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The Heart Mountain Thrust

The Heart Mountain Thrust is an Eocene feature. As was stated earlier, mid-Paleozoic rocks are on top of younger rocks. The fault is a thrust. Here is a basic overview of the extent of the fault.

2.5 meters above the base of the Bighorn Dolomite a bedding-plane fault developed covering an area 96km long and 24km wide, causing rocks to slide eastward. The sliding rocks caused a high-angle breakaway zone to develop on the northwest margin of the detatchment, and the rocks moved along a transgressive fault zone (15km long and 3km wide), cutting upsection and distributing upper plate blocks up to 50km across the ground surface! The heart mountain blocks (50) were distributed over a total area of 3400km squared.
One of the most fascinating things about the blocks is that they are not klippes (erosional remnants from a thrust sheet). If one were to add all the heart mt fault blocks they would fit almost perfectly into the place of origin. Therefore, the blocks were emplaced as seperate bodies. The question of how the blocks were transported such a great distance is still under debate. Here are some of the major theories:



The Absaroka Volcanics are another integral feature, when trying to understand the Heart mt thrust. There is considerable debate about this subject as well as to where the volcanics originated and when. In some places it appears as if the volcanics have been transported as one of the Heart mt fault blocks as well, or are interlaced among mid-Paleozoic sedimentary rocks, that lay unconformably on younger rocks. Some suggest that the volcanics were emplaced elsewhere and then transported due to one or another of the above theories. Others suggest that the Heart mt thrust occured prior to the emplacement of the volcanics, and that the volcanics that can be seen today are erosional remnants. There are even theories which suggest that there were phases of volcanism before and after the thrusting. Though there is more detail to these theories they are too deep to go into on this site, but if you wish to study them further, go to the source.


Results from my field work
The region of field work is located due east of the Ancestral Sunlight Volcano. Characteristics of the rocks suggest that many of the volcanics in the field area are transported remnants of this once-active cone. The volcanic features of the region consist of a series of dikes and lahars.

The dikes of the region contain plagioclase, horneblende, and augite and are therefore andesitic. The size and dominance of crystals in these rock bodies vary from outcrop to outcrop. This is due to the presence of a series of dikes, each occuring at different times, the latest ones cutting into the earlier. Dikes cap certain hills in the mapping region, or are repeated continiously down and along a saddle between two peaks. The latter occurance can be interpretted as a set of radial dikes, each of which came from the same magma chamber, which in this case would be that which was located below the Ancestral Sunlight Volcano.

Rocks containing volcanic clasts in a muddy, volcanic matrix are remnants of lahars. Not as common as dikes in this region, lahars are alligned with dikes on some peaks and along saddles in the mapping area. The clast size within lahars vary from flow to flow, and in some places seem to grade from small to larger stratigraphically upward. This represents the presence of seperate lahars occuring each after the previous.

Eocene Volcanism occured elsewhere, outside of the mapping area, in close approximity with the Ancestral Sunlight Volcano. This is evident due to the presence of radiating dikes, which typically occur around a volcanic center. The radial dikes found in the southwestern portion of the mapping area are now located too far from a volcanic center to have originated in the mapped area. Therefore, the thrusting occured after the formation of dikes and lahars (volcanics).

The mere presence of Madison Limestone (Mississippian) resting on younger, Chugwater Fm (Triassic) and Park City - Dinwoody Fms. (Permian) is evidence of the thrust. In the southwest, the volcanics are intermingled with Madison Limestone, resting on Park City - Dinwoody Fms. This is evidence that the volcanics formed elsewhere since they appear to have been transported along with older rock, as a Heart mt fault block.

The simplest evidence that volcanics occured elsewhere, before the thrusting, is on the top of Hill 8038T where an andesitic dike and volcanic lahar are resting unconformably on Triassic Chugwater Fm. Also, the dike ends abruptly at the Chugwater Fm, obviously not rooted in it.





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