Clea Developme T Mecha Ism Project Desig

Total Page:16

File Type:pdf, Size:1020Kb

Clea Developme T Mecha Ism Project Desig PROJECT DESIGN DOCUMENT FORM (CDM PDD) - Version 03.1. CDM – Executive Board page 1 CLEA DEVELOPMET MECHAISM PROJECT DESIG DOCUMET FORM (CDM-PDD) Version 03 - in effect as of: 28 July 2006 COTETS A. General description of project activity B. Application of a baseline and monitoring methodology C. Duration of the project activity / crediting period D. Environmental impacts E. Stakeholders’ comments Annexes Annex 1: Contact information on participants in the project activity Annex 2: Information regarding public funding Annex 3: Baseline information Annex 4: Monitoring plan Annex 5: CEMPPSA´s newspaper article Annex 6: Photographs of project PROJECT DESIGN DOCUMENT FORM (CDM PDD) - Version 03.1. CDM – Executive Board page 2 SECTIO A. General description of project activity A.1 Title of the project activity : Exploitation of the Mendoza River, Potrerillos Project (Original title: Aprovechamiento Integral del río Mendoza, Proyecto Potrerillos) – Hydroelectric Power - Argentina. Version 01 April 2007 A.2. Description of the project activity: The objective of this Project is the generation of renewable electric power at the Álvarez Condarco and Cacheuta Nueva Hydroelectric Power Stations, located in the Province of Mendoza, Argentine Republic. The reduction of CO 2 emissions is achieved through the displacement of electricity generated from fossil fuel by electricity generated from renewable sources. Thus, it is estimated that the annual average of emission reduction will be of 221,998.53 tons of equivalent CO 2 during a crediting period of 7 renewable years (21 altogether). The Potrerillos Exploitation Project was carried out by CEMPPSA (Consortium of Mendocinian Companies for Potrerillos Business Corporation). The Project uses the water flow of the Mendoza River with the following purposes: • To enlarge and normalize the irrigated area; • To control flood events in the Mendoza River; • To satisfy the requirements of potable water and water for agriculture and industrial use in the Mendoza suburban area and its influence area; • To increase the production of electric power in the province. CEMPPSA was granted the concession of the old power stations Álvarez Condarco and Cacheuta and it has undertaken the construction of the Potrerillos Dam and the Cacheuta Nueva Power Station. Moreover, two existing machines from the Álvarez Condarco Station were repowered and a third machine was incorporated, as explained below: − To the effects of this CDM project activity, the Cacheuta Nueva Power Station has been built. The station has a Maximum Installed Generation Capacity of 126.40 MW, and is made up of four (4) generation units of 31.60 MW each. This station has replaced the old Cacheuta Station, which had a maximum installed capacity of 9 MW and three (3) generators of 3 MW each of which had been working since the year 1926. − Also, as part of the CDM Project, two existing equipment units of 13.7 MW have been repowered at the Álvarez Condarco Station, which now have 15.20 MW, and a new generator has been incorporated of 24.54 MW. Both stations are located in a cascade design and are fed by their own adduction, which originates at the Potrerillos Dam. During the period between May 2002 and October 2003, the units at both stations gradually began operating commercially. However, this Project does not claim retroactiveness for the years of operation before 2007. PROJECT DESIGN DOCUMENT FORM (CDM PDD) - Version 03.1. CDM – Executive Board page 3 With the registration of the Project in the CDM, CEMPPSA plans to implement an aid fund for state technical schools in the province of Mendoza. The funding necessary to carry out said activity will be secured from the sale of carbon credits obtained by this Project, by means of a trust fund created for this purpose. This will be an important contribution by the Project to the region´s sustainable development, apart from the contributions inherent to the Project which are set forth below: • The increase of the clean energy rate in the Argentine Interconnection System (SADI), by displacing sources of intensive carbon generation, and covering approximately 25% of the electric power consumption of the Province. • Expansion and improvement of the water supply for the irrigated oasis, which will favor the necessary conditions for the sustained growth of Mendoza´s economy. • The assurance of a potable water supply for the population of the Mendoza River oasis , control of its flow volume and reduction of the risk caused by its periodic overflooding. • A substantial boost to local and foreign tourism, through the existence of a permanent water mirror, attractive to both effective and sedentary tourists, which will represent an important source of indirect employment and a growth factor for the whole province. In fact, during the construction stage, 1,200 people have benefited from direct employment. A.3. Project participants : ame of Party involved (*) Private and/or public Kindly indicate if ((host) indicates a host Party) entity(ies) the Party involved project participants (*) wishes to be (as applicable) considered as project participant (Yes/o) Argentina (Host) CEMPPSA ( Consortium of o Mendocinian Companies for Potrerillos Business Corporation ) (*) In accordance with the CDM modalities and procedures, at the time of making the CDM-PDD public at the stage of validation, a Party involved may or may not have provided its approval. At the time of requesting registration, the approval by the Party(ies) involved is required. PROJECT DESIGN DOCUMENT FORM (CDM PDD) - Version 03.1. CDM – Executive Board page 4 A.4. Technical description of the project activity : A.4.1. Location of the project activity : A.4.1.1. Host Party (ies): Argentine Republic A.4.1.2. Region/State/Province etc.: Province of Mendoza A.4.1.3. City/Town/Community etc: Departments of Las Heras and Luján de Cuyo. A.4.1.4. Detail of physical location, including information allowing the unique identification of this project activity (maximum one page): The Potrerillos Exploitation Project is located on the Mendoza River, in the Province of the same name, in the Cuyo region of the Republic of Argentina (mid-west). Mendoza is bounded by the province of San Juan to the north, by the provinces of San Luis and La Pampa to the east, by the provinces of La Pampa and Neuquén to the south and finally by the Republic of Chile to the west. The Potrerillos Dam is situated on the Mendoza River, at 33° 01´ south latitude and 69° 06´ west longitude, at 1,300 m.a.s.l. in the area near the village of Cacheuta and downstream from the village of Potrerillos. The Project area has access from Provincial Route N° 82. The distance from the city of Mendoza is 35 km from Cacheuta and 46 km from Potrerillos. In the Project area, the Mendoza River –which is part of the Desaguadero Basin- constitutes the boundary between the departments of Luján de Cuyo and Las Heras, the former extending from the right margin of the River while the latter from the left margin. The Cacheuta Nueva Station is specifically located at geographic coordinates X: 6.346.375 and Y: 2.489.575, while the Álvarez Condarco Station is located at coordinates X: 6.344.300 and Y: 2.495.200, both on the margins of the Mendoza River. The department of Luján de Cuyo has a surface of 4,847 km 2 and a population of approximately 70,000 inhabitants; while the department of Las Heras has 8,955 km 2 and 130,000 inhabitants. PROJECT DESIGN DOCUMENT FORM (CDM PDD) - Version 03.1. CDM – Executive Board page 5 South America Mendoza/Argentina Area of the Project activity Map References : Río Mendoza: Mendoza River Vertedero: Spillway (Morning Glory type, Río Blanco: Blanco River Design flood 1800 m 3/sec) Río Seco Cacheuta: Cacheuta Dry River Túnel de aducción: Adduction Tunnel Zona Curva del icho: Curva del icho Area Central Cacheuta: Cacheuta Power Station Túnel de riego, desvío y descargador de fondo: Central Álvarez Condarco: Álvarez Condarco Irrigation, Diversion and Bottom Discharge Power Station Tunnel (350 m of length, 10.80 m in diameter) Sub-Estación Luján de Cuyo: Luján de Cuyo Presa Potrerillos: Potrerillos Dam Substation PROJECT DESIGN DOCUMENT FORM (CDM PDD) - Version 03.1. CDM – Executive Board page 6 A.4.2. Category(ies) of project activity : According to the Categories and Scope of the CDM projects defined by the UNFCCC, this project activity belongs to Category 1: Renewable Energy (Scope umber: 1 - Sectorial Scope: Energy industries (renewable - / non-renewable sources)). A.4.3. Technology to be employed by the project activity : The basic operating principle by which the technology used allows the generation of electricity consists of exploiting the potential energy of the water collected in the dam, situated at a higher level than the power station, where the hydraulic turbines and generators are placed. The water gets there carried through a discharge or adduction pipeline. The Potrerillos dam consists essentially of a main body of triangular shape made of loose rockfill, not earthfill, strongly compacted and with a high draining capacity, and of a thin layer of concrete in the upstream face to provide impermeability. This type of dam is also commonly called CFRD (Concrete Faced Rockfill Dam). It is situated at around 3.5 km upstream from the village of Cacheuta, where the riverbed reaches around 1,272 m.a.s.l. Its maximum height from the foundation is 116 m, its length at the crest is 480 m, and its width is 395 m wide at the base. The dam thus formed floods a maximum surface of 1,300 Ha and creates a useful volume of 310 hm 3. The dam has a Morning Glory-type spillway with a tunnel that is 300 m long and 11.8 m in diameter.
Recommended publications
  • Debris Flows Occurrence in the Semiarid Central Andes Under Climate Change Scenario
    geosciences Review Debris Flows Occurrence in the Semiarid Central Andes under Climate Change Scenario Stella M. Moreiras 1,2,* , Sergio A. Sepúlveda 3,4 , Mariana Correas-González 1 , Carolina Lauro 1 , Iván Vergara 5, Pilar Jeanneret 1, Sebastián Junquera-Torrado 1 , Jaime G. Cuevas 6, Antonio Maldonado 6,7, José L. Antinao 8 and Marisol Lara 3 1 Instituto Argentino de Nivología, Glaciología & Ciencias Ambientales, CONICET, Mendoza M5500, Argentina; [email protected] (M.C.-G.); [email protected] (C.L.); [email protected] (P.J.); [email protected] (S.J.-T.) 2 Catedra de Edafología, Facultad de Ciencias Agrarias, Universidad Nacional de Cuyo, Mendoza M5528AHB, Argentina 3 Departamento de Geología, Facultad de Ciencias Físicas y Matemáticas, Universidad de Chile, Santiago 8320000, Chile; [email protected] (S.A.S.); [email protected] (M.L.) 4 Instituto de Ciencias de la Ingeniería, Universidad de O0Higgins, Rancagua 2820000, Chile 5 Grupo de Estudios Ambientales–IPATEC, San Carlos de Bariloche 8400, Argentina; [email protected] 6 Centro de Estudios Avanzados en Zonas Áridas (CEAZA), Universidad de La Serena, Coquimbo 1780000, Chile; [email protected] (J.G.C.); [email protected] (A.M.) 7 Departamento de Biología Marina, Universidad Católica del Norte, Larrondo 1281, Coquimbo 1780000, Chile 8 Indiana Geological and Water Survey, Indiana University, Bloomington, IN 47404, USA; [email protected] * Correspondence: [email protected]; Tel.: +54-26-1524-4256 Citation: Moreiras, S.M.; Sepúlveda, Abstract: This review paper compiles research related to debris flows and hyperconcentrated flows S.A.; Correas-González, M.; Lauro, C.; in the central Andes (30◦–33◦ S), updating the knowledge of these phenomena in this semiarid region.
    [Show full text]
  • Where Does the Chilean Aconcagua River Come From? Use of Natural Tracers for Water Genesis Characterization in Glacial and Periglacial Environments
    water Article Where Does the Chilean Aconcagua River Come from? Use of Natural Tracers for Water Genesis Characterization in Glacial and Periglacial Environments Sebastián Andrés Crespo 1,* ,Céline Lavergne 2,3 , Francisco Fernandoy 4 , Ariel A. Muñoz 1, Leandro Cara 5 and Simón Olfos-Vargas 1 1 Instituto de Geografía, Facultad de Ciencias del Mar y Geografía, Pontificia Universidad Católica de Valparaíso, Valparaíso 2362807, Chile; [email protected] (A.A.M.); [email protected] (S.O.-V.) 2 Laboratory of Aquatic Environmental Research, Centro de Estudios Avanzados, Universidad de Playa Ancha, Viña del Mar 2581782, Chile; [email protected] 3 HUB Ambiental UPLA, Universidad de Playa Ancha, Valparaíso 234000, Chile 4 Laboratorio de Análisis Isotópico (LAI), Facultad de Ingeniería, Universidad Andrés Bello, Viña del Mar 2531015, Chile; [email protected] 5 Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales (IANIGLA-CONICET), Mendoza 5500, Argentina; [email protected] * Correspondence: [email protected] Received: 1 August 2020; Accepted: 12 September 2020; Published: 21 September 2020 Abstract: The Aconcagua river basin (Chile, 32 ◦S) has suffered the effects of the megadrought over the last decade. The severe snowfall deficiency drastically modified the water supply to the catchment headwaters. Despite the recognized snowmelt contribution to the basin, an unknown streamflow buffering effect is produced by glacial, periglacial and groundwater inputs, especially in dry periods. Hence, each type of water source was characterized and quantified for each season, through the combination of stable isotope and ionic analyses as natural water tracers. The δ18O and electric conductivity were identified as the key parameters for the differentiation of each water source.
    [Show full text]
  • Snowmelt Mathematical Simulation with Different Climatic Scenarios in the Tupungato River Basin, Mendoza, Argentina
    126 Remote Sensing and Hydrology 2000 (Proceedings of a symposium held at Santa Fe, New Mexico, USA, April 2000). IAHS Publ. no. 267, 2001. Snowmelt mathematical simulation with different climatic scenarios in the Tupungato River basin, Mendoza, Argentina JORGE MAZA INA Centra Regional Andino, Belgrano (oeste), 210-5500 Mendoza, Argentina e-mail: [email protected] FEDERICO CAZORZI Dipartamenlo Territorio e Sistemi Agro-Forestali, University of Padova, Via Romea, 1-35020 Legnaro, Padova, Italy PATRICIA LOPEZ, LUIS FORNERO, ADRIAN VARGAS & JOSE ZULUAGA INA Centro Regional Andino, Belgrano (oeste), 210-5500 Mendoza, Argentina Abstract The impact of climate change on water resource availability in the Mendoza River oasis, Argentina where 1 000 000 inhabitants live and 80 000 ha of crops are irrigated was assessed. The snow coverage depletion curve was obtained from the NEVE model using Landsat-TM images for calibration. The possible evidence of climate change and its severity was analysed. The results obtained from the SRM model showed an important peak flow and runoff volume variation. Key words Argentina; climate change; NEVE model; snowmelt; SRM model INTRODUCTION The area under study is the Tupungato River basin (1858 km2, and 4251 m a.m.s.l. average elevation), a tributary of the Mendoza River in Argentina, located at 70° W and 33°S. The major source of streamflow is snowmelt that takes place between September and February with a negligible precipitation contribution. The objective of this study was to assess the influence of climatic change on the snowmelt-runoff process. METHOD NEVE (CaZorzi & Dalla Fontana, 1996) is a morpho-energetic model of apparent sun motion with a very simple distributed snowmelt rate algorithm.
    [Show full text]
  • Seasonal Variation of the Mountain Phytoplankton In
    Seasonal Variation of the Mountain Phytoplankton in the Arid Mendoza Basin, Westcentral Argentina Patricia Peralta Instituto Argentino de NillOlogia Glaciologfa y Cienciss Ambientales (IAN/GLA)- CRICYT Av. Ruiz Leal shI, C.C. 330 5500 Mendoza, Argentina (pperal/a@/ab.cricyt.edu.er) and Cristina Claps instituto de Limnologla "Dr. R. Ringuelef' All. Calchaqui km 23,5 1888 FIorencio Varela, Argentina ([email protected]) ABSTRACT We anaJyzed the seasonal composition of phytoplankton from the Mendoza River and its rnoutaries from the High Cordillera to the plain in centralwest Acgenlina. A total of 72 algae species were identified; among them, 36 species were diatoms, 17 chlorophytes. 15 cyanophytes, three cuglenophytes and one pyrrophyte . A marked seasooaliry was observed. Diatoms were dominant in all seasons at most of the sampling sites. with abundance peaks in autumn and winter. Cyanophytes were found throughout the year but with highest numbers in summer and spring. Chlorophytes were well represented throughout the year except in winter. The pyrropbytes were represented by Poidinium gatunensis. which was recorded exclusively in the spring along with the chlorophyte Sraurast1Um s~ba/dii at most of the sampling sites. Eugienophytes were found only in the lower basin and with maximum richness and density in autumn. Most of the diatoms were benthic. Nitzschia paka. Eugl~ruJ proxima and E. oxyUtuS were limited to ce rtain sectors of the river that receive sewage discharge. The remainder of the river is generally free from significant anthropogenic impact. INrRODucnON The Me ndoza Rjver in cenlralwest Argentina is fonned by tributaries that arc fed largely from snowmelt and from the glaciers of the Cordillera de Los Andes.
    [Show full text]
  • Temporal and Altitudinal Variations in Benthic Macroinvertebrate Assemblages in an Andean River Basin of Argentina
    J. Limnol., 2014; 73(1): 92-108 ORIGINAL ARTICLE DOI: 10.4081/jlimnol.2014.789 Temporal and altitudinal variations in benthic macroinvertebrate assemblages in an Andean river basin of Argentina Erica E. SCHEIBLER,1* M. Cristina CLAPS,2 Sergio A. ROIG-JUÑENT1 1Laboratorio de Entomología, IADIZA, CCT CONICET Mendoza. Avda. Ruiz Leal s/n. Parque Gral. San Martín, CC 507, 5500 Mendoza; 2ILPLA, CCT CONICET La Plata, Boulevard 120 e/62 y 63, 1900 La Plata, Argentina *Corresponding author: [email protected] ABSTRACT Environmental variables and benthic macroinvertebrate assemblages were spatially and seasonally examined over two con- secutive years (2000-2002) along a glacier and snowmelt river in the central-west of Argentina where lies the highest peak in America, Mount Aconcagua (6956 m elevation). The goal was to assess seasonal and altitudinal variability in benthic community structure and to define whether physical-chemical variables affect distribution of aquatic insects. The Mendoza River basin was characterised by high variability in flow and transparency, high conductivity, hard calcium sulphate water, neutral and alkaline pH, and dominant sub- strate composed of small blocks, cobbles, pebbles, and sand-silt. Richness of invertebrates was low, with the lowest taxonomic richness being recorded at the mouth. The dominant group with highest taxonomic richness was Diptera, althoughonly caddisflies, mayflies, beetles, and stoneflies were present. Seasonal and spatial variations in biotic and abiotic variables were detected. Maximal densities and tax- onomic richness were recorded in autumn and winter. From Modified Morisita’s Cluster analysis it was found that the system is divided into two groupings of sites related to each other by faunal composition.
    [Show full text]
  • Interactive Comment on “Mountain Water Cellars: a Chemical
    Hydrol. Earth Syst. Sci. Discuss., https://doi.org/10.5194/hess-2018-212-AC2, 2018 HESSD © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Interactive comment Interactive comment on “Mountain water cellars: a chemical characterization and quantification of the hydrological processes and contributions from snow, glaciers and groundwater to the Upper Mendoza River basin (∼ 32◦ S), Argentina” by Sebastián A. Crespo et al. Sebastián A. Crespo et al. [email protected] Received and published: 6 October 2018 Responses to Referee 1, identified as follows: (1) comments from Referee, (2) author’s response, (3) author’s changes in manuscript. Printer-friendly version Answer to Referee, comment 1. Discussion paper (1) An English proofreading must be performed for the manuscript, also including the C1 figure captures. It is out of scope of this review to address the frequent grammatical deficits or the necessity to rephrase sentences (e.g. “Cuevas, Vacas and Tupungato HESSD rivers when join in Punta de Vacas, form the Mendoza River.” (P22L7-8) should be “Cuevas, Vacas and Tupungato rivers form the Mendoza River in Punta de Vacas”. It is unclear, what “The logo of Copernicus Publications” means in this figure capture.). Interactive There are many examples which could be provided here. comment (2) We agree. The entire manuscript is being reviewed and corrected by a technical reviewer and native English speaker. (3) New Figure 1 and caption added. The figure captions were streamlined and the specific indication (P22L7-8) was framed by the legend, becoming no longer necessary in the figure caption.
    [Show full text]
  • Multi-Isotopic and Morphometric Evidence for the Migration Of
    www.nature.com/scientificreports OPEN Multi‑isotopic and morphometric evidence for the migration of farmers leading up to the Inka conquest of the southern Andes Ramiro Barberena1,2*, Lumila Menéndez3,4*, Petrus J. le Roux5, Erik J. Marsh1,2, Augusto Tessone6, Paula Novellino7, Gustavo Lucero8, Julie Luyt9, Judith Sealy9, Marcelo Cardillo10, Alejandra Gasco1,2, Carina Llano1,11, Cecilia Frigolé1,2, Daniela Guevara7, Gabriela Da Peña7, Diego Winocur12, Anahí Benítez12, Luis Cornejo13, Fernanda Falabella14, César Méndez15, Amalia Nuevo‑Delaunay15, Lorena Sanhueza14, Francisca Santana Sagredo16, Andrés Troncoso14, Sol Zárate1, Víctor A. Durán1,2 & Valeria Cortegoso1,2 We present isotopic and morphometric evidence suggesting the migration of farmers in the southern Andes in the period AD 1270–1420, leading up to the Inka conquest occurring ~ AD 1400. This is based on the interdisciplinary study of human remains from archaeological cemeteries in the Andean Uspallata Valley (Argentina), located in the southern frontier of the Inka Empire. The studied samples span AD 800–1500, encompassing the highly dynamic Late Intermediate Period and culminating with the imperial expansion. Our research combines a macro‑regional study of human paleomobility and migration based on a new strontium isoscape across the Andes that allows identifying locals and migrants, a geometric morphometric analysis of cranio‑facial morphology suggesting separate ancestral lineages, and a paleodietary reconstruction based on stable isotopes showing that the migrants had diets exceptionally high in C4 plants and largely based on maize agriculture. Signifcantly, this migration infux occurred during a period of regional demographic increase and would have been part of a widespread period of change in settlement patterns and population movements that preceded the Inka expansion.
    [Show full text]
  • Impact of Hydraulic Structures and Water Use on Solids in Water in the Andean Argentinian Piedmont: Case Studies of Tunuyan and Mendoza River Valleys
    Geogr. Fis. Dinam. Quat. DOI 10.4461/GFDQ.2013.36.9 36 (2013), 119-130, 8 figg. ÉMILIE LAVIE (*), RICHARD LAGANIER (*), JOSÉ ANTONIO MORÁBITO (**) (***), SANTA ESMERALDA SALATINO (**), ROSA MEDINA DE DIAS (***), SUSANA MIRALLES (***) & ROCIO HERNÁNDEZ (**) IMPACT OF HYDRAULIC STRUCTURES AND WATER USE ON SOLIDS IN WATER IN THE ANDEAN ARGENTINIAN PIEDMONT: CASE STUDIES OF TUNUYAN AND MENDOZA RIVER VALLEYS ABSTRACT: LAVIE É., LAGANIER R., MORÁBITO J.A., SALATINO S.E., INTRODUCTION MEDINA DE DIAS R., MIRALLES S. & HERNÁNDEZ R., Impact of hydraulic structures and water use on solids in water in the Andean Argentinian piedmont: case studies of Tunuyán and Mendoza river valleys. (IT ISSN The Cuyo, a wide depression of the Argentinian An- 0391-9838, 2013). dean piedmont, contains half-a-dozen oases characterised The province of Mendoza has a tradition of irrigation inherited from by urban (cities of Mendoza and San Juan; fig. 1), industrial the Incas, from pre-Columbian times. It contains 36,000 ha irrigated and (oil zones of Malargüe and Mendoza), and mostly agricul- distributed in oases located on the banks of snow-glacial water-regime tural uses. Most of the oases are organised into specialised rivers from the Andes Mountains. After several years of monitoring the areas, each containing a horticultural sector, fruit and olive quality of irrigation water in two of the largest basins (Mendoza and Tunu- yán rivers; latitude 32°30’S, 33º50’S and longitude 67°50’W, 69°30’W, trees, and vineyards. They are all located in semi-arid to respectively), this survey seeks to evaluate the quantitative and qualitative arid lands and have been developed by the diversion of the variations of dissolved (TDS) and suspended (TSS) solids in water flows.
    [Show full text]
  • Trip to Mendoza
    TRAVEL MART - Trip to Mendoza Journey to Buenos Aires & Mendoza 4 Days South American Tours Argentina 3 De Febrero 2823, 6° Floor, Buenos Aires, Argentina Phone: ++54 11 4780 1037, [email protected] Jun 05, 2018 QUOTE CLIENT / TRAVEL MART - Trip to Mendoza Page 2 - File: 15438 Argentina – The name Argentina comes from the Latin word “argentum” (silver) and has been used since the first so called “Conquistador” (Conqueror) from Spain came to the “Rio de la Plata” (silver river). The country has 40 million inhabitants, many Spanish, Italians, Germans and French immigrated to Argentina, being the most European influenced country of the subcontinent. Argentina is a fascinating land of contrasts and of unspoiled nature along its 3.694km (2.295mi.) from north to south and 1.423km (885mi.) from east to west. You can find impressive waterfalls, appealing landscapes, delicious wines, peaceful lakes, breath-taking glaciers, the world´s southernmost city also known as “the end of the world” as well as abundant wildlife. Buenos Aires, the capital city, is one of the most elegant and busiest cities of South America. Day 01 - Saturday, September 22, 2018 Arrival in Buenos Aires-Mendoza Optional: Transfer Hotel - Domestic Airport Flight Buenos Aires / Mendoza (not included) Transfer Airport - Hotel Optional: Transfer from your Hotel to Aeroparque Domestic Airport At the given time, you will be picked up and taken to the Domestic Airport to board your flight to Mendoza. Mendoza - the province counts with rivers, valleys, canyons, and the imposing Andean range, with the highest peak in the Western Hemisphere, the Aconcagua Mountain with 6.959m (22.831ft.) Mendoza is a green city in a kind of dessert.
    [Show full text]
  • Impacto De La Obra Presa Potrerillos En Los Habitantes De La Villa Y Su Entorno Inmediato 1
    Año 2- Vol 1- Número 2 - ISSN 1852 - 0006 Impacto de la obra Presa Potrerillos en los habitantes de la villa y su entorno inmediato 1 “Potrerillos Dam” building work Impact on the village inhabitants and its close environment Prof. Dra. María E. Gudiño de Muñoz Resumen A fines de la década de los noventa se inicia en Mendoza la construcción de la presa Potrerillos, obra hidroeléctrica que tiene el propósito de regular las aguas del río Mendoza, del cual depende el riego y la vida de gran parte del oasis Norte de la provincia. En la serie de beneficios que se esperan de esta obra no figura la población local, que es la directamente afectada. Los resultados obtenidos permiten descubrir aspectos de la realidad y del estilo de vida de Potrerillos hasta el momento desconocidos y que hacen predecir el fuerte impacto socioeconómico que tendrá esta obra, al tener que trasladar población y al constituirse en un polo de atracción para grandes contingentes de turistas ocasionales que buscan aprovechar el espejo de agua o disfrutar del medio natural. El diagnóstico obtenido permite descubrir las alteraciones socioeconómicas a producirse debido a la relocalización de familias, cuyos lotes y viviendas quedarán bajo el agua, aspectos que no se tienen en cuenta en la evaluación de impacto ambiental, en donde se pone el acento en aquellos impactos que pueden llegar a alterar el ecosistema local y regional, pero no en los efectos que ocasionará en la calidad de vida de los lugareños. Palabras claves: Impacto ambiental / Ecosistema local / Ordenamiento territorial. Abstract At the end of the nineties, the Potrerillos dam building is started in Mendoza, a hydroelectric building work intended to regulate the Mendoza river waters, from which a large part of the irrigation and life of the Province North oasis depends.
    [Show full text]
  • A Case Study in Hydrology and Cultural Identity: 2,500 Years of Landscape-Making in Mendoza, Argentina
    A CASE STUDY IN HYDROLOGY AND CULTURAL IDENTITY: 2,500 YEARS OF LANDSCAPE-MAKING IN MENDOZA, ARGENTINA DAVIS, BRIAN Cornell University, Ithaca, New York, United States, [email protected] 1 ABSTRACT 2 INTRODUCTION Through an analysis of the Parque General San On the western edge of the city of Mendoza, Martin in Mendoza, Argentina, this paper Argentina there is a large park whose origins examines the work of 19th century landscape date to the late 19th century. In the park a sinuous designer Carlos Thays alongside the material lake and verdant forests and lawns combine contributions of the indigenous Huarpes people to with tennis courts, soccer fields and cultural consider the discipline of landscape architecture as monuments, all set against the sheer wall of the part of a long line of landscape practice in the Andean Cordillera rising just to the west. From challenging environment of western the interior of this landscape a visitor can see the Argentina. Mendoza, Argentina is a modern city of great, jagged heights of the mountains and sense nearly one million inhabitants situated on the border the expanse of the arid semi-desert that surrounds between the great agricultural plains of Argentina the city in all other directions. While dramatic, and the desert foothills of the Andes from inside Parque General San Martin these feel Mountains. Historically it has been a frontier far enough removed to impress without settlement of utmost strategic importance, existing overwhelming. variously at the southern edge of the Incan Empire, In this paper I explore a simple hypothesis: that the the eastern edge of colonial Chile, and now the Parque General San Martin, and the modern western border of Argentina.
    [Show full text]
  • Fly&Drive Mendoza
    Wednesday, April 8, 2015 Fly & drive in Mendoza - Argentina Day 1: Arrival at the airport. Pick up rental car. Our team welcomes you with open arms to Argentina and will give you directions to your hotel. Talk to our account executive for the best places to visit along the way, depending on the airport in which you arrive. Overnight in a 4-star hotel in Mendoza. Day 2: A tour of Mendoza, located at the foothills of the Andes, is scheduled today. We suggest you check out the old part of the city, where it was originally founded: la Alameda, Microcentro, Barrio Civico, and the General San Martin Park where you find La Gloria Hill, the sports stadium “Estadio Malvinas Argentinas”, and the Frank Romero Day Amphitheater (site of the National Wine Harvest Festival). The afternoon destination is Lujan de Cuyo, where you will spend the night, and the route you will follow is National Highway 40 to Provincial Highway 60. You should stop at the town of Carrodilla to visit the church, Our Lady of Carrodilla, the patron saint of wineries. Another recommendation: check out any of the following vineyards: Zuccardi, Clos de Chacras, Lopez, and Trivento. Overnight and dinner at the Club Tapiz Hotel. Day 3: We suggest a day of adventure and outdoor fun in the Potrerillos Valley. The route takes you back the same way you arrived: Provincial Highway 60 to National Highway 40 (Lujan de Cuyo) and then Highway 7 to Potrerillos. Once there, you will find all the facilities you need: a bar, restaurant, bathrooms, changing rooms with showers, lockers, towel rental, and photography services for all the activities.
    [Show full text]