Himalayan Journals — Volume 1: Or, Notes of a Naturalist in Bengal, the Sikkim and Nepal Himalayas, the Khasia Mountains, etc.Hooker, Joseph Dalton
History
Himalayan Journals — Volume 1: 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 degrees, that of
the air varying from 77.5 degrees, 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 degrees at 10 p.m.; and on
the following morning 71.5 degrees in the deepest hole, and
70 degrees in the shallower: that of the external air varied from
71 degrees at 3 p.m., to 57 degrees at daylight on the following
morning. At the latter time I took the temperature of the earth near
the surface, which showed, surface 53 degrees, 1 inch 57 degrees,
2 inches 58 degrees, 4 inches 62 degrees, 7 inches 64 degrees.
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.* [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 degrees
where sheltered from the wind, and 104 degrees 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.
Public-domain text, read in full here on John Shaqi.
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