The Quarterly journal of the Geological Society of London . his is, however, not quitecertain, the very thin wall of bone between the olecranon and thesupratrochlear fossae having perhaps been broken away by trochlear surfaces (t., fig. 2, A & C) are oblique ; the inter-trochlear ridge () is highly developed, and situated well tothe outer side of the trochlear groove, so that the outer surfacefor the radius is considerably narrower than the inner, much as in 1 Ueber Paarhufer der Fluviomarinen Schichten des Fajum Geol. Jena, vol. xv (1913) p. 200 [48] & pi. x
The Quarterly journal of the Geological Society of London . his is, however, not quitecertain, the very thin wall of bone between the olecranon and thesupratrochlear fossae having perhaps been broken away by trochlear surfaces (t., fig. 2, A & C) are oblique ; the inter-trochlear ridge () is highly developed, and situated well tothe outer side of the trochlear groove, so that the outer surfacefor the radius is considerably narrower than the inner, much as in 1 Ueber Paarhufer der Fluviomarinen Schichten des Fajum Geol. Jena, vol. xv (1913) p. 200 [48] & pi. xxi [v], figs. 1-3, 11. - The Structure & Relationships of Aiicodus Journ. Acad. Nat. Sci>Philad. ser. 2, vol. ix (1895) p. 474. 174 dr. c. w. Andrews on lower Miocene [June 1914, Brachyodus. In Diplopus the intertrochlear ridge is less marked,and nearer the middle of the surface ; moreover, the outer borderof the articulation is strongly produced downwards, a condition Fig. 2.—Humerus of an Anthraeothere (a fifth ofthe natural size). h^ a. B.
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Keywords: ., bookcentury1800, bookdecade1840, bookidquarte, booksubjectgeology
