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Guidebook to the Rio Grande Rift inRio Grande rift begin near the rift boundary, although the boundary in some locations may be elusive BRIEF GEOLOGICAL BACKGROUND OF THE RIO GRANDE RIFT The Rio Grande rift is a northtrending and northwardnarrowing (propagating) zone of lithospheric extension expressed in the upper crust by a series of northsouth–trendingThe 550kmlong Rio Grande rift is composed of a series of linked sedimentary basins trending northward from southern New Mexico into southern Colorado The focus of this report is the Española Basin, which is one in a series of four structurally linked, northtrending, rightstepping, en echelon basins in the central part of the rift (fig 2)

Geographic Focal Areas

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Location rio grande rift map-Location The Mount Princeton geothermal area is on the west side of the upper Arkansas Valley between the towns of Buena Vista and Salida in Chaffee County, Colorado (fig 1) The area is along the western flank of the northern extension of the Rio Grande rift ·zone and inc1udes aGEOL 1111 Principles of Earth Science Laboratory 8 – Spring 21 Plate Tectonics – Part 2 Hazards Associated with Plate Boundaries Part I – Divergent Plate Boundaries We have a divergent plate boundary, the Rio Grande rift, in our own backyard The map below shows the major basins of the rift zone 1) What is the total extent of the rift zone mapped in the United States?

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Buy BLM and Forest Service Maps for western public lands This comprehensive, spiral bound, waterproof, 122page river guide provides detailed, fullcolor maps of 153 miles of the Rio Grande, from Lasauses, Colorado to Cochiti Dam in New Mexico Divided into eleven river stretches�including the popular whitewater runs in the Taos Box, Racecourse, and White RockRio Grande Rift The Rio Grande rift is a major continental rift located within the western North American Cordillera Regional crustal extension in what is now the western United States initiated during the late Oligocene as a result of lithosphericplate interactions along and under the western margin of North American (Ingersoll et al, 1990)RiftBasin Hydrogeologic Framework Complexity "Seismic reflection, gravity, and drilling data have delineated the many large, deep basins that form the upper crustal expression of the Rio Grande rift Initially, the primary emphasis was on gravity studies However, the petroleum industry has released a considerable amount of seismic reflection

 The Rio Grande Rift The volcanoes are located near the middle of the Rio Grande Rift Valley A rift valley is a zone of weakness and thinning in the Earth's crust As the crust is pulled apart, large blocks of land drop down forming the valleyFigure 1 Simplified geologic map and tectonic setting of the Rio Grande rift (modified from Baldridge et al, 19) Dashed lines are approximate locations of magnetotelluric profiles Black rectangle indicates location of LA RISTRA seismic profile (Wilson et al, 05)100% (22 ratings) 1) Total extent of rift zone is approximately 400km long from north to south 2)Basin size generally View the full answer Transcribed image text Part 2 Exploring The Rio Grande Rift Rio Grande Rift Denver *Leadville 2 → Area of Locality Map Rio Grande (River San Luis Basin Utah Arizona Colorado New Mexico Major

#11 Taos Plateau volcanic field Unclassified Updated The Taos Plateau volcanic field is an area of extensive volcanism in Taos County, New Mexico, United States It is the largest volcanic field in the Rio Grande Rift, spreading over 7,000 km The age of most of the vents and associated lava flows in the field is estimated to be between 18 and 4 million years, with a few 22One of the littleknown reasons that it is unique is that it is the site of the Rio Grande Rift which extends from southern Colorado (the San Luis Valley) down the center of our state and into northern Mexico* (see map and diagram on following pages) The Rio Grande Rift is an arm of the Basin and Range Province extending across westernmost Texas, New Mexico, and southern Colorado Earthquakes, faultblock mountains, and volcanism at Guadalupe Mountains National Park and Bandelier and White Sands national monuments are consequences of the ongoing continental rifting

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Rio Grande rift Last updated Locality map showing the Rio Grande rift extending from southern Colorado to Chihuahua, Mexico The Rio Grande follows this rift for much of its course The Rio Grande rift is a northtrending continental rift zone It separates the Colorado Plateau in the west from the interior of the North American craton on the east 1The red triangles in the map below represent Rio Grande Rift network GPS station locations If you want to know more about a particular site, click on a triangle below or the site link at right to get details Click here to find out what a GPS site installation looks like!At 650 feet (0 m) above the Rio Grande, it is the fifth highest bridge in the United States The span is 1,280 feet;

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 The headwaters are in the San Juan Mountains of Colorado, and entire course of the river through New Mexico follows a topographic depression that traces the Rio Grande Rift (RGR) The RGR is relatively uncommon geologic phenomena, a continental rift (there are only three others in world), and it represents a stable continental plate slowly being torn apart;The Rio Grande Rift is a series of rift valleys along faults in the Southwestern United States The Rio Grande Rift separates the Colorado Plateau, which is generally moving in a clockwise direction, from the older part of the North American plate The Rio Grande Rift stretches from central Colorado to the Mexican state of ChihuahuaThere is evidence that the Rio Grande Rift is tectonically active by the presence of the Socorro magma body at midcrustal depths and the occurrence of earthquake swarms associated with it (ie Balch, et al, 1997;

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Trending Rio Grande rift and the northeasttrending Jemez lineament (figs 1 and 2) The region is a potential location for geothermal exploration, as indicated by several boiling pools of acidsulfate muddy water, fumaroles, and the many hot springs in the area This bibliography was compiled as part of a study by theC Heat Flow Across the Rio Grande Rift The Rio Grande rift system is an en echelon train of elongate, discontinuous tectonic basins with Tertiary and Quaternary volcanism, high heat flow, seismicity, and negative gravity anomalies occurring in New Mexico and Colorado (Fig 1) rift ranges in age from 37 Myr at Latitude 33'N,The Rio Grande, known in Mexico as the Río Bravo del Norte and as the Río Bravo, is one of the principal rivers in the southwestern United States and in northern Mexico The length of the Rio Grande is 1,6 miles and originates in southcentral Colorado, in the United States, and flows to the Gulf of Mexico The Rio Grande drainage basin has an area of 1,0 square miles;

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Schlue, et al, 1996) The Socorro magma body has experienced active magma intrusions as currentSchematic regional map showing the locations of major pre and synrift volcanic fields in Colorado and New Mexico and their spatial association with conventionally defined borders of the Rio Grande rift and major uplifts of the Southern Rocky Mountains Modified from Thompson and others (1991) after Tweto (1979) Details Image Dimensions 800 x 550The oceanic ridges have a cleft, or rift, in the middle rather than a peak The photo below shows the Rio Grande Rift from east of Socorro, New Mexico Here you can observe a mountainous region in the background and the Socorro basin in the middle region of the photo

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To the east you have an excellent view of the Rio Grande valley Here on the fissure line of the Albuquerque Volcanoes you are standing very near the center of the Rio Grande rift The rift starts in the area of the Rio Puerco over the western horizon and goes all the way over to the base of the Sandia MountainsThe Basin and Range Province is the archetypal example of a wide rift, and the neighboring Rio Grande rift is one of the classic modern examples of a narrow continental rift (eg, Buck, 1991) For most of its length, the Rio Grande rift isThe Rio Grande rift is a major structural element of the Southern Rocky Mountain region During the last years this feature has become widely recognized as a

Figure 1 Identifying Buried Segments Of Active Faults In The Northern Rio Grande Rift Using Aeromagnetic Lidar And Gravity Data South Central Colorado Usa

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Tectonic history of the rift has many parallels with the Basin and Range to the west (Chapin and Seager, 1975; World River Map World Map With Major Rivers And Lakes A Map Of The Study Area And The Pelotas Basin The Location Physiographic Provinces Of The Southwestern United States Indus River On A World Map Html Template Design Geography Of Puerto Rico Rio Grande River On World Map Rio Grande Ree Oh Grand Is New Mexico Map Map Of New Mexico NmTwo 300footlong approach spans with a 600footlong main center span The bridge was dedicated on and is a part of US Route 64, a

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Location Of The Albuquerque Basin Within The Rio Grande Rift Download Scientific Diagram

 The Rio Grande Rift Valley extends 1000 km (Chapin, 1972) from Southern Colorado to Northern Mexico The rift has created a series of basins with an average width of 50 km (Chapin, 1972) Basins in the north are larger, but the rift widens towards the south where smaller basins occupy a larger area similar in structure as the Basin and Range Provinces west of the riftThe late Cenozoic Rio Grande rift extends from northern Colorado to southern New Mexico, and it consists of numerous half grabens of alternating polarity that are separated by structural accommodation zones The northnorthwestelongate, eastdipping San Luis graben system defines the rift in southernThe Rio Grande rift is a northsouth trending zone of approximately eastwest oriented extension that bisects the state of New Mexico The extension is due to the Colorado Plateau pulling away from the High Plains, which causes the Earth's crust to be stretched and thinned

Oxygen Isotope Evidence For Subduction And Rift Related Mantle Metasomatism Beneath The Colorado Plateau Rio Grande Rift Transition Springerlink

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The Rio Grande rift is a continental rift, stretching from northern Colo­ rado into Mexico, that began development 30 Myr ago (Chapin, 1979) The rift is composed of three major segments that become progressively older to the south Three en echelon basins compose the middle segmentThe Rio Grande rift and Basin and Range Province are two of the most iconic extensional domains on Earth;The Rio Grande Rift, as it is known, is a massive rent in the Earth's crust, miles wide and several miles deep Stretching for miles, it forms Colorado's San Luis Valley and slashes New Mexico in two As explained by the New Mexico Bureau of Geology and Mineral Resources, the rift resembles "a plowed furrow with raised shoulders"

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 3 The Colorado PLAteau/RIo Grande Rift Seismic TRAnsect Experiment (La Ristra) is a passive seismic experiment that was run along a transect from the Great Plains, across the Rio Grande rift and Jemez lineament, to the middle of the Colorado Plateau The experiment consisted of 54 broad band seismic instruments deployed in a northwest oriented linear array shown in#6 Taos Plateau volcanic field Unclassified Updated The Taos Plateau volcanic field is an area of extensive volcanism in Taos County, New Mexico, United States It is the largest volcanic field in the Rio Grande Rift, spreading over 7,000 km The age of most of the vents and associated lava flows in the field is estimated to be between 18 and 4 million years, with a few 22millionFurther west, SHmax is approximately NS along the Rio Grande Rift of central Colorado to northeast Mexico West of the Rio Grande Rift, on the Colorado Plateau, SHmax regains an

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Geographic Focal Areas

Seager and others, 1984) The geology of the southern Rio Grande rift is among the best characterized of any rift system in the world Also,Geologic Model of the Rio Grande Rift Byron D Stone, James C Cole, and David A Sawye Regional location map of the Middle Rio Grande Basin study area 2 B1 Estimates of paleorecharge for the Middle Rio Grande Basin 6 C1 Map of the Middle Rio Grande Basin showing location of thirteenThe Rio grande rift is a late cenozoic continental rift extending south from at least Leadville, colorado to chihuahua, Mexico it represents the easternmost expression of widespread continental extension in the western United States during the past 30 million years The Rio grande rift is characterized by normal fault

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Map Of The Rio Grande Rift In Colorado New Mexico And Texas Showing Download Scientific Diagram

Sanford, A R, 1979, Characteristics of the Rio Grande rift in the vicinity of Socorro, New Mex­ico, from geophysical studies;The Rio Grande Rift began forming between 35 and 29 million years ago when Earth's lithosphere began to spread apart, triggering volcanism (volcanic activity) in the region It stretches from the state of Chihuahua, Mexico, to at least Leadville, The Rio Grande rift of the southwestern United States is one of the world's principal continental rift systems It extends as a series of asymmetrical grabens from central Colorado, through New Mexico, to Presidio, Texas, and Chihuahua, Mexico—a distance of more than 1000 km Although the Rio Grande rift is closely related in timing and

Perspectives On Continental Rifting Processes From Spatiotemporal Patterns Of Faulting And Magmatism In The Rio Grande Rift Usa Abbey Tectonics Wiley Online Library

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Goff and Janik, 02;The most prominent feature on this map is a tight cluster of activity centered near the community of Socorro Fig 4 The next map is a closer look at that cluster The area covered is the Rio Grande rift from south of Socorro to north of Albuquerque The time period is 1962 through 1994 and the cutoff magnitude is 251 Location map, land status, and regional setting of southern Taos Valley 2 2 Regional geologic map of the southern San Luis Basin of the Rio Grande Rift 9 3 Generalized geologic map of the study area, showing cross section lines 11 4 Stratigraphic chart of the southern

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The Rio Grande rift The Rio Grande rift is a region where the lithosphere is being per­ manently altered through thinning and (probably less importantly) in­ trusion of mafic magmas The rift is the culmination of a long and complex geologic history Initiation of rifting probably resulted fromRio Grande River It is one of the longest rivers in North America (1,5 miles) (3,034km) It begins in the San Juan Mountains of southern Colorado, then flows south through New Mexico It forms the natural border between Texas and the country of Mexico as it flows southeast to the Gulf of Mexico In Mexico it is known as Rio Bravo del NorteWith the help of UNAVCO, we are installing a network of 24 GPS stations across the Rio Grande Rift in Colorado and new MexicoA few stations are already permitted and other station locations are currently being finalized and we are requesting input from the community for stations in Colorado (CO station map) and in New Mexico (see map below)Our stations will form a dense

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The study area is located at the intersection of the Rio Grande rift (RGR) and the Jemez lineament (Fig 1A), an area defined by thin crust, slow mantle velocities, and a young volcanic history (Easely et al, 11;

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