IntroductionThe dominantly andesitic-to-dacitic Chimborazo volcano is mostly of Pliocene-to-Pleistocene age. The volcano collapsed about 35,000 years ago, producing a major debris avalanche, whose deposits underlie Riobamba and temporarily dammed the Río Chambo, producing an ephemeral lake.
Subsequent eruptions have been dominantly andesitic and constructed three edifices along an east-west line, the youngest and westernmost of which forms the current summit of Chimborazo.
Chimborazo sector collapse and debris avalanche
The debris avalanche deposit has not been directly dated, but a pyroclastic flow directly overlying the deposit has been dated at over 35,000 years, meaning that the collapse occured not too long before the eruption that produced the pyroclastic flow. The debris avalanche deposit has an average thickness of 40 m, covers an area of 280 sq km, and has a volume of > 11 cubic km.
- Smithsonian / GVP volcano information)
- Alcaraz et al (2005) "The debris avalanche of Chimborazo, Ecuador", 6th International Symposium on Andean Geodynamics (ISAG 2005, Barcelona), Extended Abstracts: 29-32
Chimborazo is a popular and challenging climb. The normal route up the mountain takes 10 hours to the summit and 4 hours to return.
Interesting fact: Chimborazo's distance from the earths center
Chimborazo's summit is the farthest point of the earth's surface from the center of the earth. Due to the centrifugal forces of its rotation, the earth's shape deviates from a perfect shpere and has a larger diameter at the equator than the length of its N-S axis. The distance of Chimborazo's summit from the center is 6,384.4 km, 2229 m more than the distance of Mt Everest's top to the center. (Source: Wikipedia)
See also: Sentinel hub | Landsat 8