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.RUBY MINES DISTRICT
327
it is close to the northern boundary of the District, when it bends
sharply south-west again to meet the Irrawaddy a few miles above
Tigyaing in Katha District. The valley below Myitson is wide and to
a certain extent cultivated, in marked contrast to the country on the
upper course. At Myitson the Shweli is joined on the left by a stream
formed by the junction of the Kin, which rises near Shwenyaungbin in
the Mogok subdivision, and the Nam Mit (Meik); watering the valley
in which the capital of the MSngmit State is situated. Another stream
deserving of mention is the Moybe or Nam Pe, which rises in the
Tawngpeng State, and, after skirting the southern boundary of Mong-
mit and of the District proper, turns south to separate the Hsipaw
State from Mandalay District, finishing its course as the Madaya
chaung.
The whole of the Ruby Mines District is occupied by crystalline
rocks, mainly gneisses, and pyroxene granulites, traversed by grains of
tourmaline-bearing granite. Between Thabeikkyin and Mogok batids .
of crystalline limestone are interbedded with the gneiss,-and from these
the rubies of the District are derived. The stones were formerly
obtained from the limestone itself, but the principal sources now are
the clays and other.debris filling up fissures and caves in the limestone
and the alluvial gravels and clays of the valleys of Mogok and
Kyatpyin. Besides rubies, sapphires and spinels with tourmaline are
found in the alluvium, Graphite occurs in small flakes disseminated
through the limestone, and in a few localities is concentrated in
pockets of considerable size along the junction of the limestones with
the gneiss.
The vegetation is much the same as is described in the article on
the NORTHERN SHAN STATES. In the evergreen tracts it is very
luxuriant.
Tigers and leopards are common and are very destructive to cattle,
Bears, hog, bison, sdmbar, and gyi (barking-deer) are all numerous,
Elephants are found in places, especially in Mongmit territory, and
here and there rhinoceros have been met with.
The Mogok plateau is situated at a high altitude and possesses
a temperate climate well suited to Europeans, the maximum and
minimum temperatures at Mogok averaging 7o° and 37° in' December
and 8o° and 5g° in May, Bernardmyo, a small station io miles to the
north-west of Mogok, and somewhat higher, enjoys a climate colder
and more bracing. It used to be,a military sanitarium, but the troops
have~now been withdrawn from it. The climate of the river-side town-
ships resembles that of Mandalay, but the country farther from the
river. at the foot of the hills is very :malarious. The Mbngmit valley,
too, is unhealthy, but, unlike that of Mogok, is excessively hot. ; The
rainfall varies considerably in the different subdivisions. During the
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