107 
Quercus simplex Newberry 
Plate XI, figures 1-4 
Quercus simplex Newberry, U.S. Geol. Surv., Mon. 35, p. 78, PI. 43, fig. 6, 
1898. 
The coriaceous lanceolate leaves of this species in all sizes are exceed- 
ingly common at Burrard inlet. They include, I believe, the materials 
from this locality which Sir William Dawson recorded as Salix varians 
Goeppert 1 and Salix Integra Goeppert 2 . All belong, in my judgment, to 
a single species and the venation is not that of Salix, but Quercus. The 
species is abundant in the Upper Clarno beds of Oregon, and it has also 
been recorded from Eugene, Oregon. Knowlton records it 3 from the 
Raton formation of Colorado and New Mexico, but I regard this last 
determination as doubtful. 
Quercus banksiaefolia Newberry 
Plate XVI, figure 6 
Quercus banksiaefolia Newberry, U.S. Geol. Surv., Mon. 35, p. 69, PI. 18, 
figs. 2-5, 1898. 
This species was described by Newberry from the Puget group at 
several localities in the state of Washington. Entirely characteristic 
specimens come from Kitsilano. 
Quercus uglowi Berry n. sp. 
Plate XV, figure 8 
Leaves of small size and sub-coriaceous texture, elliptical in general 
outline, with a shortly pointed tip and cuneate base. Margins entire 
basally for a greater or less distance, above which they are beset with 
somewhat irregularly sized and spaced, small serrate tenth. Length 
about 3*5 cm. Maximum width, in the median part of the leaf, about 
1-5 cm. Petiole stout and curved, enlarged poximad, about 7 mm. long. 
Midrib stout, and prominent on the under side of the leaf. Secondaries 
about 5 or 6 pairs, diverging alternately from the midrib at angles of 
about 45 degrees, rather straight and craspedodrome except for one or 
two basal camptodrome pairs. 
This is a well-marked new species, not particularly close to any pre- 
viously described forms. It shows some resemblance to the minimum- 
sized leaves of the Pacific Coast species Quercus chrysolepis and Quercus 
densifolia. It is named for the collector. Among previously described 
fossil forms it is somewhat similar to the minimum-sized leaves of Quercus 
consimilis Newberry* from the Bridge Creek Eocene of Oregon, and it is 
also something like what Lesquereux 6 identified as Rhus acuminata from 
the Green River Eocene. 
It comes from Joseph creek. 
1 Dawson, J. W., Trans. Roy. Soc., Can., 2nd aer., vol. 1, sec. 4, p. 147, fig. 11, 1895. 
* Idem., fig. 12. 
1 Knowlton, F. H., U.S. Geol. Surv., Prof. Paper 101, p. 298, PI. 70, fig. 3, 1918. 
* Newberry, J. S., U.S. Geol. Surv., Mon. 35, PI, 43, fig. 4, 1898. 
* Lesquereux, L., Cret. and Tert. FI., p. 194, PI. 42, figs. 14-17, 1883. 
