Federal Trade Commission: Study Needed to Assess the Effects of Recent Divestitures on Competition in Retail Markets

This historic book may have numerous typos and missing text. Purchasers can usually download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1905 edition. Excerpt: ...of the lower 20 feet of section 4 and the upper portion of section 2; in the latter, Gypidula pseudogaleata (Hall) is also present, thus closely resembling the Becraft. Ed r i 0 c rinus pocilliformis Hall occurs in the lower beds of section 5 while it was not found earlier than the Becraft at Trilobite moun tain. The Becraft is a coarsely crystalline limestone (calcarenite) in sections 1, 2 and 3, containing many specimens of Gypidula pseudogaleata (Hall) and Spirifer concinnus Hall. In section 4 these beds will probably be found in the lower portion of the covered strata called Port Ewen, as the upper 20 feet of that section, correlated with the Becraft on stratigraphic grounds, are very similar both lithically and faunally to the uppermost New Scotland of section 3. No Gypidula pseudogaleata occurs in the Maryland section but S p i r i f e r c 0 n c i n n u s does; the latter species is thus found in all the sections, omitting section 4. Spirifer macropleura (Conrad) does not occur in the Becraft in any section. The Port Ewen is not recognized in section 5, and is covered in section 4. In section I it is very similar lithically and faunally to the Coeymans, while in sections 2 and 3 it quite closely resembles in like characters the New Scotland. The Oriskany of all the sections is more or less silicious. Some beds of section 2 and the upper Oriskany of section 5 are more distinctly sandstones. The fauna of sections I and 2 and the upper beds of 3 and 4 represent the calcareous facies of the normal Oriskany.1 Sections I and 2 contain many more of the typical shallow water forms than do sections 3 and 4. The lower beds of sections 3, 4 and 5 contain an older Oriskany fauna. In the shallowing waters of the upper portion of the Oriskany of...