Himalayan Journals — Complete: Or, Notes of a Naturalist in Bengal, the Sikkim and Nepal Himalayas, the Khasia Mountains, etc.Hooker, Joseph Dalton
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Himalayan Journals — Complete: Or, Notes of a Naturalist in Bengal, the Sikkim and Nepal Himalayas, the Khasia Mountains, etc.
Hooker, Joseph Dalton
Himalaya Mountains -- Description and travel; Natural history -- Himalaya Mountains
The road being highly cultivated, and the Date-palm becoming more
abundant, we encamped in a grove of these trees. All were curiously
distorted; the trunks growing zigzag, from the practice of yearly
tapping the alternate sides for toddy. The incision is just below the
crown, and slopes upwards and inwards: a vessel is hung below the
wound, and the juice conducted into it by a little piece of bamboo.
This operation spoils the fruit, which, though eaten, is small, and
much inferior to the African date.
At Mudunpore (alt. 440 feet) a thermometer, sunk 3 feet 4 inches in the
soil, maintained a constant temperature of 71·5°, that of the air
varying from 77·5°, at 3 p.m., to 62 at daylight the following morning;
when we moved on to Nourunga (alt. 340 feet), where I bored to 3 feet 8
inches with a heavy iron jumper through an alluvium of such excessive
tenacity, that eight natives were employed for four hours in the
operation. In both this and another hole, 4 feet 8 inches, the
temperature was 72° at 10 p.m.; and on the following morning 71·5° in
the deepest hole, and 70° in the shallower: that of the external air
varied from 71° at 3 p.m., to 57° at daylight on the following morning.
At the latter time I took the temperature of the earth near the
surface, which showed,
Surface 53° 1 inch 57° 2 inches 58° 4 inches 62° 7
inches 64°
The following day we marched to Baroon (alt. 345 feet) on the alluvial
banks of the Soane, crossing a deep stream by a pretty suspension
bridge, of which the piers were visible two miles off, so level is the
road. The Soane is here three miles wide, its nearly dry bed being a
desert of sand, resembling a vast arm of the sea when the tide is out:
the banks are very barren, with no trees near, and but very few in the
distance. The houses were scarcely visible on the opposite side, behind
which the Kymore mountains rise. The Soane is a classical river, being
now satisfactorily identified with the Eranoboas of the ancients.[19]
[19] The etymology of Eranoboas is undoubtedly _Hierrinia Vahu_
(Sanskrit), the golden-armed. Sons is also the Sanskrit for _gold._
The stream is celebrated for its agates (Soane pebbles), which are
common, but gold is not now obtained from it.
The alluvium is here cut into a cliff, ten or twelve feet above the bed
of the river, and against it the sand is blown in naked _dunes._ At 2
p.m., the surface-sand was heated to 110° where sheltered from the
wind, and 104° in the open bed of the river. To compare the rapidity
and depth to which the heat is communicated by pure sand, and by the
tough alluvium, I took the temperature at some inches depth in both.
That the alluvium absorbs the heat better, and retains it longer, would
appear from the following, the only observations I could make, owing to
the tenacity of the soil.
2 p.m. Surface 104° 2·5 inches 93° 5 inches 88° Sand at
this depth 78° 5 a.m. Surface 51° 28 inches 68·5°
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