Red Hill volcanic field
Red Hill-Quemado
Campo vulcanico · United States · 2300 m

- Tipo
- Campo vulcanico
- Paese
- United States
- Regione
- North America Volcanic Regions / Basin and Range Volcanic Province
- Altitudine
- 2300 m
- Coordinate
- 34.250, -108.830
- Ultima eruzione
- -9450
- Contesto tettonico
- Rift zone / Continental crust (> 25 km)
- Forma vulcanica
- Cluster
- Roccia principale
- Basalt / Picro-Basalt
Sintesi geologica
The Red Hill-Quemado volcanic field in western New Mexico is across the border from the Springerville volcanic field in Arizona and contains more than 40 cinder cones and maars that were active from the late Miocene to early Holocene. The volcanic field lies along the NE-trending Jemez Lineament that extends from SE Colorado to east-central Arizona. Dating by Onken and Forman (2017) showed that three eruptive events took place during the early Holocene, and that the 2-km-wide Zuni Salt Lake maar with its late-stage nested cinder cones was formed about 11,000-11,800 calibrated 14C years ago.
Sintesi da Wikipedia
Riassunto in ingleseRed Hill volcanic field, also known as Quemado volcanic field, is a monogenetic volcanic field located in the vicinity of the ghost town of Red Hill in Catron County New Mexico. Red Hill is 24 kilometers (15 mi) east of the larger Springerville volcanic field and includes Zuñi Salt Lake. The area is made up of scoria cone and silicic dome fields. Over 40 volcanic vents have been identified in the field. These erupted basaltic flows, with no other rock types evident in the field.
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Storia delle eruzioni
Cronologia dettagliata
- 9450 a.C. (±400 anni)VEI ?Stima geologicaBCE 9450 – In corsoZuni Salt Lake maar
- 9700 a.C. (±450 anni)VEI ?Stima geologicaBCE 9700 – In corso2.5 km radius of Zuni Salt Lake
- 9850 a.C. (±500 anni)VEI ?Stima geologicaBCE 9850 – In corsoCerro Pomo?
Link esterni
⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.