ESAEducationHomeWeather and ClimateGlobal ChangeNatural Disasters
   
Coastal change
Danube Delta change detectionOil spills
Deforestation
Bardia National ParkCongo River BasinKameng-Sonitpur Elephant ReserveKilimanjaroRondoniaShillong and Guwahati
Ice
Antarctica 2003Climate change and glaciersGlacier analysis using radar imageryGlacial retreat in the AlpsGlacier Ice FlowMonitoring of glaciers in the HimalayasRemote sensing of ice and snow
Urbanisation
CairoCity of KathmanduCórdobaHimalayasKathmandu ValleyLagos
Vegetation
Annapurna Conservation AreaLost in the AndesNgorongoro Conservation AreaNiger Inland DeltaVegetation in South America
 
 
 
 
Article Images
Background
 
The movements of the Continental Crust and Lithosphere constrain the Oceanic Crust, Lithosphere and Asthenosphere to move downwards. This causes the Continental Crust to fold and lift up, producing volcanic activity.

Credits: Ministerio de Educación de España, Gobierno de España
 
 
Profile between Muelle Llico (Chile) and Malargue (Argentina)
Profile between Muelle Llico (Chile), 34°45’16”S 72°05’03”W and Malargue (Argentina), 35°30’S 69°35’W.

Credits: Rubén Mario Menso and Bernabe Franchino
 


Lost in the Andes!
Lost in the AndesIntroduction
Exercises
Exercise 1: The Andean regionExercise 2: Vegetation cover (NDVI) (for university students)Exercise 3: The geographical setting of the accidentExercise 4: The route back to civilisationExercise 5: Expedition “Alive!”Exercise 6: A multidisciplinary workshop
Eduspace - Software
LEOWorks 3LEOWorks 4 (MacOS)LEOWorks 4 (Windows)LEOWorks 4 (Linux)
Eduspace - Download
Lost_in_the_Andes.zip
More on the Andes tragedy
Wikipedia summary
 
 
 
   Copyright 2000 - 2015 © European Space Agency. All rights reserved.