190 st. Michael's and erandon hilis,
completed by an horizontal line srom Durdham
Downs to the opposite summits os the rocks.
In addition to this evidence I shall adduce
the warm-springs of Clifton, situated between
Brandon hill and St. Vincent's rocks. How are
those springs heated,- which are of the tempera-
ture of 70 degrees by Farenheit's scale, as all
springs of pure water which gush from rocks are
extremely cold ? A subterraneous fire must there-
fore slill exist in this neighbourhood, though
probably at a very great depth beneath them,
yet sufficiently near to produce a very sensible
heat after passing a long dislance through cold
fubfiances.
The last., and as it appears to me conclu-
sive evidence, terrified the inhabitants of Bristol,
on the 1 st of November, 1755, when the wa-
ter of the hot-well became red, perhaps with
the ochre before mentioned, and utterly unfit
for use, and continued so sor some time. This
esfect was produced by the dreadful earthquake
at Lisbon, and demonslrates a remote connec-
tion with the cause of that horrible convulsion
os Nature.
It would be futile to say the concussion of the
earth roosed a cleposit of soil from the sides and
bottom of the spring, and spread it through the
water,
completed by an horizontal line srom Durdham
Downs to the opposite summits os the rocks.
In addition to this evidence I shall adduce
the warm-springs of Clifton, situated between
Brandon hill and St. Vincent's rocks. How are
those springs heated,- which are of the tempera-
ture of 70 degrees by Farenheit's scale, as all
springs of pure water which gush from rocks are
extremely cold ? A subterraneous fire must there-
fore slill exist in this neighbourhood, though
probably at a very great depth beneath them,
yet sufficiently near to produce a very sensible
heat after passing a long dislance through cold
fubfiances.
The last., and as it appears to me conclu-
sive evidence, terrified the inhabitants of Bristol,
on the 1 st of November, 1755, when the wa-
ter of the hot-well became red, perhaps with
the ochre before mentioned, and utterly unfit
for use, and continued so sor some time. This
esfect was produced by the dreadful earthquake
at Lisbon, and demonslrates a remote connec-
tion with the cause of that horrible convulsion
os Nature.
It would be futile to say the concussion of the
earth roosed a cleposit of soil from the sides and
bottom of the spring, and spread it through the
water,