Proceedings of the California Academy of Sciences, Volume III, 1863-1867Various
Science
Proceedings of the California Academy of Sciences, Volume III, 1863-1867
Various
California Academy of Sciences -- Periodicals; Science -- Periodicals
Stem simple or dichotomous above, minutely velvety glandular
pubescent throughout, upper and cauline leaves lanceolate,
acute or acuminate, sessile or sub-sessile, opposite, erect,
slightly cilliate at base (radical leaves unknown). Flowers
white, very small, sub-solitary on long peduncles; calyx
tubular-campanulate, at length inflated, teeth short, acute
(tipped with purple), tube ten-nerved; petals not crowned,
minute border sub-two-lobed, lamina expanded, claws long and
very slender; stamens ten, longer, at length shorter, filaments
glabrous, anthers sagittate; styles two to three, separate,
recoiled; stigmatose along the entire inner face. Ovary
somewhat globose, apex slightly contracted; compressed seeds
granular, stipe of the capsule very short.
A plant about three to five inches in height.
Collected by Mr. Herbert C. Dorr in Nevada Territory.
Dr. James Blake read a paper on the gradual elevation of the land in the
environs of San Francisco.
On the Gradual Elevation of the Land in the Environs of San Francisco.
BY JAMES BLAKE, M.D., F.R.C.S.
The gradual elevation and depression of large portions of the
earth’s surface has, within the last few years, been attracting
considerable attention from geologists. It is a vast geological
process of which we are the actual spectators, offering us
the most imposing terrestrial phenomenon of which we can be
cognizant, and at the same time affording us some tangible
idea of the vast periods that have been required for bringing
the surface of the earth to its present shape. It is the
general opinion of geologists that the western shore of our
continent is gradually rising. This has been proved to be the
case as regards the southern portion of the continent; but the
following facts, observed in the neighborhood of this city,
afford undoubted evidence that at least this portion of the
northern continent is being gradually elevated above the level
of the ocean.
Public-domain text, read in full here on John Shaqi.
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