROMERO 451 FRENTE AL MERCADO CENTRAL ANCASH HUARAZ HUARAZ HUARAZ ENKANTOS BOUTIQUE JR JULIAN DE MORALES 709 FRENTE A LA FACULTAD DE MINAS ANCASH HUARAZ HUARAZ HUARAZ IMPORTACIONES TINA JR JOSE DE SAN MARTIN 571 A MEDIA CUADRA DEL PARQUEO ANCASH HUARAZ HUARAZ HUARAZ INVERSIONES DENNYS JR. -
LOCATION: Central Pacific Coast of South America
PERU *LOCATION: Central Pacific coast of South America. *GEOGRAPHY With 1,285,215 square km. Peru is the third-largest country in South America after Brazil and Argentina, ranking it amongst the world's 20 largest nations. Peru is divided into three regions: coast, mountains and jungle; also holds sway over the sea up to 200 miles from the coast and has territorial rights to an area of 60 million hectares in the Antarctic. It´s divided into 24 departments, being Lima the capital of the country. *POPULATION 29, 798, 000. *OFFICIAL LANGUAGE Spanish. Also English, French, spoken in most hotels and restaurants *TIME ZONE 5 hours behind the Greenwich Meridian Time (-5 GMT). *ELECTRICITY 220 V, 60Hz. It is recommendable to carry an adaptor for flat plugs. *CURRENCY The official currency in Peru is the Nuevo Sol (S/.), which is divided into 100 centimos. The currency includes coins for 5, 10, 20 and 50 centimos and 1, 2 and 5 sol coins. There are bills in the denomination of 10, 20, 50, 100 and 200 Nuevos Soles. *EXCHANGE RATE US$ to S/. 3.40 aprox € to S/. 3.80 *WEATHER IN LIMA °C: 22 – 18. °F 72 – 66. No precipitations. *PHONES AND COMMUNICATION Country area code: +51. Lima area code: 01. Peru features a far-reaching telephone network that provides services for national and international long-distance calls from private telephone lines and public cabins. There are also currently 1.3 million clients who have cellular phones, and satellite communications are currently being developed. *AIRPORTS Lima is 14 airports equipped to receive commercial flights and 10 ready for international flights: Lima, Arequipa, Chiclayo, Pisco, Pucallpa, Iquitos, Cusco, Trujillo, Tacna and Juliaca.17 airlines operating international flights and 7 airline companies, offering domestic flights *LOCAL TRANSPORTATION Use of public transportation, such as taxis or buses is common in Peru. -
CALLAO, PERU Onboard: 1800 Saturday November 26
Arrive: 0800 Tuesday November 22 CALLAO, PERU Onboard: 1800 Saturday November 26 Brief Overview: A traveler’s paradise, the warm arms of Peru envelope some of the world’s most timeless traditions and greatest ancient treasures! From its immense biodiversity, the breathtaking beauty of the Andes Mountains (the longest in the world!) and the Sacred Valley, to relics of the Incan Empire, like Machu Picchu, and the rich cultural diversity that populates the country today – Peru has an experience for everyone. Located in the Lima Metropolitan Area, the port of Callao is just a stone’s throw away from the dazzling sights and sounds of Peru’s capital and largest city, Lima. With its colorful buildings teeming with colonial architecture and verdant coastline cliffs, this vibrant city makes for a home-away-from-home during your port stay in Peru. Nearby: Explore Lima’s most iconic neighborhoods - Miraflores and Barranco – by foot, bike (PER 104-201 Biking Lima), and even Segway (PER 121-101 Lima by Segway). Be sure to hit up one of the local markets (PER 114-201 Culinary Lima) and try out Peruvian fare – you can’t go wrong with picarones (fried pumpkin dough with anis seeds and honey - pictured above), cuy (guinea pig), or huge ears of roast corn! Worth the travel: Cusco, the former capital of Incan civilization, is a short flight from Lima. From this ancient city, you can access a multitude of Andean wonders. Explore the ruins of the famed Machu Picchu, the city of Ollantaytambo – which still thrives to this day, Lake Titcaca and its many islands, and the culture of the Quechua people. -
Aduana De Destino Descripción De La Ruta Plazo (Horas)
ANEXO 5 DESPA-PG.27: CODIGOS DE RUTA Y PLAZOS PARA EL TRÁNSITO ADUANERO INTERNACIONAL DE MERCANCÍAS Plazo Código de Ruta Aduana de Partida - Aduana de Destino Descripción de la Ruta (horas) 019-019-A Tumbes - Tumbes TUMBES - TUMBES 2 019-028-A Tumbes - Talara TUMBES - TALARA 10 019-046-A Tumbes - Paita TUMBES - SULLANA - PIURA - PAITA 14 019-055-A Tumbes - Chiclayo TUMBES - SULLANA - PIURA - CHICLAYO 27 019-082-A Tumbes - Salaverry TUMBES - SULLANA - PIURA - CHICLAYO - TRUJILLO - SALAVERRY 37 019-091-A Tumbes - Chimbote TUMBES - SULLANA - PIURA - CHICLAYO - TRUJILLO - CHIMBOTE 40 019-118-A Tumbes - Marítima Callao TUMBES - SULLANA - PIURA - CHICLAYO - TRUJILLO - CHIMBOTE - MARITIMA CALLAO 64 019-127-A Tumbes - Pisco TUMBES - SULLANA - PIURA - CHICLAYO - TRUJILLO - CHIMBOTE - LIMA CALLAO - PISCO 80 TUMBES - SULLANA - PIURA - CHICLAYO - TRUJILLO - CHIMBOTE - LIMA CALLAO - PISCO - ICA - 019-145-A Tumbes - Mollendo/Matarani 125 CAMANA - REPARTICIÓN -MOLLENDO/MATARANI TUMBES - SULLANA - PIURA - CHICLAYO - TRUJILLO - CHIMBOTE - LIMA CALLAO - PISCO - ICA - 019-154-A Tumbes - Arequipa 124 CAMANA - REPARTICIÓN - AREQUIPA TUMBES - SULLANA - PIURA - CHICLAYO - TRUJILLO - CHIMBOTE - LIMA CALLAO - PISCO - ICA - 019-163-A Tumbes - Ilo 134 CAMANA - REPARTICIÓN - MOQUEGUA - ILO TUMBES - SULLANA - PIURA - CHICLAYO - TRUJILLO - CHIMBOTE - LIMA CALLAO - PISCO - ICA - 019-172-A Tumbes - Tacna 136 CAMANA - REPARTICION - MOQUEGUA -TACNA TUMBES - SULLANA - PIURA - CHICLAYO - TRUJILLO - CHIMBOTE - LIMA CALLAO - PISCO - ICA - 019-181-A Tumbes - Puno 145 CAMANA -
Lake Titicaca
III. PALEOHYDROLOGY IIL1. A 20,000 years paleohydrological record from Lake Titicaca DENIS WIRRMANN, JEAN-PIERRE YBERT and PHILIPPE MOURGUIART The Bolivian Altiplano is an endorheic basin which extends from 16° to 20° S. Lat. and from 65° to 69°W. Long., with altitudes ranging from 3700 to 4600 metres, covering 200,000 km2 between the Western and Eastern Cordilleras which are 6500 m high (Fig. 1). From north to south, three major lacustrine areas occupy this high plateau: 2 - Lake Titicaca at 3809 metres above sea level, covering 8562 km ; 2 - Lake Poopo at 3686 m.a.s.l. covering 2530 km ; - Coipasa-Uyuni, a group of dry salt lakes, covering 11 ,000 km2 at 3653 m.a.s.l. Over the last 1.8 million years these basins have registered episodes of greatly enlarged lake areas. According to Lavenu et al. (1984) and to Servant and Fontes (1978, 1984), the Pleistocene record of Titicaca lake level fluctu ations can be summarised as follows: - during the Early Pleistocene the paleolake Mataro rose with a water level established at 140 metres above the present level. This stage is related to the end of the Calvario glaciation (Servant, 1977) and the corresponding deposits are recognisable mainly at the NW edge of the basin; - the paleolake Cabana occurred during the middle Pleistocene with a water level established at 90 metres above the present Lake Titicaca level: the associated sediments are present on the eastern and western shores of the basin; - then with the retreat of the Sorata glaciation (Servant, 1977) the Ballivian stage occurred with