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J See also: steel-blue upper plumage, and the dusky See also: white —in some cases reddening so as almost to
See also: vie with the frontal and gular patches—of the See also: lower parts are well known to every See also: person of observation, as is the markedly forked tail, which is become proverbial of this See also: bird
.
Taking the word swallow in a more extended sense, it is used for all the members of the See also: family Hirundinidae,' excepting a few to which the name See also: martin (q.v.) has been applied, and this family includes from 8o to 10o
See also: species, which have been placed in many different genera
.
The true swallow has very many affines, some of which range- almost as widely as itself does, while others seem to have curiously restricted limits, and much the same may be said of several of its more distant relatives
.
But altogether the family forms one of. the most circumscribed and therefore one of the most natural See also: groups of Oscines, having no near See also: allies; for, though in outward appearance and in some habits the swallows bear a considerable resemblance to swifts (q.v.), the latter belong to a different See also: order, and are not Passerine birds at all, as their structure, both See also: internal and See also: external, proves
.
It has been sometimes stated that the Hirundinidae have their nearest relations in the flycatchers (q.v.) ; but the assertion is very questionable, and the supposition that they are allied to the Ampelidae (cf
.
Waxw1NG), though possibly better founded, has not been confirmed
.
An See also: affinity to the See also: Indian and Australian Artamus (the species of which genus are often known as See also: wood-swallows or swallow-shrikes) has also been suggested but has not been accepted
.
(A
.
N.)
SWALLOW-HOLE, in See also: physical geography the name applied to a cavity resulting from the solution of See also: rock under the See also: action of See also: water, and forming, or having at some See also: period formed, the entrance to a subterranean stream-channel
.
Such holes are See also: common in calcareous (See also: limestone or chalky) districts, or along the See also: line of outcrop of a limestone See also: belt among non-calcareous strata
.
These cavities are also known as sinks, dolinas or butter-tubs, and by otherSee also: local names, and sometimes as pot-holes; the last See also: term, however, is also synonymous with Giant's Kettle (q.v.)
.
See CAVE
.
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