acquired August 16, 2011

Rhodes, Greece



Rhodes is the biggest island in the Greek Dodecanese chain in the southeastern Aegean Sea. Rhodes (also known as Rodos) stretches roughly 77 kilometers (48 miles) from northeast to southwest. Its highest point, Mount Attavyros reaches 1,200 meters (3,900 feet) above sea level. A variety of vegetation thrives on the rugged island and migratory birds use it as a resting place. Humans have lived here since the Stone Age.

The Thematic Mapper on the Landsat 5 satellite captured this image of Rhodes on August 26, 2011. Green vegetation is fairly abundant over the island, except for Mount Attavyros and some spots along the coast.

Satellite images such as this have provided more than pretty pictures. They have contributed to geologists’ understanding of the island’s history and structure. Geological research of Rhodes is nothing new, as the first studies of the island occurred in the 1850s. More systematic research from 1960 to 1965 resulted in a map issued by the Institute of Geology at the University of Milan, Italy.

Unfortunately, these studies occurred before the widespread acceptance of plate tectonic theory. Geologists now understand that our planet’s surface is composed of plates that move relative to each other. Rhodes sits in an active area, where the African Plate slides below the Aegean Plate, producing fairly strong earthquakes. Fossils found on Rhodes date back to the late Paleozoic Era before the dinosaurs evolved. The fossils are found in limestone, indicating that the island of Rhodes was once underwater. Around 15 million years ago, tectonic activity uplifted the whole region, but between 4 million and 3 million years ago, the land sank and left just the mountaintops above water.

When geologists reexamined Rhodes to create a new map, they not only incorporated advances in geologic theory but also advances in remote sensing. A paper published in 2007 described the compilation of a new geological map of Rhodes based in part on satellite observations by Landsat and by Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) on NASA’s Terra satellite.

  1. References

  2. Landsat Science. (2011, October 26). Rhodes. Accessed January 27, 2012.
  3. The Dodecanese Islands. Accessed January 27, 2012.
  4. Tsombos, P.I., Nikolakopoulos, K.G., Photiades, A., Psonis, K. (2007). Updating the 1:50.000 geological maps of Rhodes Island using remote sensing data and GIS techniques. Proc. SPIE, 6749, 67491H.
  5. U.S. Geological Survey. (2010, March 29). Tectonic Summary of Greece. Accessed January 27, 2012.
  6. U.S. Geological Survey. (2011, September 19). This Dynamic Earth: The Story of Plate Tectonics. Accessed January 27, 2012.

NASA Earth Observatory image created by Jesse Allen and Robert Simmon, using Landsat data provided by the United States Geological Survey. Caption by Michon Scott.