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Mid-Carboniferous black shales in central Montana were included in the Heath Formation of the Big Snowy Group by Scott in 1935. Poor surface exposures have led to debate as to: 1) the existence of an unconformity between the Heath and the overlying Tyler formations, 2) the age of similar Tyler facies, and 3) whether strata assigned to the Tyler are mappable. New subsurface cores provide data that facilitate an internal subdivision of the Heath and enhance understanding of the relationship between Heath and Tyler strata. Historically, the definition of the base of the Heath has been based on a color change from bright green shales in the Otter to black shales in the Heath. This is problematic in that the contact is not exposed at the surface and is not mappable with precision. This study proposes that the base of the Heath / top of the Otter be redefined as the top of a laterally persistent limestone bed that is regionally correlative in the subsurface and is mappable at the surface (Scott, 1935). All of the bright green mudrocks of the type Otter are below this limestone, and all of the black mudrocks of the type Heath are above this limestone. The top of the Heath Formation should be defined as the sequence boundary above which sandstones and large wood fragments are present. The clastic-bearing unit above the Heath, deposited in incised valleys, is assigned to the Stonehouse Canyon Member of the Tyler. The Bear Gulch Limestone is within the Stonehouse Canyon and it should be included in the Tyler. The overlying Cameron Creek is distinguished by the predominance of red and green mudrocks and overlies a regional unconformity. New data allow for an informal subdivision of the Heath. These units, in ascending order, are the lower Heath, Van Dusen zone, Cox Ranch Oil Shale Interval (expanded from the original definition), Red Hill Carbonate (includes the Loco Ridge Gypsum bed), Winnett Shale (lowstand basin fill), and upper Heath. These cyclic, mudrock-dominated strata record an overall rising relative sea level during Heath deposition and a changing climate from moderately humid during deposition of the Van Dusen to very arid during deposition of the Red Hill Carbonate. Large eustatic sea level falls resulted in sequence boundaries at the Heath-Stonehouse Canyon and Stonehouse Canyon-Cameron Creek contacts.

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