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576 PHIPPs’s JOURNALs
O./ervations made by Dr. Irving of the Heat of the Sea agitated by a Gale of Wind, and that
of the Atmofphere.
SrpremBER the twelfth, the thermometer plunged into a wave of the fea, rofe to 62°
the heat of the atmofphere 50°.
This experiment was frequently repeated during the gale, and it gave nearly the fame
difference. At night, when the weather became moderate, the heat of water thirty fa-
thoms below the furface was 55°; the furface and the atmofphere were 54°
September the twenty-fecond, the fea-water was 60°; the atmofphere 59°: the wind
at S. W., a frefh gale.
Obfervations for determining the Height of a Mountain in Latitude 79° 44! ; by the Baro
4 meter, and Geometrical Meafurement,
Obfervations taken by the Barometer by Dr. Irving.
Avcust the eighteenth, the day remarkably clear.
Inches. -
At fix in the morning, the barometer by the fea-fide ftood at - 30,040
‘The thermometer 50°.
On the fummit of the mountain, about an hour and three quarters
later than the firft obfervation below, - - - 28,266
Thermometer 42°.
At about an hour later at the fame place, - - - 28,258
Thermometer 42°.
By the fea-fide, where the firlt obfervation was made, and about
three hours later, - gots de % “ - 30,032
Thermometer 44°.
Height of the mountain calculated by M. De Luc from the
firft obfervation - - - 1585 feet
From the fecond obfervation - . 1592
Mean - - « - I 588 I
Means ufed to afcertain the Height of the Mountain Geometrically.
A point was fixed upon, in the moft convenient place the ground would aduiit of
between the fummit of the mountain (a well-defined object) and the fea-fide; from
hence, in a right line from the mountain, a ftaff was placed at the fea-fide, by a theodo-
lite made by Ramfden, with two telefcopes and double Vernier divifions. ‘The inftru-
ment was carefully adjufted ; firft, by levelling the ftand with a circular level, and after-
wards the whole inftrument by the crofs levels. From hence(A) at right angles to the
{tation at the fea-fide.(C) and the top of the mountain (E), a bafe was meafured each
way to (B) and (D) of eight lines of feventeen fathom each ; in all, five hundred and
forty-four yards. ‘The divifions of both the Verniers were carefully examined, both at
fetting off the ftation by the fea-fide, and thofe at the extremities of each bafe, the fixed
telefcope being kept directed to the fummit of the mountain, and the moveable one di-
rected at right angles each way, both divifions of the Vernier coinciding exactly. Sta-
tion ftaves were fixed perpendicular by the vertical hair of the telefcope. The altitude
5 of
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