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| Heart Trail |
This post was originally published on rockychrysler.com in June 2015.
The following was written and submitted by me "in partial completion of the requirements" for a Geology For Teachers course I took at Northern Arizona University in the summer of 2004, during what is probably best characterized as the second-phase (of four, I think) of my 20+ year-long post-baccalaureate academic career at NAU.
The paper is about some of the really interesting non-volcanic, sedimentary geology found on the eastern end of Mount Elden that's conveniently bisected by the Heart Trail*.
After I completed this paper, I uploaded it to Wikipedia where it became the initial kernel for the site's Mount Elden topic. I'm pleased to report, much of my original content is still intact to this day.
The descriptions and photographs below are based on observations that I made along the original Heart Trail in the summer of 2004.
* Beginning in 2019, the entire trail was rebuilt at a new, less-severe grade and on a lengthier and more sustainable alignment. Despite these changes, all the geologic features referenced below can still be observed at the general elevations indicated below, however the approximated distances between features may vary given the changes to the trail.
An Overview of the Geology of the Eastern Sedimentary Block of Mount Elden
A paper submitted in partial completion of the requirements for
GLG 599
GLG 599
Middleton
30 September 2004






