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
Of the total number noted, twenty-seven have occurred from San
Luis Obispo south, and of the thirty-two remaining, nine have
been felt in San Francisco at the same time they were observed
at San Luis Obispo, while the remaining twenty-three were felt
at San Francisco and north of that point.
Notwithstanding we have had, what may, perhaps, be considered
a frequency in the recurrence of these phenomena, still there
are but a _very few_ of the total number that would merit a
moment’s consideration south of the twenty-fifth parallel of
north latitude, for there they would be regarded as minor
affairs entirely.
From all the facts in our possession relating to the phenomena
on our coast, it appears that the greatest preponderance in
action and severity of effects, is exerted, for the most part,
south of Point Conception, for, from this place, east, south
and north, to near the Colorado, the most conclusive evidence
exists of very recent volcanic action having been exerted on
rather an extensive scale, and is also still persistent in
several localities within the area named, though in a minor
degree.
It would be interesting to examine the changes of level that
have evidently taken place in this State within the last five
years; but as more extended observations would greatly assist
us in forming conclusions on this subject, I will defer that
portion until a future day.
1856.
At the close of 1855, I presented to the Academy a statement of
the occurrence of earthquakes in this State for that year and a
term of years preceding.
During the year just passed, I have kept a careful record
of these phenomena, which have been noticed in this city,
and other parts of the State, and which will be found below,
with their date, and the hour of the day on which they took
place; they comprise all that have occurred, with perhaps two
exceptions, the dates for which were so obscure as to render
it impossible to determine with accuracy the precise period
of their occurrence. So far as I am informed, those shocks
that have taken place in this State during the past year have
not been marked with more severity than has been usual in
years preceding, frequently amounting to a slight tremor, and
at other times to more distinct movements; three only have
possessed sufficient intensity as to command general attention
during the busy hours of day.
Very few have been noticed by persons who were standing upon
the earth at the period of their occurrence. By far the greater
proportion were observed in high situations from the ground,
and in the more retired parts of the city, or on the alluvial
covering of the country to the west and south.
The total number for the past year is sixteen, and of this
number thirteen were observed between sunset and sunrise.
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