Cooperative Institute for Research in Environmental Sciences

Day 3 & 4: Trilobites and Tectonics »

by kanarde | posted: July 19th, 2009

6/24-6/25

After leaving base camp at the Iowa State Field Camp in Shell, we drove upstream through the canyon to take a look at Shell Falls. The folding in Shell Canyon triggered a discussion on how the structure of the Big Horns fits in the big picture of the formation of the Rockies.

Folding in Shell Canyon

Folding in Shell Canyon

Continue reading Day 3 & 4: Trilobites and Tectonics

Day 2: Sheep Mountain »

by kanarde | posted: June 29th, 2009

6/23/09

“And be on guard, I saw five or six rattlesnakes last time I was here.”

Chris and Eric at the anticline

Chris and Eric at the anticline

Not only were we walking blindly on train tracks into the canyon, now with the prospect of snakes this venture became ten times more exciting! Eric was in the lead, narrating the way through Sheep Mountain where he and his students have done research previously. Continue reading Day 2: Sheep Mountain

Day 1 (6/22/09): Across the Bighorns »

by kanarde | posted: June 29th, 2009

I joined EarthScope investigators Christine Siddoway and Megan Anderson (Colorado College) and Eric Erslev (University of Wyoming) on a 4-day structural geology tour of the Bighorn Mountains in northern Wyoming. A group to be led by Megan will install seismic stations throughout the range this summer as part of the Foreland Basement Arch Seismic Experiment. Christine and Eric have students starting fieldwork in the Bighorns for structural geology theses. For all who are involved in the work this summer, the field trip provided an introduction to the regional geology of the Bighorns basement arch. Continue reading Day 1 (6/22/09): Across the Bighorns

New Zealand research location

Figure 1. Design of the proposed Bighorns seismic experiment on a shaded relief digital elevation model of the northern Rocky Mountains (BHM: Bighorn Mountains). Lines 1 & 2 are short period passive / active source transects, with active source shots marked by small stars. Broadband seismic stations (purple squares) infill the USArray grid (TA broadband stations, filled black triangles). Large stars are source areas for mine blasts. Circles are epicenters for regional seismicity, 1973 to 2008.

About the blog

How did the Rocky Mountains form? Join geology undergraduate Katherine Anarde as she travels with structural geologists and geophysicists planning a seismic experiment in Northern Wyoming. Learn about the science and follow the journey here.

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