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The Former Philippines thru Foreign Eyes by Rudolf Ludwig Carl Virchow;Chas. Wilkes;Fedor Jagor;Tomás de Comyn
page 52 of 732 (07%)
together by a narrow neck of land scarcely three miles broad. Two small
streams which rise nearly in the same spot and pour themselves into
the two opposite gulfs, make the separation almost complete, and form
at the same time the boundary between the province of Tayabas on the
west, and that of Camarines on the east. The western portion, indeed,
consists almost entirely of the first-named district, and the eastern
is divided into the provinces of North Camarines, South Camarines,
and Albay. The first of these three is divided from Tayabas by the
boundary already mentioned, and from South Camarines by a line drawn
from the southern shore of the Bay of San Miguel on the north to the
opposite coast. The eastern extremity of the peninsula forms the
province of Albay; separated from South Camarines by a line which
runs from Donzol, on the south coast, northwards across the volcano
of Mayon, and which then, inclining to the west, reaches the northern
shore. A look at the map will make these explanations clearer.

[The monsoons.] There are two seasons in the Philippines, the wet and
the dry. The south-west monsoon brings the rainy season, at the time of
our summer, to the provinces which lie exposed to the south and west
winds. On the northern and eastern coasts the heaviest downpours take
place (in our winter months) during the north-eastern monsoons. The
ruggedness of the country and its numerous mountains cause, in
certain districts, many variations in these normal meteorological
conditions. The dry season lasts in Manila from November till June
(duration of the north-east monsoon); rain prevails during the
remaining months (duration of the south-west monsoon). The heaviest
rainfall occurs in September; March and April are frequently free from
rain. From October to February inclusively the weather is cool and dry
(prevalence of N.W., N., and N.E. winds); March, April, and May are
warm and dry (prevalence of E.N.E., E., and E.S.E. winds); and from
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