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
In describing the watershed of this wide region, I may point out
that the area of the lake basin may be defined by those divisions of
the country which give rise to the rivers, creeks, and other waters
flowing into it, and which have their origin for the most part in
the extensive mountain ranges scattered over various parts of the
table-lands.
Although on the most recent maps of the colony only about eight rivers,
namely, the Waitahanui, Hinemaiai, Tauranga, Waimarino, Upper Waikato,
Waihaha, and Waihora, are represented as flowing into the lake, I
found on the western shore, in addition to other smaller streams, the
Kuramanga, Kuratao, Whareroa, Mangakara, Whanganui,[40] Waikino, and
Waikomiko, besides three other streams on the northern shore, the names
of which I was unable to obtain.
It will therefore be seen that there are not less than seventeen rivers
running into this lake, with innumerable smaller streams, while it
should be remarked that the only river or stream of any kind flowing
out of this immense area of water is the Waikato, at the north-east
end. Most of the rivers on the eastern side of the lake receive their
waters from the north-western slope of the Kaimanawa mountains, and
those from the west, from the Tuhua, Hauhungaroa and Hurakia ranges.
Comparatively little water flows into the lake at the northern end,
since the country thereabouts dips mostly in the direction of the
valley of the Waikato. It is in fact at its southern end that the lake
receives its greatest volume of water from the Upper Waikato river,
and its numerous tributaries. This river, rising at an altitude of
7000 feet on the eastern side of Ruapehu, is fed by the snows of that
mountain, and of Tongariro, as well as by the enormous watershed of a
large portion of the Kaimanawa mountains, along the western base of
which it runs in its winding course to the lake, receiving likewise
on its way the eastern streams of the Kakaramea ranges, and the
overflowing waters of Lake Rotoaira, as they descend by the Poutu
river. With but one outlet to relieve it of this tremendous watershed,
it is not surprising that the waters of the lake rise rapidly during
the rainy season, while with the continuance of heavy winds its waves
are lashed into fury, and break upon its shores with the force and roar
of a raging sea.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account