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Red Hill volcanic field

Red Hill-Quemado

Campo vulcanico · United States · 2300 m

The Red Hill-Quemado Volcanic Field in New Mexico, USA, contains more than 40 scoria cones, some of which are in the area shown in this August 2019 Planet Labs satellite image monthly mosaic (N is at the top; this image is approximately 34 km across). There are also phreatomagmatic features including the 2-km-wide Zuni Salt Lake maar at the top of this Planet Labs satellite image monthly mosaic (N is at the top; this image is approximately 69 km across).
The Red Hill-Quemado Volcanic Field in New Mexico, USA, contains more than 40 scoria cones, some of which are in the area shown in this August 2019 Planet Labs satellite image monthly mosaic (N is at the top; this image is approximately 34 km across). There are also phreatomagmatic features including the 2-km-wide Zuni Salt Lake maar at the top of this Planet Labs satellite image monthly mosaic (N is at the top; this image is approximately 69 km across). · Foto: Satellite image courtesy of Planet Labs Inc., 2019 (https://www.planet.com/).
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 inglese

Red 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

Riepilogo (VEI nel tempo)
Fai clic su una barra per vedere le singole eruzioni
9850 BCE~9810 BCE · 1 eruzioni · VEI max. ?9730 BCE~9690 BCE · 1 eruzioni · VEI max. ?9490 BCE~9450 BCE · 1 eruzioni · VEI max. ?9850 BCE9770 BCE9650 BCE9570 BCE9490 BCE

Cronologia dettagliata

  1. 9450 a.C. (±400 anni)VEI ?Stima geologica
    BCE 9450 – In corso
    Zuni Salt Lake maar
  2. 9700 a.C. (±450 anni)VEI ?Stima geologica
    BCE 9700 – In corso
    2.5 km radius of Zuni Salt Lake
  3. 9850 a.C. (±500 anni)VEI ?Stima geologica
    BCE 9850 – In corso
    Cerro Pomo?

Link esterni

⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.