Although we did not imagine that the weather would clear so rapidly we determined to seize this, the first opportunity, and to start at once for the ascent.
We were about two miles away from the base, and we had previously determined to hide our packhorse away in the bush, and to ride to the foot of Tongariro with our blankets and tent, make the ascent, and camp at the foot of the mountain at night.
It took just half an hour to saddle up, and get everything prepared, and then, skirting the forest near to which we had been camped, we ascended a hill some 400 feet high, to gain the Waihohonu Valley beyond.
The sun now shone warm and brightly, our course seemed clear, and all was going as merrily as the proverbial marriage-bell, when Turner hastily directed my attention to four mounted Maoris coming across the plains to our rear; but just at the moment we caught sight of them they disappeared behind a low hill. They were some distance off, but they were quite near enough to easily discern us, especially as Turner, with the white tent on his dark pony, formed a conspicuous object. Fortunately we saw no more of the natives, although we watched carefully for some time, but they nevertheless haunted us for days afterwards—during our ascent both of Tongariro and Ruapehu—as we felt fully convinced that they must have seen us, and we were likewise equally sure that they could, if they so wished, follow up our tracks, when, by the marks of the shod horses, they would have at once discovered that we were Europeans. If we had been going in any other direction the circumstances would have been as nothing, but riding as we were straight for Tongariro, we knew that that fact alone was sufficient to excite their suspicion. When we had ridden across the top of the hill we were at once out of sight, and we rode as fast as our weak horses would allow over the scoria ridges which surrounded the base of the cone. We passed on our right an enormous bluff of volcanic rocks, and then descended a steep, precipitous incline strewn with enormous boulders which at some remote age had evidently been hurled from the fiery crater. It was impossible for our horses to walk down this treacherous place with their heavy burdens on their backs, even whilst we led them, so taking them off and putting them on our own shoulders we made the animals follow us, when they picked their way over and around the big stones like cats.
At the foot of the incline we gained the Waihohonu Valley, a wild, desolate-looking ravine with a winding stream running down its centre. To the left, on the opposite side of this watercourse, was a dense forest growth, while on the ground around the tussock grass and dwarfed alpine plants peculiar to this region struggled for life amidst the huge stones and small low scoria hillocks which were dispersed about in a confused but picturesque way. At the end of the cluster of forest towards the mountain a steep wall of lava-like rock rose abruptly up, and ended in high scoria ridges which closed in the valley to the south-west. Looking in a north-easterly direction, the rugged promontories and jagged edges of the broken extinct craters of the lower mountains rose high in the air, piled about in a confused mass, and coloured dark red and black by the effects of the volcanic fires which appeared to have rent and torn them asunder until they had assumed the appearance of embattled walls and crumbling ruins. The whole conformation of this valley, which was nearly two miles in length, assumed a somewhat semicircular appearance, as if, at some period or another, it had formed part of an enormous crater, out of which the gigantic cone that towered thousands of feet above us had ultimately reared its lofty summit. Although the sun shone with a dazzling splendour over us, and a light-green vegetation clothed many of the hills around, and even crept up the steep scoria sides of the great mountain itself, the Waihohonu Valley had a wild, dreary, and parched-up look, as if some fiery breath had but recently swept over it, and it was only just getting cool from the effects of the volcanic fires, which had left stupendous monuments of their work in the enormous lava ridges, which seemed to have cooled suddenly in their molten course down the steep precipices; while the gigantic boulders of black, shining, volcanic rock, which lay scattered about in every direction, looked like tremendous thunderbolts just newly hurled to earth by the hand of Titan. Not a few of these enormous stones appeared to have been rounded by the action of fire, and in some cases to have been partially melted before being sent high into the air from the fiery mouth of the crater, to fall with terrific force into their present positions.
Securing our horses in the scrub, we scrambled for about a mile over huge boulders, and up rough, narrow watercourses, when, ascending a steep spur of the mountain, we reached the base of the great cone near to its south-eastern side, at a point which marked 4000 feet above the level of the sea. Gazing upwards, the steep, clean-cut sides of the tall mountain looked almost precipitous, and it was clear, at a glance, that the task to reach the summit and make the descent by nightfall would be no easy matter. Just at this part of the cone some volcanic disturbance, which had occurred probably ages ago, had poured down a stream of liquid lava, which, cooling, as it were, by some sudden blast, had congealed into a rugged and almost perpendicular ridge of dark, lustrous, adamantine-like rock in its overflow from the summit of the mountain. It was up this precipitous ridge that we had determined to fight our way. When we first began the ascent, the steep climbing told severely on our backs and legs, while the enormous protruding masses of porous lava which fringed the outside portion of the ridge, and over which we had to climb as much by our hands as by our feet, were as sharp as if they had cooled and crystallized but yesterday. Besides the cautious and often dangerous way we had to pick our footing, it was necessary to be careful, in order to avoid the many holes in the lava formation, which were just large enough to receive a man's body, and which, when we threw stones into them, appeared to be of enormous depth. As we climbed higher and higher, the shelving, colossal sides of the mountain seemed to become steeper and steeper, while the summit appeared to get further away at every step we took.
Fortunately the weather kept beautifully clear, and as we mounted gradually upwards, each hundred feet or so disclosed some new and enchanting view of the surrounding country, which lay mapped out beneath us radiant in all the beauties of the creation. At an altitude of 5000 feet we obtained a magnificent view of Mount Egmont, its peaked, snow-clad summit rising like a glittering island above the vapoury cloud that hung around the lower portion of the mountain, which was a little over eighty miles away from our point of observation, the intervening country being formed of a wide expanse of broken, forest-clad ranges of minor elevation, and which appeared, judging from their numerous valleys, to have a general north-westerly and south-easterly bearing. At an altitude of 5900 feet the climbing was very steep, and at 6400 feet we could see open plains in the distance, towards the west, with patches of forest, which gave them a park-like appearance. At 6600 feet, two small blue lakes were distinctly visible immediately below us, situated on the summit of a flat-topped spur, which stretched out from the base of the great cone in the direction of the open plains beyond, while about six miles distant, in the same direction, rose the colossal form of Ruapehu, brilliant in its fleecy mantle of snow, above which its glacier-bound peaks, rising one above the other, shot up in the form of glittering cones high into the calm, clear air. This was the most extended view we had, up to this time, obtained of the mountain king of the North Island, and we gazed upon its stupendous form with increased interest, as it was to be our field of operations for the morrow. Indeed, it was from this elevated point that we carefully observed all the principal physical features of the giant mountain, and laid down our plan of the ascent, which we successfully carried out two days afterwards. At this point, too, we found the last sign of vegetation in the small alpine plant, Gnaphalium bellidioides.[49] At 6950 feet we found enormous icicles adhering to the rocks, the lava ridge up which we had with great difficulty kept our course, became very steep and rugged, while the climbing was exceedingly difficult and tiring. The mass of dark, black lava stood out in some places like a huge wall, and while on one side the thermometer marked 48° Fahr., on the other, where there were big clusters of icicles over a foot long, it indicated 30°. In this way we could enjoy a great variation in temperature at any moment. During the whole ascent we never allowed ourselves more than five minutes' rest at a time, as we knew that a shift of wind, which might occur at any moment, would sweep the clouds over the mountain again, when its steaming vapours would soon envelop it in an impenetrable mist. Tongariro at all times indicates sudden changes in the weather with the accuracy of a well-balanced barometer. When its vapour-cloud coils upward in the form of a feathery palm, the gods are propitious, and sunshine will be the order of the day; when it shoots out in a long streak horizontally from the crater, a change is impending; and when the vapoury cloud gathers round the summit and coils rapidly down the sides of the cone, as it does often with singular rapidity, it is time to look out for squalls. For a long distance up the mountain its rugged sides glittered with icicles, which clustered about the enormous masses of trachytic lava which cropped up everywhere around, while the ground was covered in every direction with a thick coating of frost and frozen snow. At a height of 7000 feet the whole aspect of the cone had a very bare and desolate look, and, besides the enormous boulders we encountered, we passed over a steep slope covered with volcanic conglomerate, which was very treacherous and slippery with sheets of ice. Here we had to go on all fours, and even in this way it was very difficult to keep our equilibrium sufficiently to prevent ourselves from rolling down the precipitous slopes below. We could now smell the sulphurous fumes of the crater as the clouds of steam rolled over us while we clambered over the enormous ice-bound rocks in the direction of the yawning chasm.
We crawled up a frozen, steep incline on to the hot, quaking edge of the great crater, where a grand and curious sight burst upon the view. We gained the rugged summit of the cone at its highest side, but just as we did so the great cloud of steam rolling up from the enormous basin beneath us swept over us in a dense white cloud, and what with the loud bubbling of the boiling springs, the hissing, screeching sound of the great columns of steam as they burst with terrific force from the rocky vents, the unearthly gurglings of the jets of boiling mud as they shot into the air, and the strong sulphurous fumes that pervaded the atmosphere in every direction, we seemed for once in our lives to be standing on the brink of Hades. Mounting a little to the right along the hot soil that smoked beneath our feet, we gained the very topmost point of the mountain, formed by a broken, rugged peak that fell on the inner side with a precipitous descent into the boiling crater below. We were now on the windward side of the steam-cloud, and at an altitude of 7376 feet above the level of the sea.
From this elevated position we had a clear and well-defined view of the whole summit of the mountain, which appeared to be permeated in every direction by a vast thermal action. The steep, broken sides of the enormous crater wound before us in the form of an almost complete circle of nearly a mile in circumference; and it could be plainly seen that, towards its north-western and western sides, it was considerably lower than on the side upon which we stood. Within the great circle, at its northern side, there was a smaller or inner crater of an almost complete rounded form, the sides of which inclined gradually towards its centre in the form of a complete funnel. This minor crater was separated from the larger one only by a narrow ridge or lip. Looking down into the main crater, which appeared to be about 400 feet in depth, its sides, rugged and broken, as it were, by the force of volcanic fires, were built up principally of enormous masses of trachytic rock, lava ridges, and beds of conglomerate, formed mostly of rounded stones and boulders fused together into a compact mass by what must, at some period or another, have been a very powerful igneous action. In fact, it could be plainly seen that the whole volcano when at the height of its eruptive force must have been the seat of a powerful volcanic activity, until gradually its exhausted fires subsided into their present state. In some places the sides of the crater were perpendicular and fell with a sheer descent, while in others they were more disturbed and broken. At the bottom of the crater there were scattered about huge rocky ridges, from the large crevices and fissures of which enormous jets of steam burst forth with a roaring, screeching noise, which echoed from the depths below like the wailings of the condemned. Hot springs sent up streams of boiling water, which ran over the rocks and then lost themselves in the hot, quaking soil, which sent them high into the air again in the form of coiling jets of vapour. Miniature cones of dark, smoking mud rose up in every direction, while around all was a seething, fused mass of almost molten matter, which appeared to require just one or two degrees more of heat to transform it into a lake of liquid lava. In every direction were large deposits of pure yellow sulphur, some of which assumed a rock-like formation; at other places it formed a crust over the steaming earth, and where the thermal action was less intense, the glittering yellow crystals covered the ground like a thick frost. No fire was visible in the crater, nor was there any indication of a very recent volcanic eruption. The whole crater of the mountain was in the state of a very extensive solfatara, which was evidently more active at some periods than at others. The inner or second crater, which likewise sent forth a vast volume of steam from its boiling depths, was in much the same condition of activity as the larger one, only that the deposits of sulphur literally lined its sloping sides with a bright-yellow coating, which came up to the very summit of its rim and looked like a circle of gold beneath the bright rays of the sun, which lit up the feathery steam-clouds in the most brilliant prismatic hues.
We obtained a complete view of all parts of the great mountain, as likewise of the smaller volcanic cones and ridges which lay below. Looking in the direction of the north-east, and down upon the rugged clusters of minor elevations, we could see several extinct craters of considerable size; some perfect in their formation, while others had been rent and distorted by the action of volcanic fires, which had left their marks upon them in the form of enormous lava ridges and extensive deposits of scoria.