FIGURE 1. Index map of Montana showing study area 3. Correlation of measured sections in the 4-6. Photographs showing: 4. Cliff-forming Cut Bank Sandstone Member 5. Cut Bank Sandstone Member 6. Lower part of Cut Bank Sandstone Member 7. Correlation chart of Lower Cretaceous and Page 2 4 8 10 11 12 14 III CONTRIBUTIONS TO STRATIGRAPHY LOWER CRETACEOUS MOUNT PABLO FORMATION, NORTHWESTERN MONTANA By MELVILLE R. MUDGE and DUDLEY D. RICE ABSTRACT The newly established Mount Pablo Formation includes strata that crop out in the Sawtooth Range that are equivalent to the lower part of the Kootenai Formation in and west of the Sweetgrass Arch. Palynomorphs indicate an age of early Albian to possibly late Aptian. The Mount Pablo Formation unconformably overlies Jurassic rocks and is overlain unconformably by the Lower Cretaceous Kootenai Formation. Lateral equivalents of the Mount Pablo belonging to the Kootenai are widespread in the subsurface west of the crest of the Kevin-Sunburst dome. The Mount Pablo consists of nonmarine sandstone and conglomerate in the lower part, variegated mudstone interbedded with some sandstone in the middle part, and limestone interbedded with and overlain by mudstone in the upper part. The lower sandstone and conglomerate is the Cut Bank Sandstone Member, a previously established unit assigned as the basal member of the Kootenai Formation in the subsurface in the Cut Bank area that is extended to the Sawtooth Range and assigned to the Mount Pablo. This member ranges in thickness from 9 to 30 m (meters), whereas the formation ranges from 34 to 90 m. The Mount Pablo Formation is correlative with the Cut Bank Sandstone Member, Lander Member as described in 1966 by M. H. Oakes, and the basal "brown lime" unit of the Moulton Member, all of which are included in the lower part of the Kootenai Formation in the Cut Bank area. Lateral equivalents of the Mount Pablo pinch out eastward onto the Kevin-Sunburst dome, where the Sunburst Sandstone Member forms the basal unit of the Kootenai Formation and is correlative with the upper part of the Moulton Member. In the Canadian Foothills, the Cadomin Formation, which is a prominent conglomerate, correlates with the Cut Bank Sandstone Member of the Mount Pablo Formation or of the Kootenai Formation. The upper part of the Mount Pablo is equivalent to the Gladstone Formation in the southern foothills, to the Gething Formation in the northern foothills, and to the McMurray Formation in the central plains of Alberta. The palynological assemblage in the Mount Pablo is similar to that found in other Lower Cretaceous formations in the Western Interior and is somewhat similar to assemblages in the early to early middle Albian McMurray Formation of Alberta. 1 INTRODUCTION The Mount Pablo Formation is herein established as the lowest Cretaceous unit in the Sawtooth Range in northwestern Montana (fig. 1). Palynomorphs indicate an early Albian to possibly late Aptian age. Strata composing the Mount Pablo were formerly the lower part of the Kootenai Formation. The now geographically restricted and locally stratigraphically restricted Kootenai is retained as a formation. The Mount Pablo, which underlies the Kootenai and overlies Jurassic rocks, is named after Mount Pablo in the northern part of the Sawtooth Range, about 14 km (kilometers) south of East Glacier Park, in Glacier County. This report describes the Mount Pablo in outcrop and subsurface, and establishes its Early Cretaceous age and its correlation with other units elsewhere in the northern Rocky Mountains. The Kootenai Formation, as applied in the Sweetgrass Arch area and along the disturbed belt by previous workers, included all Lower Cretaceous rocks between the overlying Blackleaf Formation and the underlying Jurassic Morrison Formation. Cobban (1945, 1955) recognized two distinctive units in the Kootenai in the subsurface west of the Kevin-Sunburst dome and in a few exposures along the Rocky Mountain Front. The Mount Pablo Formation is essentially his lower unit. It mostly consists of red mudstone and whitish sandstone; the Cut Bank Sandstone Member is at the base, and beds of freshwater limestone are near the top. The FIGURE 1.-Index map of Montana showing study area. 104° Cut Bank Sandstone Member, named by Bartram (1935), is an oil and gas reservoir above a post-Jurassic unconformity in the Cut Bank area. The upper unit described by Cobban (1945) is darkbluish-green, olive-green, olive-drab, purple, and drab-maroon mudstone containing very lenticular beds of greenish-gray sandstone, and it is retained as the Kootenai Formation. The Mount Pablo Formation has been referred to as the unnamed formation in recent reports (Mudge, Earhart, and Rice, 1977; Mudge, Earhart, and Claypool, 1977; Mudge and Earhart, 1979; and Mudge, 1979). The Cut Bank is here retained as the basal member of the Mount Pablo. Other units mapped in subsurface in the Cut Bank area have not been recognized in the Sawtooth Range. MOUNT PABLO FORMATION The Mount Pablo Formation forms widespread outcrops in the Sawtooth Range south to the Dearborn River (fig. 2) and in the foothills east of the mountains from the South Fork Two Medicine River south almost to Birch Creek. In the western part of the Sun River area, Mudge (1972, p. A51) erroneously assigned rocks making up the Mount Pablo to the western facies of the Jurassic Morrison Formation. South of the Sun River the Mount Pablo is present in the westernmost Cretaceous exposures along Ford and Smith Creeks and as far south as about 3 km south of Elk Creek (fig. 2). TYPE SECTION OF MOUNT PABLO FORMATION AND REFERENCE SECTION OF CUT BANK SANDSTONE MEMBER A completely exposed section of the Mount Pablo Formation on the north side of Badger Creek is established as the type section, even though it is overturned, of the Mount Pablo and the reference section of the Cut Bank. This section is in the NE 1/4 SW1/4 sec. 3, T. 29 N., R. 11 W., in the Blackfeet Indian Reservation, Half Dome Crag 71/2minute quadrangle, Pondera County, and is accessible by an unimproved road that terminates at Badger Creek, a few meters west of the exposure. All fossil collections are catalogued by U.S. Geological Survey Mesozoic Collection numbers. The section was measured by M. R. Mudge using steel tape where direct measurements were possible and Jacob's staff elsewhere. Where applicable, the color of the rocks was determined by use of the "Rock Color Chart" of the Geological Society of America (Goddard and others, 1948). Measurements begin at the base of the lowest greenishgray, massive, crossbedded sandstone of the Kootenai Formation, which strikes N. 50° W. and dips 55° SW, overturned. The section is described as a normal section from top to bottom. |