Naya-Micay Fault
| Naya-Micay Fault | ||
|---|---|---|
| Falla de Naya-Micay | ||
Age Quaternary | | |
| Orogeny | Andean | |
The Naya-Micay Fault (
strike of 034.1 ± 12 in the Tumaco Basin
along the Pacific Coast of Colombia.
Etymology
The fault is named after the Naya and Micay Rivers.[1]
Description
The Naya-Micay Fault runs parallel to and inland of the southwestern
alluvial deposits. In general, there are uplifted Tertiary sediments on the east and Quaternary sediments on the western side of the fault. The fault appears to be a northern continuation of the Remolino-El Charco Fault. The fault controls drainage of the Guapi River, locally offsets Quaternary deposits, and forms folded paleosoils, elongated basins and ridges and has strong general linear features. Along the coast, it forms typical fault-controlled linear landforms.[1]
See also
References
Bibliography
- Paris, Gabriel; Michael N. Machette; Richard L. Dart, and Kathleen M. Haller. 2000a. Map and Database of Quaternary Faults and Folds in Colombia and its Offshore Regions, 1–66. USGS. Accessed 2017-09-18.
Maps
- Paris, Gabriel; Michael N. Machette; Richard L. Dart, and Kathleen M. Haller. 2000b. Map of Quaternary Faults and Folds of Colombia and Its Offshore Regions, 1. USGS. Accessed 2017-09-18.
| Tectonic plates |    | ||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|
| Terranes | |||||||||||
| Terrane-bounding fault systems |
| ||||||||||
| Intraterrane faults |
| ||||||||||
| Major earthquakes | |||||||||||
| Orogenies | |||||||||||
| Other topics | |||||||||||
| Sources | Paris, Gabriel; Machette, Michael N.; Dart, Richard L.; Haller, Kathleen M. (2000). Map and Database of Quaternary Faults and Folds in Colombia and its Offshore Regions (PDF). USGS. pp. 1–66. Retrieved 2017-06-20.
Gómez Tapias, Jorge; Montes Ramírez, Nohora E.; Almanza Meléndez, María F.; Alcárcel Gutiérrez, Fernando A.; Madrid Montoya, César A.; Diederix, Hans (2015). Geological Map of Colombia. | ||||||||||
