This is an active volcanic field and future eruptions are anticipated. The Pinacate volcanic field is located in northwestern Sonora, Mexico, near the northern end of the Gulf of California. [4], The El Pinacate y Gran Desierto de Altar Biosphere Reserve is a biosphere reserve, in the spanish language Reserva de la Biosfera el Pinacate y Gran Desierto de Altar, managed by the Mexican Federal Government's SEMARNAT - the Ministry of the Environment and Natural Resources, in collaboration with the government of the State of Sonora's IMADES agency. The tallest of the peaks is Cerro del Pinacate (also called Volcan Santa Clara), elevation 3,904 feet (1,190 m). There were two distinct episodes of tephra production, Tephra Unit 1 (T1)followed by Tephra Unit 2 (T2). The source vent of the eruption is Tecolote volcano (27 ± 6 ka, 40 Ar/ 39 Ar). Pinacate volcano is a young volcanic field of maars, tuff rings, more than 500 basaltic cinder cones in the Sonoran desert in NW Mexico, a nearly unpopulated region between Arizona and the Gulf of California. NOTE: In a previous version of this post, I featured the EO-1 ALI image below, and an astute reader pointed out that these peaks, while in the Biosphere Reserve, are not Pinacate Peaks, but rather the Sierra de Rosario range nearby. Pinacate volcano is a young volcanic field of maars, tuff rings, more than 500 basaltic cinder cones in the Sonoran desert in NW Mexico, a nearly unpopulated region between Arizona and the Gulf of California. The shield Volcan Santa Clara is the largest volcano in the field and is pimpled with smaller cinder cones. The field comprises 2,000 km2 of basaltic volcanic rocks. The United States/Mexico border runs across the upper right corner of the image. The field covers an area of about 60 x 55 km and has been active less than 10,000 years ago. More than 300 volcanic vents occur in the Pinacate field, including cinder cones that experienced small eruptions as recently as 1934. The United States/Mexico border runs across the upper right corner of the image. Here we reconstruct one of the youngest eruptions in the Pinacate volcanic field (Sonora, Mexico)and estimate the volumes of the lava flows, scoria cone, and tephra units. The field is prominent in satellite photos of this arid region of NW México near the head of the Gulf of California. Discover (and save!) While a milestone that was not the culmination of his love affair with the Pinacate volcanic field. The Pinacate Desert is home to the largest sand dunes of the Americas. El Pinacate Volcanic Field (PVF) is located on the NNW region of Sonora, Mexico, and it consists on older lava flows, covered and surrounded by some cinder cones and younger lava flows, result of two different volcanic events, the older one, the event Pre Pinacate (Miocene) and the younger one Pinacate (Quaternary). English: The Pinacate volcanic field is a roughly 55 x 60 km area containing numerous maars, tuff rings, and cinder cones in NW México near the head of the Gulf of California. Maar-calderas created by steam activity are common enough to be considered major features of monogenetic volcanic fields; sixteen of those "Fifty Fields" have them. Pinacate Volcano Field (Public domain.) Location. The volcanic cinder cone field stains the landscape of bright sand and tall dunes in the El Pinacate y Gran Desierto de Altar Biosphere Reserve. Pinacate Volcanic Field, Mexico. The field comprises more than 300 small basaltic volcanoes - cinder cones and maars. This website is my Pinacate book. Oct 14, 2013 - This Pin was discovered by Lynn Recker. The source vent of the eruption is Tecolote volcano (27 ± 6 ka, 40Ar/39Ar). Here we reconstruct one of the youngest eruptions in the Pinacate volcanic field (Sonora, Mexico) and estimate the volumes of the lava flows, scoria cone, and tephra units. Pinacate is a 1500 km oval of Lower Sonoran Desert covered with lava flows and cinders of more than 450 small volcanoes distributed across the area. These magmas were evolved from basalt by fractional crystallization and constitute the entire alkaline rock series from basalt to trachyte. One of the small cones, Tecolote, is unique in the world. The field today is part of El Pinacate and Gran… Surrounded by the Sonora Desert, this field contains more than 300 volcanic vents and cinder cones, including at least 10 maar craters. Monogenetic volcanic fields of Quaternary age like this one are scattered across all the tectonically active regions of the Earth; more than fifty lie within 1000 km of Pinacate. It is a kilometer-tall Cerro (mountain) rather than Sierra (range) dotted with younger cone volcanoes like Pinacate Peak, the highest point in the field. Among the youngest lava flows of the Pinacate volcanic field, Sonora, Mexico, is a large outpouring of tholeiite, the Ives flow. Pinacate is a monogenic volcanic field in Sonora, Mexico that lies just south of the Arizona border, seventy miles east of where the Colorado River empties into the Sea of Cortez. The Biosphere Reserve contains young volcanoes, basalt lava flows, and giant maar craters on the Pinacate Volcanic field. Part of El Pinacate y Gran Desierto de Altar Biosphere Reserve — Sonora. From space its a landmark at the head of the Gulf of California. The Pinacate volcanic field is a roughly 55 x 60 km area containing numerous maars, tuff rings, and cinder cones. Most of the rock fell into the space formerly occupied by gravel beneath the flows. The trachyte shield could be called a point-source volcano because its low viscosity magmas seem to have erupted through a small summit conduit system and flowed easily outward and downslope to build a volcanic shield. Much of its surface is covered with bombs of sizes that rival the giants of Germany’s Eifel District. The Pinacate volcanic field (PVF), located in the El Pinacate y Gran Desierto de Altar Biosphere Reserve of Sonora, Mexico, comprises a 1,500 km2 area of Pleistocene lava flows and contains nearly 400 cinder cones and eight maars. I reconstructed the third youngest eruption in the PVF. The Spanish name for the Pinacate Peaks geographic feature is the Sierra Pinacate, which is used in their homeland of Mexico. The field today is part of El Pinacate and Gran Desierto de Altar Biosphere Reserve and is a UNESCO World Heritage Site. Apollo 14's Alan Shepard and Ed Mitchell, and Apollo 17's Jack Schmitt trained here in Feb. In 1981, Dan Lynch completed his Ph.D. dissertation, "Genesis and Geochronology of Alkaline Volcanism in the Pinacate Volcanic Field, Northwestern Sonora, Mexico" at the University of Arizona. Tecolote appears to have melted internally but I’ll be damned if I know how. Pinacate volcan cinder cones 1200+ m / 3,937 ft Northwestern Mexico, 31.77°N / -113.5°W Condition actuelle : normal / en sommeil (1 sur 5) | Reports Pinacate livres [ afficher la carte This tube-fed pahoehoe flow contrasts sharply with other Pinacate lavas in its great volume, alkali-poor composition and morphologic features, which include novel small structures named "spatter tubes." Excavating a crater like the one pictured requires Herculean energies; that hole once held half a billion tons of rock and gravel that was ejected by steam explosions. The Pleistocene-Holocene Pinacate volcanic field encroaches on the Gran Desierto of Sonora, Mexico. Here we reconstruct one of the youngest eruptions in the Pinacate volcanic field (Sonora, Mexico) and estimate the volumes of the lava flows, scoria cone, and tephra units. NASA Information and Satellite Image: Pinacate Mountains, http://www.biology.ed.ac.uk/research/groups/jdeacon/desertecology/pinacate.htm, http://www.desertinvasion.us/areas/pinacate_res.html, Official Pinacate y Gran Desierto de Altar Biosphere Reserve website, Global Volcanism Program: Pinacate Mountains, https://en.wikipedia.org/w/index.php?title=Pinacate_Peaks&oldid=929892691, Articles containing O'odham-language text, Articles containing Spanish-language text, Creative Commons Attribution-ShareAlike License, This page was last edited on 8 December 2019, at 22:52. Dan Lynch’s love affair with the Pinacate Volcanic Field – Pinacate in Stereo. The field includes one large shield volcano and several hundred cinder cones and associated lava flows. The crest of the East Ridge subsided into a graben, and three valleys formed in the South Wall, each at the head of a short lava flow. The Pinacate Peaks (Sierra Pinacate, O'odham: Cuk Doʼag) are a group of volcanic peaks and cinder cones located mostly in the Mexican state of Sonora along the international border adjacent to the U.S. state of Arizona, surrounded by the vast sand dune field of the Gran Desierto de Altar, at the desert's southeast.[1]. Strong sulfur fumarole activity followed the bomb eruption, indurating some of the bomb-covered surfaces solidly enough to hold vertical scarps when the cone melted and the surface cracked apart along a profusion of faults. At its core lies the Sierra Pinacate, a central massif of old lava flows that is mantled with and surrounded by younger flows and cinder cones. Crater Elegante: a maar volcano in the Quaternary Pinacate volcanic field on the Arizona-Mexico frontier. Pinacate’s volcanoes are all on continental crust of the Southern Basin & Range geologic province; a colorful background of preCambrian gneisses, Permian and Laramide granites, and mid-Tertiary andesites. P-47415 September 19, 1996 This spaceborne radar image shows the Pinacate Volcanic Field in the state of Sonora, Mexico, about 150 kilometers (93 miles) southeast of Yuma, Arizona. All of the Pinacate magmas came through at least some ground water under the field but only about a dozen out of 465 eruptions even noticed the water and interacted with it. are a 30 mile wide volcanic field with many separate small volcanoes, rather than one giant volcano. The larger circular craters seen in the image are a type of volcano known as a "maar", which erupts violently when rising magma encounters groundwater, producing highly pressurized steam that powers explosive eruptions. The crater rim in the center of the photo is that of Crater Elegante, a 1.6-km-wide maar. Tecolote volcano, Pinacate volcanic field (Sonora, Mexico): A case of highly explosive basaltic volcanism and shifting eruptive styles April 2019 Journal of Volcanology and Geothermal Research 379 False-color … Rocks of the Organ Pipe-Pinacate region have been faulted and eroded into mountains and basins typical of the Basin and Range Province of SW North America. The source vent of the eruption is Tecolote volcano (27 ± 6 ka, 40 Ar/ 39 Ar). Pinacate has three giants that rival anything in Africa as well as a bunch of smaller ones. The cones are monogenetic, each is the product of a single, short eruption of a unique batch of magma that produced less (usually much less) than a tenth cubic km of rock. It is dominated topographically by the Sierra Pinacate, a broad, composite volcanic pile in the southern half of the field with a maximum elevation of 1,206 m. Many of these volcanic rocks evidently are of late Among hundreds of volcanic vents and cinder cones are rare maar craters, formed when rising magma met underground water to create pockets of steam that blew nearly circular holes in the … The Gran Desierto de Altar is one of the major sub-ecoregions of the Sonoran Desert, located in the State of Sonora, in northwest Mexico.It includes the only active erg dune region in North America.The desert extends across much of the northern border of the Gulf of California, spanning more than 100 kilometres (62 mi) east to west and over 50 kilometres (31 mi) north to south. The Pinacate volcanic field is located in northwest Sonora, Mexico, and comprises a 1500 km 2 area of lava flows with over 400 scoria cones and 8 maars (Gutmann, 2007) . In addition, there are a number of maar volcanoes, the most prominent of which is the Elegante Crater. 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