The King Country; or, Explorations in New Zealand: A Narrative of 600 Miles of Travel Through Maoriland.Kerry-Nicholls, J. H. (James Henry)
History
The King Country; or, Explorations in New Zealand: A Narrative of 600 Miles of Travel Through Maoriland.
Kerry-Nicholls, J. H. (James Henry)
New Zealand -- Description and travel
All the country within the existing range of thermal action, and, in
fact, considerably beyond it, bears the distinctive traces of the
combined work of fire and water, while the ground for miles around is
covered with silicious and sulphurous deposits, together with pumice,
scoria, obsidian, alum, oxide of iron, and various other products, the
result of the igneous and aqueous action which is everywhere observable
in the form of geysers, hot springs, boiling mud-holes, _solfataras_,
and _fumaroles_, and which are known to the natives under the more
general terms of _ngawha, puia_, and _waiariki_.[18] All the geysers
and most of the springs are intermittent, while not a few are very
erratic in their movements, subsiding in one place and breaking out
in another with wonderful rapidity. The water of some of the springs
is as blue and as bright as crystal, in others it is of a greenish
tint, while in not a few it assumes a dirty yellow colour. Nearly
every spring possesses properties peculiar to itself, and mostly all
are more or less efficacious in the treatment of rheumatic and nervous
complaints, and cutaneous and spinal disorders.
[Illustration: NATIVE VILLAGE.
(_Lake Rotoiti_).
_Page 62._]
Upon analysis, the springs are found to contain various chemical
ingredients, but in different proportions, according to the quality or
properties of the water. Among the principal chemical bodies may be
mentioned the chlorides of sodium, potassium, lithium, calcium, and
magnesium; the sulphates of soda, lime, potash, magnesia, alumina,
and iron; the silicates of soda, lime, and magnesia. In the acids,
hydrochloric, sulphuric, and muriatic are found in abundance, while
both sulphuretted hydrogen and carbonic acid gas are largely evolved.
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