Sierra la Primavera

{{Infobox mountain

| name = Sierra la Primavera

| photo = File:Cerro El Colli.jpg

| photo_caption = Cerro el Colli lava dome

| elevation_m = 2270

| elevation_ref =

| location = Jalisco, Mexico

| range =

| map = Mexico

| map_caption = Location in Mexico

| coordinates = {{coord|20.62|N|103.52|W|display=inline,title}}

| topo =

| age = Pleistocene

| volcanic_arc/belt = Trans-Mexican Volcanic Belt

| last_eruption =

| first_ascent =

| easiest_route =

}}

Sierra la Primavera is a Late Pleistocene volcanic centre in Jalisco of central-western Mexico, located immediately west of Guadalajara in La Primavera Biosphere Reserve. It consists of a caldera, lava domes and lava flows that have formed in the last 200,000 years, with the latest known volcanic eruption having occurred about 30,000 years ago.

Geology

The formation of Sierra la Primavera commenced about 120,000 years ago with the eruption of rhyolitic flows and domes. This was followed by a VEI-6 eruption about 95,000 years ago that deposited {{Convert|20|km3|mi3|abbr=on}} of tephra with the creation of an {{Convert|11|km|mi|abbr=on}} wide caldera.{{cite gvp|title=Sierra la Primavera|vn=341820|accessdate=2020-03-13}} The tephra forms a volcanic deposit known as the Tala Tuff and consists of voluminous pumice flows.{{citation |last1=Ceballos|first1=Giovanni Sosa|last2=Vázquez|first2=José Luis Macías|last3=Cruz|first3=Diego Miguel|url=https://vhub.org/resources/4090/download/3Workshop_on_Volcano_Geology_2016_Abstract_book.pdf?4d0e3011e46f27f570a0b1079bd3e65f=1|title=IAVCEI Commission on Volcano Geology 3rd International Workshop, Etna-Aeolian Islands|work=Petrology of La Primavera caldera magmas; the Tala Tuff case study|page=50|year=2016}}

Subsequent filling of the caldera with water resulted in the formation of a lake through which several lava domes were created. Several lava domes were emplaced along the caldera about 95,000 years ago, which was followed by the eruption of a younger series of ring domes about 75,000 years ago.

After uplift and sedimentation filled the lake, a final series of lava domes were erupted along the southern margin of the caldera about 60,000 to 30,000 years ago. Although volcanic eruptions are not known to have occurred from Sierra la Primavera in recorded history, it is still potentially active, containing a series of fumaroles and hot springs.

Subfeatures

Sierra la Primavera contains 29 named subfeatures:

class="wikitable sortable"
scope="col" | Name

! scope="col" | Type

! scope="col" | Coordinates

Cerro AltoDome{{Coord|20|42|0|N|103|32|0|W}}
Arroyo ColoradoDome{{Coord|20|35|0|N|103|30|0|W}}
Arroyo IxtahuatonteDome{{Coord|20|38|0|N|103|30|0|W}}
Arroyo la CuartillaDome{{Coord|20|43|0|N|103|31|0|W}}
Arroyo las AnimasDome{{Coord|20|37|0|N|103|35|0|W}}
Arroyo los PilasDome{{Coord|20|39|0|N|103|29|0|W}}
Arroyo SaucilloVent{{Coord|20|32|0|N|103|33|0|W}}
Cañón de las FloresVent{{Coord|20|42|0|N|103|35|0|W}}
Cerro el ChapulínDome{{Coord|20|41|0|N|103|29|0|W}}
Cerro ChatoDome{{Coord|20|42|0|N|103|34|0|W}}
Cerro el ColliDome{{Coord|20|39|0|N|103|28|0|W}}
Cerro la CuestaDome{{Coord|20|37|0|N|103|30|0|W}}
Cerro el CulebreadoDome{{Coord|20|37|0|N|103|33|0|W}}
Dos CoyotesDome{{Coord|20|40|0|N|103|29|0|W}}
Llano GrandeVent{{Coord|20|35|0|N|103|36|0|W}}
El MadrónDome{{Coord|20|37|0|N|103|31|0|W}}
Mesa el BurroDome{{Coord|20|43|0|N|103|35|0|W}}
Mesa el ChiquihuitilloDome{{Coord|20|43|0|N|103|36|0|W}}
Mesa el LeónDome{{Coord|20|41|0|N|103|36|0|W}}
Mesa el NajahueteDome{{Coord|20|40|0|N|103|31|0|W}}
Mesa la LoberaDome{{Coord|20|43|0|N|103|30|0|W}}
Cerro el PedernalDome{{Coord|20|40|0|N|103|35|0|W}}
Pinar de la VentaDome{{Coord|20|43|0|N|103|25|0|W}}
Cerro las PlanillasVent{{Coord|20|35|0|N|103|33|0|W}}
La PuertaDome{{Coord|20|37|0|N|103|35|0|W}}
Río SaladoDome{{Coord|20|41|0|N|103|35|0|W}}
Cerro San MiguelVent{{Coord|20|36|0|N|103|36|0|W}}
Cerro el TajoVent{{Coord|20|36|0|N|103|29|0|W}}
Cerro el TuleDome{{Coord|20|38|0|N|103|32|0|W}}

See also

References