Espinaso Formation
{{Use American English|date=November 2020}}
{{Short description|A geologic formation in New Mexico}}
{{Infobox rockunit
| name = Espinaso Formation
| image = Espinaso Formation.jpg
| caption = Volcaniclastic beds of the Espinaso Formation at Arroyo del Tuerto
| type = Formation
| age = Late Eocene to Early Oligocene
{{Geological range|34.6|26.9}}
| period = Oligocene
| prilithology = Volcaniclastic
| otherlithology =
| namedfor = Espinaso Ridge
| namedby = K. Bryan and J.E. Upson
| region = Central New Mexico
| country = United States
| coordinates = {{coord|35.4065805|N|106.3183249|W|display=inline}}
| unitof =
| subunits =
| underlies = Tanos Formation
| overlies = Galisteo Formation
| thickness = {{convert|430|m|feet|abbr=on}}
| extent =
| area =
| map = {{Location map+ | United States#New Mexico
| relief = 1
| width = 250
| float = center
| places =
{{Location map~ | United States#New Mexico
| lat_deg = 35.407
| lon_deg = -106.318
| mark = Orange pog.svg
| marksize = 12
}}
}}
| map_caption =
}}
The Espinaso Formation is a geologic formation in New Mexico. It has a radiometric age of 34.6 to 26.9 million years, corresponding to the late Eocene through Oligocene epochs.
Description
The Espinaso Formation is principally debris flows and lahars from the Ortiz porphyry belt, with some interbedded lava flows and tuff beds. The upper part of the formation is dominated by upward-fining sequences, where sediments are coarser near the base of the sequence and finer towards the top. This suggests waning volcanic activity and decreasing topographic relief.{{sfn|Kautz|Ingersoll|Baldridge|Damon|1981}} The formation intertongues with the underlying Galisteo Formation but unconformably underlies the Tanos Formation of the Santa Fe Group.{{sfn|Stearns|1953}} Radiometric dating gives an age range of 34.3 +/-0.8 million years (Ma) near the base of the formation, 34.6 +/-0.7 Ma near the middle, and 26.9 +/-0.6 my near the top. A basalt flow at the base of the overlying Tanos Formation has an age of 25.1 +/-0.6 Ma.
The formation crops out in the Hagan and Galisteo Basins and the La Cienega area of New Mexico. The type section is at Arroyo del Tuerto (Arroyo Pinovetito) where the arroyo cuts a slot canyon through Espinaso Ridge. Espinaso Ridge is a hogback produced by the strongly cemented volcaniclastics of the Espinaso Formation, which contrast with the less erosion-resistant beds of the underlying Galisteo Formation and overlying Tanos Formation.{{sfn|Stearns|1953}} The formation is also found in the subsurface in the southern Espanola Basin, where it was deposited on the eroded surface of a now-buried block of crust that was uplifted during the Laramide orogeny and thrown back down with the opening of the Rio Grande rift.{{sfn|Myer|Smith|2006}}
The formation records the style and composition of volcanic activity in the Ortiz porphyry belt, which is otherwise obscured by erosion of the volcanic centers.{{sfn|Erskine|Smith|1993}} The paleomagnetism of the formation has been closely studied, with one study indicating that the block of crust on which the formation was deposited subsequently experienced a counterclockwise rotation of 17.8° ± 11.4°, due to opening of the Rio Grande Rift,{{sfn|Brown|Golombek|1986}} but another showing no such rotation.{{sfn|Harlan|Geissman|2009}}
History of investigation
The formation was first described by C.E.Stearns in 1943, who credited the name "Espinaso Volcanics" to an unpublished manuscript by Kirk Bryan and J.E. Upson.{{sfn|Stearns|1943}} P.F. Kautz and coinvestigators recognized that it was primarily alluvial and designated it as the Espinaso Formation in 1981.{{sfn|Kautz|Ingersoll|Baldridge|Damon|1981}}
Footnotes
{{Reflist}}
References
- {{cite journal |last1=Brown |first1=Laurie L. |last2=Golombek |first2=Matthew P. |title=Block rotations in the Rio Grande Rift, New Mexico |journal=Tectonics |date=June 1986 |volume=5 |issue=3 |pages=423–438 |doi=10.1029/TC005i003p00423|bibcode=1986Tecto...5..423B }}
- {{cite journal |last1=Erskine |first1=Daniel W. |last2=Smith |first2=Gary A. |title=Compositional characterization of volcanic products from a primarily sedimentary record: The Oligocene Espinaso Formation, north-central New Mexico |journal=GSA Bulletin |date=1 September 1993 |volume=105 |issue=9 |pages=1214–1222 |doi=10.1130/0016-7606(1993)105<1214:CCOVPF>2.3.CO;2|bibcode=1993GSAB..105.1214E }}
- {{cite journal |last1=Harlan |first1=Stephen S. |last2=Geissman |first2=John W. |title=Paleomagnetism of Tertiary intrusive and volcaniclastic rocks of the Cerrillos Hills and surrounding region, Española Basin, New Mexico, U.S.A.: Assessment and implications of vertical-axis rotations associated with extension of the Rio Grande rift |journal=Lithosphere |date=June 2009 |volume=1 |issue=3 |pages=155–173 |doi=10.1130/L53.1|doi-access=free |bibcode=2009Lsphe...1..155H }}
- {{cite journal |last1=Kautz |first1=P. F. |last2=Ingersoll |first2=R. V. |last3=Baldridge |first3=W. S. |last4=Damon |first4=P. E. |last5=Shafiqullah |first5=M. |title=Geology of the Espinaso Formation (Oligocene), North-Central New Mexico |journal=GSA Bulletin |date=December 1981 |volume=92 |issue=12_Part_II |pages=2318–2400 |doi=10.1130/GSAB-P2-92-2318|bibcode=1981GSAB...92.2318K }}
- {{cite journal |last1=Myer |first1=Caroline |last2=Smith |first2=Gary A. |title=Stratigraphic analysis of the Yates #2 La Mesa well and implications for southern Española Basin tectonic history |journal=New Mexico Geology |date=August 2006 |volume=28 |issue=3 |pages=75–83 |doi=10.58799/NMG-v28n3.75 |url=https://geoinfo.nmt.edu/publications/periodicals/nmg/28/n3/nmg_v28_n3_p75.pdf |access-date=13 July 2021}}
- {{cite journal |last1=Stearns |first1=C.E. |title=Early Tertiary vulcanism in the Galisteo-Tongue area, north-central New Mexico |journal=American Journal of Science |date=June 1953 |volume=251 |issue=6 |pages=415–452 |doi=10.2475/ajs.251.6.415|doi-access=free |bibcode=1953AmJS..251..415S }}
- {{cite journal |last1=Stearns |first1=C.E. |title=The Galisteo formation of north-central New Mexico |journal=Journal of Geology |date=1943 |volume=51 |issue=5 |pages=301–319 |doi=10.1086/625156|bibcode=1943JG.....51..301S |s2cid=129038565 }}