This was the second annual
Geology Train. The Cumbres & Toltec Scenic Railroad (http://www.cumbrestoltec.com/)
offers numerous tourist trips each day during the summer. Unlike the other
train trips on this narrow gauge, steam-powered train, the Geology Train makes
numerous stops along the way and one of the geologists on board spends several
minutes explaining the geology we are passing through. The train also makes a
couple of stops where the passengers were able to get off and look at the rocks
more closely. At one of the stops, Toltec Gorge, we were able to walk through a
tunnel and take pictures of the train as it came through.
Map of Rio Grande Rift region showing the primary basins of the rift. Image courtesy of the USGS.1 |
The graphic above depicts a cross-section of a rift. Image courtesy of the USGS.1 |
Large-scale geologic features of the San Juan volcanic field in northwestern New Mexico and southwestern Colorado. 2 |
About 100
million years ago, the Farallon tectonic plate was subducting along the western
margin of the North American plate at a fairly steep angle. Magmatism and
crustal deformation associated with this subduction produced the Sierra Nevada
intrusive granitic rock in California and mountain
building events included the Siever orogeny in Nevada. Compressional stresses generated across the
subduction zone resulted in mountain building that progressively moved eastward
over time. About 75 million years ago, the modern Rocky Mountains began to
rise, reaching their peak elevations around 45 million years ago. The eastward
migration of mountain building is thought to be the result of the flattening in
the angle at which the Farallon plate was subducting. When the mid-ocean rift
separating the Farallon plate from the Pacific plate reached the western margin
of the North American plate, relative motion between the plates changed from
subduction to the strike-slip faulting that is observed today along the San
Andreas Fault. The compressional forces generated by subduction were relaxed as
the Pacific plate moved northward relative to the North American plate. At the same time, the
subducted Farallon plate began to sink into the mantle.
This is thought to have set up conditions that generated the explosive and
voluminous volcanism in the San Juan Mountains and elsewhere in Colorado,
My wife and I took
this train trip about 10 years ago. However, having USGS geologists and
geoologists from local colleges explaining the geology this time made the trip
more interesting. The geologists kept their descriptions pretty simple so that
the non-geologists on the trip were able to learn something. If you are in
southwestern Colorado next summer around this time, I would recommend the trip.
For trip schedules consult the Cumbres & Toltec Scenic Railroad website at
http://www.cumbrestoltec.com/.
References:
1 Rio Grande Rift FAQ, ____, Measuring Rio Grande Rift Crustal Deformation; www.earthscope.org, 2 pages.
2 _____, 2012, Geology Train Excursion on June 24th 2012 Aboard the Cumbres and Toltec Scenic Railroad; Cumbres and Toltec Scenic Railroad, 18pages.
1 Rio Grande Rift FAQ, ____, Measuring Rio Grande Rift Crustal Deformation; www.earthscope.org, 2 pages.
2 _____, 2012, Geology Train Excursion on June 24th 2012 Aboard the Cumbres and Toltec Scenic Railroad; Cumbres and Toltec Scenic Railroad, 18pages.
Humphreys, E., Hessler, E., Dueker, K., Farmer, C., Erslev, E., and Atwater, T., 2003, How Laramide-age hydration of North American Lithosphere by the Farallon Slab Controlled Subsequent Activity in the Western United States; International Geology Review, v. 45, p. 575-595.
Kelly, Shari, 2012, Conceptual Models of the Rio Grande Rift; Lite Geology, Spring 2012, New Mexico Bureau of Geology & Mineral Resources, pp 2-5.
Lipman, P.W., 2006, Geologic Map of the
Central San Juan Cluster, Southwestern Colorado; U.S. Geological Survey Map I-2799.