I well remember how universal was the outcry against our attempting to descend the Waimakariri in 1889, upon which occasion we conveyed the canoes up to the head waters in the Southern Alps, and came down ninety miles of rapids at a tremendous rate, going through the celebrated gorge fourteen miles in length. Dixon reached Christchurch in one day—a wonderful feat—but I was not able to accomplish more than half the distance, and took two days over it. This involved a descent of 2,550 feet in altitude from the starting-point.
In the following year the Waimakariri was again navigated by myself and three other kindred adventurous spirits, when a number of fine photographic views of the scenery in the gorge were secured.
The descent of the Waitaki River, however, promised some exciting work, in addition to giving a grand insight into the story of the ancient glacier formation—a subject of great geological interest.
The rainfall in the New Zealand mountain districts is enormously heavy, as much or more than 150 inches per annum being registered in some parts. The rivers consequently carry a phenomenal amount of water for their length, and the calculations as to their discharge give wonderful results. The Clutha River in Otago—the largest river of the South Island— discharges as much water per annum as the Nile! It seems a strange statement to make; but such is the fact, the calculations having been made by competent men.
The day following our return from Aorangi we left the Hermitage at 9 a.m., and by 1 p.m. had begun our exciting journey of 140 miles to the sea.
