The Khasis by P. R. T. Gurdon
page 28 of 307 (09%)
page 28 of 307 (09%)
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fuel for iron smelting in days gone by. The Government, however, has
taken steps to protect the remaining forests from further spoliation. A remarkable feature is the presence of numerous sacred groves situated generally just below the brows of the hills. In these woods are to be found principally oak and rhododendron trees. The fir-tree (Pinus Khasia) is first met with on the road from Gauhati to Shillong, at Umsning, at an elevation of about 2,500 feet. In the neighbourhood of Shillong the fir grows profusely, but the finest fir-trees are to be seen in the Jowai sub-division. In the vicinity of Nongpoh is observed the beautiful _nahor_ or _nageswar_, the iron-wood tree. The latter is also to be found on the southern slopes of the hills in the Jowai sub-division. There are some _sal_ forests to the west and south of Nongpoh, where the _sal_ trees are almost as large as those to be found in the Garo Hills. Between Shillong and Jowai there are forests of oak, the country being beautifully wooded. Chestnuts and birches are also fairly common. The low hills on the northern and western sides of the district are clad with dense forests of bamboo, of which there are many varieties. The Pandanus or screw-pine is to be met with on the southern slopes. Regarding the geological formation of the hills, I extract a few general remarks from the Physical and Political Geography of Assam. The Shillong plateau consists of a great mass of gneiss, bare on the northern border, where it is broken into hills, for the most part low and very irregular in outline, with numerous outliers in the Lower Assam Valley, even close up to the Himalayas. In the central region the gneiss is covered by transition or sub-metamorphic rocks, consisting of a strong band of quartzites overlying a mass of earthy schists. In the very centre of the range, where the table-land attains its highest elevation, great masses of intrusive diorite and granite occur; and the latter is found in dykes piercing the gneiss and sub-metamorphic series throughout the southern |
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