Hey everyone, I am back! Another semester has come to an end, and that means more time I can dedicate towards blogging again. Unfortunately to anyone who enjoys reading this blog, and fortunately for me I am a day away from boarding a plane to Ireland for 7 weeks and Switzerland for one. I will be joining the JMU Geology Field Study to Ireland to explore and map the lands of the Emerald Isle. Though I will not let my absence from the country continue my absence from the blogosphere. Today begins the series of weekly posts containing pictures I have taken through various field trips over the past semester with the question asked: “Do you see what I see?” After showing the original photo I will include an annotated version of the geologically significant feature I am noticing.
Let’s get started.
In this picture, Jeremy points at an outcrop along I-64 in Virginia that we saw on the Igneous and Metamorphic Petrology class field trip this April. Do you see what I see?
What I see in this picture is the rifting of two supercontinents hundreds of millions of years apart. At this outcrop, the Catoctin, a metabasalt from the rifting of Rodinia approximately 610 Ma, is cross-cut by the younger basalt dike from the rifting of Pangaea 175-200 Ma. Notice that the Catoctin, a favorite on this blog, is distinguishable by the greenish-gray color from the chlorite minerals within it. The chlorite formed during the metamorphosis associated with the Appalachian Orogenies. Also note that the younger basalt dike does not share this characteristic because it is yet to experience the formation of a supercontinent.
So, within this one section of highway exhibits one rifting feature cross cutting an older rifting feature. Pretty cool.
*Unfortunate update: due to cancellation issues with the airline I was unable to finish writing the other posts of this series. I promise to finish them when I get back or if I find down time in Ireland. Sorry.
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