A rosy–fingered dawn metamorphoses into a vibrantly blue morning sky. In the blink of an eye, shadows and colors shift on the canyon walls. Another plate of scrambled eggs sits balanced on my lap. It is Day Six of our Colorado River rafting adventure in Grand Canyon. A question hangs suspended in midair. Where exactly in this magnificent chasm are we now?
|A balanced breakfast (Click on any pic to enlargenate)|
|Grand Canyon Supergroup tilts at river level|
Once upon a time, North America looked much different than it does today. For one thing, the continental landmass was smaller. Studies of the chemical composition of Grand Canyon rocks have led geologists to conclude that in this region the continent grew by collision and accretion of island arcs and other continental fragments during subduction of one ancient tectonic plate beneath another. A modern parallel to this tectonic growth is likely Indonesia, where the Australian plate is sliding northward, subducting beneath the Pacific plate and forming the volcanic island arcs of the Indonesian archipelago.
|Upper Granite Gorge|
|Metamorphic rocks of the Upper Granite Gorge|
Early 20th century studies in Grand Canyon identified different “packages” of deformed metasedimentary and intrusive igneous rocks that resulted from this tectonic activity. At 1.84 billion years old, the igneous intrusive Elves Chasm pluton is considered to be “basement,” the oldest rocks upon which subsequent sedimentary and igneous rocks were deposited or intruded.
|Faulting? Shearing? Something happened here.|
|Note convoluted rocks at lower right (click to enlargenate)|
|Convoluted rocks with a rapid|
In the Upper Granite Gorge, between river miles 113 and 120 (from Waltenberg Canyon to Blacktail Canyon, where we will have lunch and a serenade), the contact between the Elves Chasm pluton (1.84 billion years old) and a younger (1.75–1.73 billion years old) Grand Canyon Metamorphic Suite of schists is exposed.
|Elves Chasm gneiss?|
|A fellow rafter is mesmerized by the enormity of it all|
|Looks to me like pillow basalt in lower right|
Where exactly is this contact? I have no idea. Our guides are not geologists and so there is no one to point these things out to me. My research is done after the fact, long after I’ve returned home from this trip of a lifetime. I study my photos, and read my references, and try to weave a thread of sense from all I have seen. I need another river trip in a bad way!
|Igneous dikes cross cut the older gneiss|
|More cross cutting|
In the meantime, I nearly fall out of the boat when we encounter the SE–NW trending Monument Fold. The folded sedimentary layers look to be the Cambrian Tapeats Sandstone, quite a bit younger than the metamorphic Elves Chasm pluton and suite of schists beneath.
I am pretty sure this perky little structure is not the Monument Fold.
On the other hand, I am fairly certain this behemoth is.
|Monument Fold near river mile 116|
|Close up of Monument Fold|
The fold runs behind Explorer’s Monument and presents itself again downstream, just beyond river mile 118. I consider that it is likely the surface manifestation of a reactivated Precambrian thrust fault buried deep in the ground. There seems to be a lot of that sort of thing going on in these parts. When the folding occurred, I have no idea.
|The Great Unconformity at river level, from the mouth of Royal Arch Creek |
and Elves Chasm
There is missing time here, between the metamorphic rocks and overlying Tapeats Sandstone. Over a billion years is unaccounted for in the geologic record. This is the Great Unconformity at river level.
|A short hike takes us to Elves Chasm|
Around river mile 117 we disembark at Royal Arch Creek for a short jaunt. The Elves Chasm waterfall is a major reward for minimal exertion. Somewhere around here is the contact between the Elves Chasm pluton (gneiss) and the Grand Canyon Metamorphic Suite. I wish I could recognize it or have someone to point it out to me. I could be right on top of it and not know it.
|Explorer's Monument from|
|The two river elves|
Soon it is time to jaunt back to the boats. A lunchtime serenade beneath the Great Unconformity awaits us downstream at Blacktail Canyon.
|Back to the boats|
Karlstrom, K.E., Ilg, B.R., Williams, M.L., Hawkins, D.P., Bowring, S.A., and Seaman, S.J., 2003, Paleoproterozoic Rocks of the Granite Gorges, in Grand Canyon Geology, Beus, S.S. and Morales, M., eds., 2nd edition, Oxford University Press
Stevens, L., 2013, The Colorado River in Grand Canyon – River Map & Guide, Grand Canyon Wildlands Council