A Micro-Prolog primer - download pdf or read online

By Clark K.L., McCabe F.G., Ennais J.R.

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In 1916, after purchasing a cheap car, Brown returned to northeastern Montana to prospect and study the geology. 6 km) to the east, he discovered an angular unconformity between the Hell Creek and Fort Union Formations. On the basis of recognition of this unconformity between the beds of the Hell Creek (= Lance) and overlying Fort Union Formation and the continuing lack of discovery of dinosaurs in the Fort Union strata, Brown wrote to Osborn confidently asserting the Hell Creek beds were deposited at the end of the Creta- ceous (see Dingus and Norell, 2010, p.

Could this unconformity represent the period of global diastrophism that some thought marked the Cretaceous-Eocene boundary? Brown’s studies carried out during 1908 and 1909 in and around the valley of Big Dry Creek, as well as observations made in other areas in Montana and Wyoming, caused him to modify his interpretation of the pattern of deposition. The unconformities between these two formations were interpreted as reflections of local erosion. “No sign of an angular unconformity has been noted between the Fox Hills and the “Lance,” and I have never yet seen any geological evidence of the ‘great diastrophic break’ which is alleged to occur here” (Brown, 1914, p.

Completing his geological analysis of the area, Brown briefly described the stratigraphically highest unit, the “Fort Union,” as being made up of “fine-grained sandstone, impure limestones and highly micaceous shales with occasional veins of lignite” (Brown, 1907, p. 836). He noted the abundant occurrence of leaf impressions, some of which were identified by Knowlton. Identification of this unit as Fort Union indicates that Brown considered it to be of “early Eocene” age in the then-current parlance.

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A Micro-Prolog primer by Clark K.L., McCabe F.G., Ennais J.R.


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