The Trinidad, Colorado Earthquakes

The Trinidad, Colorado Earthquakes
Vincent Matthews
Colorado Geological Survey
Introduction
Around midnight on August 22, 2011, Colorado experienced its largest earthquake in half a century. The earthquake was quickly relegated to obscurity by the 5.8 earthquake that occurred about 12 hours later in Virginia
(AEG News, December 2011). Colorado's 5.3 magnitude earthquake occurred in a sparsely populated area,
whereas Virginia’s earthquake affected many people. Before the Colorado earthquake could even hit the evening
news, it was overshadowed by the earthquake out East.
The Director of the National Earthquake Information Center (NEIC) and the Director of the Colorado Geological Survey (CGS) conferred early in the morning before the Virginia quake and agreed that it would be advisable to deploy a portable seismic network to better understand what was going on in the Trinidad area. That
morning, the NEIC sent their team to deploy the network and CGS put a team on the ground to make a preliminary damage assessment (Morgan and Morgan, 2011). Fortunately, the Virginia quake held off just long enough
for the NEIC crew to install the instruments in Colorado before being sent off to the east coast.
Although occurring in a sparsely populated area about 15 miles southwest of Trinidad, Colorado this earthquake did cause damage to many of the buildings in the area. Forty six structures were damaged, and two residences were condemned (Figure 1).
History, Geologic Setting, Oil & Gas Activities
This 2011 earthquake was located near a damaging 4.6 magnitude earthquake that occurred in 2001. Long-term
residents of the area reported that the intensity of the 2001 quake was similar to an even earlier earthquake in
1973. The 2001 swarm was also collaboratively investigated by the NEIC and CGS. The NEIC deployed instruments and analyzed the seismicity, and CGS investigated the geology (Meremonte and others, 2002; Matthews,
2002). The data were all consistent with the earthquake source being a previously unmapped, northeast-southwest-trending, normal fault dipping steeply to the southeast (Figure 2).
Colorado is essentially being pulled apart where the Rio Grande Rift cuts north/south across the central part of
the state. The high mountains in the state (58 named peaks greater than 14,000 feet above mean sea level) are
a result of uplift on faults (with associated earthquakes) that are part of the Rio Grande Rift system. The state
has experienced numerous natural earthquakes, including a magnitude 6.6 earthquake in 1882 (Kirkham and
others, 2012). Hundreds of written reports relative to Colorado’s Neogene fault and earthquake history can be
found in the CGS “Earthquake Reference Collection” (http://geosurvey.state.co.us/hazards/Earthquakes/Pages/
Earthquakes.aspx).
The nearest Holocene fault is 35 miles to the west of the Trinidad swarms (Figure 2). The Northern Sangre de
Cristo fault is the boundary between the Sangre de Cristo uplift and the San Luis Basin of the Rio Grande Rift.
Another fault (Cheraw) that displaces Holocene deposits lies on the Great Plains about 80 miles to the northeast
of the two swarms (Kirkham and others, 2012). Like the two swarms in the Trinidad area (Figure 2), the Cheraw fault also trends roughly northeast-southwest.
The Trinidad area has a history of natural earthquakes (Kirkham and others, 2012):
•
In 1966, a 4.5 magnitude earthquake was reported northeast of Trinidad.
•
In 1973, a swarm of four earthquakes ≤4.2 magnitude was reported west of Trinidad.
•
In 1983, a magnitude 3.2 earthquake was reported northeast of Trinidad.
•
In 1996, a series of three earthquakes ≥3.2 magnitude hit northeast of Trinidad.
The Colorado portion of the Raton Basin has 2,875 active coalbed methane (CBM) wells that are currently producing about 10 BCF of gas per month. Additionally, there are 22 Class II Underground Injection Control (UIC)
wells disposing of produced water (Figure 2). Most of these wells are not using pressure to inject the water, but
are simply gravity driven into the underground strata about 4,000 to 5,000 feet deep. Other produced water in
the basin is disposed of on the surface.
Triggered or Natural?
Colorado has a long and storied history of triggered earthquakes (Matthews, 2012) from a variety of human
activities (chemical waste injection, coal mining, brine injection, oilfield waterflood, reservoir filling, and nuclear
blasts). Therefore, it is normal to ask whether any new earthquake activity occurring in the state might be
triggered by some human activity. Indeed, the question was raised by some residents in the Trinidad area as to
whether the 2001 earthquakes might be related to coal mining, or to the CBM production in the area that had
begun in the late 1990s.
Consequently, the NEIC and CGS, independently and using different approaches, evaluated the possibility that
UIC wells for CBM-produced water might be the trigger for the 2001 earthquakes. Both groups concluded that
the data were equivocal, i.e. one could not say that they were triggered, nor could one say that they were not triggered (Meremonte and others, 2002; Matthews, 2002). A couple of points relative to the 2001 swarm:
•
The swarm occurred over a four-mile-long distance (Figure 2).
•
Two water-disposal wells were located within 7,400 feet of the fault, one very close (Figure 2). •
The earthquakes on the fault mapped in 2001 stopped, even though injection into these wells continued.
For the next decade, no earthquakes were reported on the fault by NEIC. However, earthquakes (most too small
to feel) were reported fairly regularly throughout the southern part of the Raton Basin. These earthquakes appeared to follow no pattern, but seemed fairly random (Figure 2). It should be noted that seismograph coverage in Colorado was inadequate to pinpoint the epicenters of earthquakes. Errors of plus or minus ten miles, or
more, were not unusual during that time (Matthews, 2002; 2003).
The August 2011 event renewed interest in whether the earthquakes were triggered by underground disposal
of produced water. Several seismographs were deployed by the NEIC in the area immediately after the 5.3 M
earthquake. In December of 2011, the oil and gas industry deployed additional seismographs deep underground
to complement the USGS instruments. Oil and gas operators have generously shared data with CGS in both
the 2001 and 2011 swarms. Excellent data is now being obtained on the location, number, and size of the earthquakes; most of which are too small to feel. Additionally, industry is deploying seismometers throughout the
CBM producing area for a longer term study. This new data will provide researchers with information to perhaps
finally understand the cause(s) of the earthquakes in the Raton Basin.
Preliminary data from this network reveal that the earthquakes are not randomly distributed as shown in Figure
2 from the NEIC database, but are tightly clustered into several swarms, one of which appears to consist of after-
shocks from the August 2011 event. Depths of the earthquakes are as great as 40,000 feet.
Several recent earthquake swarms across other parts of the nation have generated questions as to whether they
were triggered by oil and gas operations. Indeed, the USGS created a recent flurry of publicity and controversy
by claiming that an increase in earthquake activity throughout the midcontinent (including Colorado), is “almost certainly manmade” (Soraghan, 2012). The directors of the Oklahoma and Colorado Geological Surveys
independently characterized these conclusions for their states as premature.
The Colorado Oil and Gas Conservation Commission (COGCC) and the Potential for Triggering Earthquakes
In 2011, the COGCC took a proactive stance toward the possibility of UIC wells causing earthquakes. The
COGCC staff asked the CGS to review all new permit applications for UIC disposal wells. The CGS has been
reviewing those applications since October 2011, and is making recommendations to COGCC, and the operators, regarding the possibility of generating earthquakes. The CGS is also working with COGCC, EPA, USGS,
and industry operators to understand the origin of the Trinidad earthquakes.
Acknowledgements
I am grateful to Harley Benz, Director of NEIC, and Hal Macartney, Geoscience Advisor for Pioneer Natural
Resources, for their spirit of collaboration. Jill Carlson, Matt Morgan, Jim Milne, and Chris Eisinger provided
useful reviews.
References
Kirkham, R. M., Rogers, W. P., Powell, L., Morgan, M. L., Matthews, V., and Pattyn, G. R., 2012,
Colorado Earthquake Map Server: http://geosurvey.state.co.us/hazards/Earthquakes/Pages/Maps.aspx.
Matthews, V., 2012, Earthquakes Triggered by Humans in Colorado — a background paper by the Colorado
Geological Survey, http://geosurvey.state.co.us/hazards/Earthquakes/Documents/Earthquakes%20Triggered.pdf.
Matthews, V., 2002, We don’t have earthquakes in Colorado, do we?: RockTalk, Colorado Geological
Survey, v. 5, no. 2, 12 p.
Matthews, V. 2003, The Challenges of Evaluating Earthquake Hazard in Colorado in Boyer, D.B, Santi, P.M. Rogers, W.P., Engineering Geology in Colorado- Contributions, Trends, and Case Histories, Association of Engineering Geologists Special Publication No. 15, 22 p.
Meremonte, Mark E., John C. Lahr, Arthur D. Frankel, James W. Dewey, Anthony J. Crone, Dee E.
Overturf, David L. Carver, W. Thomas Bice, and Nancy C. Dickman, 2002, Investigation of an earthquake
swarm near Trinidad, Colorado, August-October, 2001: USGS Open File Report 02-0073.
Morgan, M. L. and Morgan, K. S., 2011, Preliminary Damage Report of the August 22, 2011 Mw 5.3 Earthquake
near Trinidad, Colorado : http://geosurvey.state.co.us/hazards/Earthquakes/Documents/Preliminary%20Damage%20Report%20of%20the%20Mw%205-3%20Triniadad%20Earthquake.pdf
Soraghan, Mike, 2012, EARTHQUAKES: Okla., Colo. Geologists criticize USGS report as hasty: Energywire,
April 16,2012, http://www.eenews.net/public/energywire/2012/04/16/1.
Captions
Figure 1. Examples of earthquake damage from the August 22, 2011 event west of Trinidad, Colorado.
Figure 2. Orientation map for Colorado part of the Raton Basin (shown in purple shading). Red lines show the
location of the Holocene, Northern Sangre de Cristo fault which is in the National Seismic Hazard Map. Red
circles are earthquakes in the NEIC database. Yellow pentagons are Class II UIC wells. Purple outlines show approximate location of 2001 and 2011 earthquake swarms.
Figure 1