526 



GEOLOGICAL SURVEY OF THE TEEEITORIES. 



Fig. 54- 



great measure only estimates, as the circumstances were uot altogether 

 favorable to the making of accurate measurements. The dip of the 

 strata is about east-southeast, from 3° to 5°, apparently diminishing to 

 the eastward. 



The bed iTo. 9 of the section, in some of its thinner layers, appears 

 to be almost entirely made up of fossil remains, mostly of a species of 

 Melanian, but also a lesser proportion of a species of Viviparus. In 

 places where the rock was decomposed the whole upper surface is cov- 

 ered to the depth of an inch or more with the loose casts of these fossils, 

 which can here be gathered in any quantity, by simply scraping them 

 off the ledges. Other layers below, No. 11, also contain numerous 

 fossils, but in very much less abundance, and casts of Unio are found 

 in large numbers, while they are very scarce in the upper strata. 

 Scarcely any fossils were found in the beds other than those specified. 



In the vicinity of Bitter Greek Station, some four or five miles distant 

 in a general westerly or southwesterly direction, Mr. 

 Meek examined outcrops of some 275 feet of alternat- 

 ing beds of soft grayish and buff sandstones and whit- 

 ish shales and clays, the uppermost of which, judg- 

 ing from the dip and strike, must have been as 

 much as 200 feet below the lowest member of the 

 Table Kock section given above. No fossils 

 were found except fragments of fossil- wood ; 

 nothing to characterizeauy of thebeds. An 

 artesian boring at the station penetrated 

 445 feet through very similar alterna- 

 tions -of sandstone, shale, &c. ; the 



most noticeable variation in the rec- 

 ord, as given, being the occurrence 

 at the depth of 184 feet of an 

 18-iuch seam of black carbon- 

 aceous shale. Between the 

 lowest part of the 

 exposure at the 

 base of Table 

 Eock and 

 those ex- 

 amined by 

 Mr. Meek .. 

 there is ■■ 

 a Ion 

 stretc 

 of near 

 ly level 



SECTION AT BLACK BUTTES. 



country, affording no prominent outcrops by which the character of 

 the intermediate beds could be ascertained. 



Black buttes.; — Between the station of Bitter Creek and that of Black 

 Buttes, the next to the westward, is a distance of about nine miles by rail- 



