By contrast, on the eastern side of the lake wide strips of beach are not uncommon, and the banks, plains, and terrace sides of whitish pumice, though not inconsiderable, are but tame when compared with the dark basaltic and trachytic heights overhanging the deep western waters. Many streams feed Taupo; only one river drains it. It is not astonishing, then, that the Maori believed that in the centre a terrible whirlpool circled round a great funnel down which water was sucked into the bowels of the earth. A variant of this legend was that a huge _taniwha_ or saurian monster haunted the western depths, ready and willing to swallow canoes and canoemen together. The river issuing from Taupo is the Waikato, which cuts through the rocky lip of the crater-lake at its north-east corner. There it speeds away as though rejoicing to escape, with a strong clear current about two hundred yards wide. Then, pent suddenly between walls of hard rock, it is jammed into a deep rift not more than seventy feet across. Boiling and raging, the whole river shoots from the face of a steep tree-clothed cliff with something of the force of a horizontal geyser. Very beautiful is the blue and silver column as it falls, with outer edges dissolving into spray, into the broad and almost quiet expanse below. This waterfall, the Huka, though one of the famous sights of the island, does not by any means exhaust the beauties of the Upper Waikato. A little lower down the Ara-tia-tia Rapids furnish a succession of spectacles almost as fine. There for hundreds of yards the river, a writhing serpent of blue and milk-white flecked with silver, tears and zig-zags, spins and foams, among the dripping reefs and between high leafy rocks, “wild with the tumult of tumbling waters.” Broadly speaking, the Taupo plateau is a region of long views. Cold nights are more often than not followed by sunny days. The clear and often brilliant air enables the eye to travel over the nearer plains and hills to where some far-off mountain chain almost always closes the prospect. The mountains are often forest-clad, the plains and terraces usually open. Here will be seen sheets of stunted bracken; there, wide expanses of yellowish tussock-grass. The white pumice and reddish-brown volcanic clay help to give a character to the colouring very different to the black earth and vivid green foliage of other parts of the island. The smooth glacis-like sides of the terraces, and the sharply-cut ridges of the hills, seem a fit setting for the perpetual display of volcanic forces and an adjunct in impressing on the traveller that he is in a land that has been fashioned on a strange design. Nothing in England, and very little in Europe, remotely resembles it. Only sometimes on the dusty tableland of Central Spain, in Old or New Castile, may the New Zealander be reminded of the long views and strong sunlight, or the shining slopes leading up to blue mountain ranges cutting the sky with clean lines.