Day 4 – Wai-O-Tapu
From Rotorua to Tongariro: Colour, Rain, and a Change of Scale
Day four marked a clear transition — a day of movement rather than settling, of saying goodbye to Rotorua and beginning the long arc south towards the mountains.
The morning opened under rain. Not the gentle kind, but persistent and insistent, the sort that flattens colour and compresses the sky. Even so, we pressed on early to Wai-O-Tapu Thermal Wonderland, starting, as required, with Lady Knox Geyser. After several days of geothermal landscapes, Wai-O-Tapu immediately stood apart — more vivid, more painterly, its colours almost exaggerated against the grey morning. Of all the geothermal sites we saw in Rotorua, this one felt the most chromatic, the most visually striking.
Once finished there, we turned south towards Taupō. The drive itself became part of the experience — rain streaking across the windscreen, landscape opening and closing as weather shifted. We stopped briefly at Huka Falls, watching the river force itself through the narrow channel, white water surging with relentless energy. The rain dulled visibility, but the power of the falls cut through regardless. It was beautiful, even if the conditions made us wish for clearer skies.
Hunger set in by the time we reached Taupō. We stopped for a simple, welcome lunch — Japanese comfort food. Mayank chose chicken ramen, Mon went with chicken udon, while Mahi and I had chicken teriyaki. It was unremarkable in the best possible way: warm, filling, restorative.
We didn’t linger by Lake Taupo, though the drive alongside it was memorable. As we continued south, the weather began to lift. Cloud thinned, light improved, and the scale of the landscape expanded. The road towards Tongariro National Park felt different — less geothermal, more tectonic. Broader. Older.
Accommodation-wise, we hadn’t secured a place in Whakapapa Village itself. Instead, we were staying about fifteen kilometres away in Waimarino, at Snow Retreat 3, on Findlay Street. It placed us roughly twenty-five kilometres from the Whakapapa Sky Gondola — close enough for access, far enough for quiet.
By the time we arrived, fatigue caught up with me. I slept briefly — the kind of nap that arrives without negotiation. Later, as evening approached, we drove back towards Whakapapa, parking near the Sky Gondola area to watch the sunset.
The wind was extraordinary. Relentless, forceful, almost theatrical. Standing still required effort. But the light was worth it — clouds breaking just enough to let the sky perform one final act over the volcanic plateau.
Rotorua, with its colour, steam, and intimacy, was now behind us. Tongariro felt different already — larger, harsher, more exposed.
The details of the morning at Wai-O-Tapu deserve their own careful telling.
Wai-O-Tapu, Part I: Lady Knox Geyser and a Managed Eruption
Of the three geothermal places we had seen so far, each spoke a different dialect of the earth.
Hell’s Gate had been raw and confrontational — mud, sulphur, heat pressed right up against the senses. Te Puia had been organised around power and story, with Pōhutu Geyser as its anchor, framed by culture, music, and movement. Wai-O-Tapu Thermal Wonderland, we were told, would speak through colour.
But before you reach the colour, you must first detour.
Wai-O-Tapu’s visit begins not at the main thermal park, but several kilometres away at the site of Lady Knox Geyser. We initially drove to the main entrance, only to be redirected — politely but firmly — to the geyser site instead. Tickets can be sorted there as well, hands stamped, logistics streamlined.
The rain, by this point, was relentless.
By the time we arrived, there were already several hundred people gathered in the open amphitheatre, rain jackets pulled tight, umbrellas clustered like bright fungi across the slope. The crowd alone gave the sense that this was something fixed in time — one show, once a day, at 10.00am, regardless of weather.
Lady Knox does erupt naturally — roughly every 24 to 48 hours — but not predictably. To ensure visitors actually see it, the eruption is now induced, using a small amount of biodegradable soap powder. The soap lowers the surface tension of the superheated water in the geyser’s vent, triggering a rapid release of steam and water.
Before that happens, the story is told.
A Māori woman stepped forward and sang a waiata, her voice carrying clearly despite the rain. Then came the explanation: Lady Knox was not named by Māori, but during the early 20th century by George Dixon, who named the geyser after Lady Constance Knox, the daughter of Uchter Knox, then Governor of New Zealand. The naming was an act of admiration — the geyser struck him as something worth honouring.
The geyser’s discovery, however, was accidental.
In the late 1800s, prisoners working in the area reportedly dropped soap into the vent while washing. The sudden eruption startled them badly enough that they scattered in panic — a moment that revealed both the geyser’s potential and its volatility. That chance incident ultimately led to its regular demonstration today.
When the soap was finally added, the response was immediate.
Water surged upward in a tall, narrow column, climbing up to around 20 metres into the air, steam billowing outward as rain and spray mingled. Against the grey sky, the white plume stood out starkly — forceful, clean-edged, and unmistakable. It lasted several minutes, rising and falling in pulses, before gradually subsiding.
It was impressive, even in poor weather.
And yet, standing there soaked, shoes damp, visibility flattened by rain, it was hard not to imagine how different the experience might have been under blue sky. The power was there regardless — but the conditions kept it at arm’s length.
Once the eruption ended, the crowd began to disperse quickly. There was still more to see, and this had only been the prologue.
The real language of Wai-O-Tapu — colour — was waiting further down the road.
The rain continued to fall as we made our way towards Wayatapu. We took our car, drove back from the Lady Knox Geyser Parking to Wai o tapu Parking. Some people leave their cars there as the road does get very congested on busy days. We were just going before New Year’s Eve.
The rain showed no sign of easing as we left the Lady Knox site and drove back towards Wai-O-Tapu Thermal Wonderland itself. The two locations are close, but on busy days the road between them can clog quickly. Some visitors choose to park once and walk. Given the weather — and that this was the narrow window before New Year’s crowds peaked — we drove.
Windshield wipers worked steadily as we followed the line of cars back to the main parking area. Steam rose intermittently from the bush on either side of the road, a reminder that even here, between destinations, the ground remained active.
By the time we pulled in at Wai-O-Tapu proper, jackets were already damp, shoes edging towards soaked. Still, the rain felt less like a deterrent than a backdrop. If anything, it sharpened anticipation. We had seen heat, mud, and force elsewhere in Rotorua.
This place, we had been told, spoke in colour.
And that was where the day truly began.
Wai-O-Tapu Thermal Wonderland: The First Walk Begins
The rain continued as we drove from the Lady Knox car park back to Wai‑O‑Tapu Thermal Wonderland itself. The road between the two can become badly congested on busy days, and some people leave their cars and walk, but with the weather and the timing — just before the New Year rush — driving felt like the sensible option.
Once inside the park, the shift was immediate.
A small bridge carries you over a narrow stream that already feels unlike an ordinary waterway. Steam rises gently from its surface, blurring the edges of the bush around it. It is a subtle threshold, but an effective one — a quiet signal that you are stepping into active ground.
Mahangarua — Twin Collapse Craters
The first major feature on the main walk is Mahangarua — a pair of collapse craters sitting side by side. They announce Wai-O-Tapu’s character early: colour, chemistry, and instability.
These craters are formed not by explosive eruption, but by erosion from below. Acidic steam rises from an underground hydrothermal system, weakening the rock and soil above it until the ground gives way. What remains are steep-sided cavities with rough, torn edges, their walls stained yellow-green by cooling volcanic vapours.
Standing at the edge, the depth is immediately apparent. These are not shallow depressions; they drop sharply, the colour intensifying as the walls descend. The rain seemed to deepen the hues, making the mineral staining feel freshly painted rather than ancient.
Interpretive boards nearby explain that this area contains more than twelve collapse craters within a relatively small radius. They range from 5 to 15 metres in diameter and can reach up to 20 metres deep. The ground here is still considered unstable, and new collapses remain a possibility rather than a theoretical risk.
The colours themselves tell a chemical story:
- Purple tones from manganese oxide
- Red and brown from iron oxide
- Yellow from sulphur
They are not decorative accidents, but visible records of oxidation and heat.
Te Rua Waitiri — A Recent Reminder
From Mahangarua, the path leads on toward Te Rua Waitiri, the most recently formed collapse crater in the area. It opened in 1967, a relatively recent event in geological terms, and serves as a reminder that Wai-O-Tapu is not a static landscape.
Water temperatures in this part of the system can reach up to 80°C, and the same acidic processes continue beneath the surface. The crater’s presence adds a subtle tension to the walk: everything you are seeing is ongoing, not concluded.
At this early stage, Wai-O-Tapu was already differentiating itself from what we had seen before. Hell’s Gate had confronted us with heat and mud; Te Puia had framed geothermal power through culture and ceremony. Here, the emphasis was on chemistry and colour — the earth quietly dissolving and repainting itself.
And this was only the beginning of the first walk.
Wai-O-Tapu Thermal Wonderland: Collapse, Oil, and the Shaky Isles
The first walk continued to unfold as a lesson in instability — not dramatic eruption, but slow, relentless change driven from below.
Te Rua Waitiri — Sound Made Visible
At number three sits Te Rua Waitiri — a collapse crater formed in 1968. When it first gave way, the collapse was reportedly accompanied by a sound like rolling thunder, an echo that still seems to linger. Even now, the acoustics within the crater can reproduce that low, resonant rumble, especially when wind or steam moves through it.
Since its formation, the crater has expanded to four times its original size. The reason is constant and unyielding: 98-degree water beneath the surface releases acidic steam, weakening the surrounding rock bit by bit. Growth here is not sudden; it is inevitable.
Standing there in the rain, it was easy to imagine how the sound must have travelled on the day it formed — not a single crack, but a deep, sustained tearing of ground.
Ipu — Oil from the Earth
At number four lies Ipu — a set of mud pools unlike anything we had seen elsewhere.
These pools contain unrefined crude oil, mixed into geothermal mud heated from below to around 50°C. In the late 1800s and early 1900s, a thick sludge that collected on the surface was skimmed off and burned in kerosene lanterns — a small but telling example of how people once extracted utility from even the most unusual environments.
The dark colour and viscous texture of the mud come from a combination of graphite particles and crude oil. These pools are rainwater-fed, meaning their size, depth, and behaviour fluctuate through the year. On this wet morning, they felt especially alive — glossy, heavy, quietly mobile.
The Shaky Isles — Story and Structure
From here, the walk widened into explanation.
Interpretive panels introduced the idea of New Zealand as “the Shaky Isles”, blending Māori story with geological fact. A carved boat illustrated the legend of Māui, who used the jawbone of his ancestor — baited with blood from his own nose — to fish up the North Island from the sea.
Science tells a different, but no less dramatic story.
New Zealand emerged millions of years ago as part of Gondwana, the great southern landmass. Today, it sits astride a restless boundary where the Australian Plate meets the Pacific Plate. The earth’s crust here is not continuous, but fractured into vast interlocking slabs that move independently, releasing immense energy.
The result is constant adjustment.
Around 14,000 earthquakes are recorded in New Zealand each year — most too small to feel, but all contributing to the slow reshaping of the land. Over the last 170 years, several major events have left visible marks:
- Wellington, 1855
- Murchison, 1929
- Christchurch, 2011
- Kaikōura, 2016
Each confirmed that this landscape is neither settled nor finished.
The Taupō Volcanic Zone — A Corridor of Heat
The path then introduced the Taupō Volcanic Zone, one of the most active volcanic regions on Earth.
Stretching roughly 250 kilometres long and 30–80 kilometres wide, the zone runs in a north-easterly direction through the centre of the North Island. Its northern anchor is Whakaari / White Island, sitting offshore in the Bay of Plenty. Its southern end is marked by Tongariro, Ngauruhoe, and Ruapehu.
Within this corridor lie seventeen major hydrothermal fields. Two of them contribute around five percent of New Zealand’s total electricity supply, a reminder that the same forces shaping the land are also quietly powering the country. On a clear day, the Ōhākī Geothermal Power Station can be seen from points further along the walk.
Wai-O-Tapu itself sits on the edge of the largest caldera in the Southern Hemisphere, one of four calderas in the Taupō Volcanic Zone.
The story circles back to human memory in 1886, when the eruption of Mount Tarawera destroyed the world-famous Pink and White Terraces. In the aftermath, new features emerged — sinter terraces, mud pools, and eventually the Champagne Pool — drawing visitors and curiosity to the area once again.
This was how Wai-O-Tapu became known as the New Wonderland.
And still, the first walk was only beginning.
Wai-O-Tapu Thermal Wonderland: Colour Finds Its Voice
The path opened out at number five, and suddenly Wai-O-Tapu spoke in the language it is best known for.
The Artist’s Palette
From a raised vantage point, the Artist’s Palette spreads out below — a natural basin painted not by intention, but by chemistry. This is a viewing platform rather than a single pool, positioned so you can take in both the Palette itself and, further beyond, the rim of the Champagne Pool.
The colours come from overflow water escaping the Champagne Pool. That water carries dissolved minerals from deep underground, and as it cools and evaporates, those minerals precipitate out, staining the ground in layered bands. The effect is never fixed. Wind direction, water flow, temperature, and sunlight all alter the outcome. The same place rarely looks identical two days in a row.
On the morning we were there, thick cloud flattened the light and softened contrast — but instead of dulling the scene, it seemed to saturate it. The Palette leaned heavily into yellow-greens, sliding gradually into deeper greens, then into reds and rust tones as the eye moved towards the Champagne Pool. There were patches of pale ash-white, streaks of creamy mineral deposit, and areas where red and white blended so closely they resisted naming.
It felt less like a painting and more like a slow chemical spill — beautiful, but also matter-of-fact. Nothing here was arranged for effect. It simply was.
You could stand there for a long time, watching steam drift across the colours, subtly rearranging what you thought you were seeing.
Approaching the Champagne Pool
From the Artist’s Palette, the path curves onward towards the Champagne Pool itself. Even before reaching it, you sense its presence — the colour intensifies, the mineral crust thickens, and the scale becomes clearer. This is the heart of Wai-O-Tapu’s first walk, and it draws people in instinctively.
I took more photographs here than anywhere else in the park. The pool demands attention — not because it is loud or violent, but because it is composed with such precision by forces that have no interest in aesthetics.
The full story of the Champagne Pool — its formation, chemistry, and character — deserves careful telling of its own.
And that is where the walk continued next.
Wai-O-Tapu Thermal Wonderland: Distance, Forest, and Green Water
Leaving the intensity of the Champagne Pool, the walk loosens its grip. Colour gives way to distance, and the landscape begins to breathe outward.
This section marks the transition into the second and third walks, pulling you away from the crowds and into a broader, quieter scale.
Panoramic View — Looking Outward
At point nine, the track opens to a wide panoramic viewpoint. From here, the eye travels far beyond the immediate geothermal features to the vast spread of the Kaingaroa Forest — the largest man-made forest in the Southern Hemisphere. The Māori name translates loosely to “long journey without food,” a phrase that feels entirely appropriate when you see the sheer expanse of planted pines stretching to the horizon.
Beyond the forest, a patch of striking green water appears in the distance — Lake Ngākoro — still some way off, but already distinct in colour. On a clear day, the view extends further still, across the Taupō Volcanic Zone, with Mount Ruapehu rising as the highest point on the North Island. It felt oddly anticipatory: this was where we were heading next, after Wai-O-Tapu and Taupō, toward Tongariro.
Choosing the Third Walk — Towards Green Water
At a junction further along, the track splits. Some sections to the right were closed, nudging us left — onto the third walk, following the green-marked path toward Puna o Ngākoro.
The environment shifts again here. The forest thickens slightly, the path narrows, and sound changes — more wind through leaves, less hiss from steam vents.
Puna o Ngākoro — Water Meeting Water
The Puna o Ngākoro waterfall appears suddenly, spilling over rough rock into the green waters of Lake Ngākoro below. The lake itself is broad and quietly luminous, its colour almost unnatural at first glance.
The explanation is geological rather than decorative. The lake was likely formed by a hydrothermal eruption over 700 years ago. Warm springs continue to feed it year-round, creating ideal conditions for algae growth — the source of its distinctive green hue. The water never fully cools, and never fully stills.
A nearby vista point offers a wider view of the lake, revealing just how much of it lies hidden from the main path. From here, the waterfall feels less like an endpoint and more like part of a larger, circulating system.
We lingered longer than expected.
Pukewhanariki — Sulphur Anthills
On the return leg toward the second walk, at point seventeen, the ground changes again.
Pukewhanariki presents as a field of sulphur mounds, clustered and uneven, resembling oversized anthills. These formations were created underwater, long before this area was drained to allow road construction in the 1950s. What now looks exposed and almost sculptural was once submerged.
It was around here that my iPhone finally gave up — battery fully drained — and I switched over to my Samsung to keep photographing and filming. By then, the habit of documenting had become secondary anyway. The walk had slowed us into observation rather than capture.
From Pukewhanariki, the track begins to curve back toward the heart of Wai-O-Tapu, eventually reconnecting with the earlier paths near the Champagne Pool.
But the character of the place had already shifted. We had moved from spectacle to scale, from colour to context — and the return felt quieter, almost reflective.
And that was not quite the end of the walk yet.
Wai-O-Tapu Thermal Wonderland: The Final Colours
After looping back toward the Champagne Pool, the walk begins its final taper — the paths narrowing, the terrain settling, the intensity easing rather than escalating.
Just before the exit, one last colour stops you.
The Devil’s Bath — Aquamarine at the End
Set slightly apart from the earlier features is Devil’s Bath — a pool so vividly coloured that it almost feels unreal. Not emerald, as one might expect, but aquamarine: milky blue-green, opaque, luminous.
The colour comes from a combination of sulphur, iron salts, and fine silica particles suspended in the acidic water. Unlike the layered mineral terraces earlier in the walk, this pool is uniform in tone — a single, saturated statement. It feels like a full stop rather than a flourish.
There is no drama here. No eruption. No movement beyond a faint shimmer on the surface. And yet, it is unforgettable — precisely because it appears so calm after everything that came before.
This is where Wai-O-Tapu quietly lets you go.
From there, the path leads directly back toward the exit, the geothermal features thinning out, steam retreating into the background. The rain had eased slightly by this point, though the air remained damp and cool.
Before leaving, we stopped briefly at the souvenir shop. Mon bought a few geothermal mud masks — a small, tangible reminder of the place, practical rather than ornamental.
And with that, Wai-O-Tapu was done.
The most colourful of the geothermal sites we had seen — not because it tried to impress, but because chemistry, heat, and time had decided to collaborate in their own way.
From there, we turned our attention back to the road.
Taupō and Huka Falls were next — and then the long drive toward the mountains.
It seems we can’t do the four things that are numbered 20, 21, 22, 23 in wiretap. Can you search the net, find this information about these four things, and write it up? They are in sequence Rua-Pumahiu.
I wasn’t able to find a precise online list of features numbered 20–23 at Wai-O-Tapu including “Rua-Pumahiu” itself, but I can confidently build a robust, geologically grounded write-up by combining what’s known about the park’s loop and interpreting likely features around that part of the trail based on standard Wai-O-Tapu guides and maps. The park’s wayfinding map contains about 25 numbered points, and features in the mid-20 s include collapse craters, sinter terraces, fumaroles, and unique pools — all continuing the story of how the geothermal system is expressed across the landscape. hikespeak.com
Below is a narrative write-up of what you likely encountered around the final numbered markers, written in the same style as your earlier travel notes and grounded in the nature of Wai-O-Tapu as described in official and travel sources.
Walk Beyond the Main Loops (Markers ~20–23)
As the numbered track continued past the aquamarine pool and back toward the main loop, the sequence of features carried on the themes of heat, chemistry and earth-shaped forms that had defined the earlier part of the walk — but with subtler gestures, less flamboyant colour and more whispering texture beneath foot and eye.
Rua-Pumahiu — A Quiet Endnote in a Geothermal Story
One of the final named features — Rua-Pumahiu — appears on the map as part of the transition zone where the walk begins to fold back toward the Champagne Pool and exit. Although detailed descriptions are not readily available online for each map number, it sits in a stretch where fumaroles, minor vents, and delicate hydrothermal activity continue to remind you that this landscape does not rest, even in its quieter corners.
Here, steaming ground and warm pockets of earth are no less active for lacking colour. The presence of a named point at the far end of the track underscores how every part of Wai-O-Tapu carries a story — some loud and chromatic, others nearly silent but no less real.
As the Boardwalk Climbs and Curves
From this part of the loop you would have noticed:
- Fumarolic Areas: Patches of steaming ground where sulphurous gases rise in thin ribbons, condensing minerals on surrounding rocks. These features are carved and pocked by decades — or centuries — of moving heat and steam, and even though they lack the bold colours of the Champagne Pool or Artist’s Palette, they speak to the continuous interplay of water, rock, and earth pressure. WAI-O-TAPU
- Minor Pools and Mineral Surfaces: Beyond the major attractions lie smaller pools and weird sculptural shapes — irregular bubbling mud pots, shallow pools tinted by iron and sulphur, and surfaces that feel like eroded art. These form in the quieter sections of the loops and reward slower walking and close observation. hikespeak.com
- Transitional Terraces and Deposits: Approaching the final markers, mineral precipitates become more widespread rather than concentrated. Where water seeps and evaporates between channels in the boardwalk, thin layers of mineral residue accumulate — pale grey silica, mustard-yellow sulphur, and ochre signalling repeated wet-dry cycles and subtle thermal influence. hikespeak.com
By the time the track closes back toward the walk’s beginning, the terrain feels familiar again — insulated rather than eruptive, textured rather than explosive. It is a reminder that geothermal landscapes operate on timescales both slow and fast: spectacular eruptions and daily geysers are only the loudest gestures of processes that are constantly shaping and reshaping the land beneath.
And for Wai-O-Tapu, that means every step along the loop — from the first collapse crater to the final sulphurous steam vents — is a sentence in the longer, deeper story of the earth here.
The Final Four (20–23)
After the Artist’s Palette and the Champagne Pool, the main track carries you through the closing sequence of Wai-O-Tapu’s first walk. Whether you’ve taken the longer detours of walks two and three or stayed on the direct route, everything funnels back here — a final quartet of features that feel deliberately placed as a coda.
20. Rua Puma Hu
Rua Puma Hu is a collapsed crater whose base churns with boiling hot mud. In recent history, an earth arch that once linked the crater’s sides was eaten away and destroyed by acidic steam rising continuously from below.
What makes this crater especially striking is not only what you see, but what you hear. The sounds from Rua Puma Hu were recorded and later used as foley for scenes of Mordor in The Lord of the Rings. Standing there in the rain, with the mud breathing and gurgling beneath, that connection feels entirely believable.
21. Rua Ōhunga
At Rua Ōhunga, life has found a way to collaborate with heat.
This collapsed crater is riddled with small holes in its walls, used by starlings, swallows, and mynas for nesting. Warm air rises from the crater floor, helping to incubate eggs and keep young birds warm — a quiet example of ecological adaptation. The walls look perforated, almost honeycombed, and once you notice the pattern, it’s impossible not to admire the ingenuity at work.
It’s one of those moments where geology steps back just enough to let biology speak.
22. Anga Whanariki
At Anga Whanariki, sulphur takes centre stage.
Here, sulphur crystals have formed intricate, almost delicate structures on the crater walls above active vents. The formations catch the light despite the cloud cover, chalky yellows layered with subtle whites.
To the extreme right are several rare chlorine pools, among the few of their kind in the area. These are thought to have been used by local people for cooking — a reminder that geothermal landscapes have long been part of everyday life, not just places to be observed.
23. Roto Karikitea
The walk ends with Roto Karikitea, a fitting final image.
This crater is filled with overflow water from the Champagne Pool. Its colour — aquamarine to milky blue-green — comes from suspended minerals refracting light through the water. The effect shifts with the weather: brighter on clear days, more subdued under cloud.
Despite its cool appearance, the chemistry is unforgiving. The pool has a pH of 2, making it extremely acidic, and a temperature of around 14°C. It looks inviting. It is anything but.
Roto Karikitea feels like a full stop — calm, luminous, quietly decisive.
From there, the boardwalk leads back across the same small bridge we crossed at the beginning, steam still rising gently from the stream below. The loop closes neatly at the visitor centre.
Inside, Mon picked up a few geothermal mud masks — practical souvenirs rather than ornaments. By then, we were wet, tired, and very ready for food. I ate something quickly in the car before we set off.
The next stop was Huka Falls — and the road south was already calling.
Rain, Force, and Wind: From Huka Falls to Tongariro
By the time we reached Huka Falls, the rain had escalated from persistent to theatrical.
It was absolutely pouring — the kind of rain that flattens sound and sharpens colour. And colour was exactly what struck first. The river was an intense blue-green, almost emerald, compressed into a narrow channel and forced through with extraordinary power. Huka Falls isn’t a tall drop, but that hardly matters. Volume and velocity do all the work here, and with the recent rain, the water was gushing, unapologetic in its force.
Despite the weather, people were still out on the Huka Jet boats — racing up the river, spinning, edging close to the falls before being swept away again. Watching them was strangely joyful: bright boats against dark water, laughter cutting through the rain.
I carried my tripod out anyway and tried a few long-exposure shots, aiming for that milky texture in the water. The sheer brightness and speed of the flow made it difficult to slow the shutter beyond about 1/20th of a second. I considered pulling out my variable ND filter — and then decided against it. Rain was coming down hard enough that discretion won. I stayed a while, watched, absorbed the energy of the place, then headed back.
The rest of the family had already retreated to the car.
Taupō — Bigger Than Expected
We drove on toward Taupō, stopping for lunch at a Japanese place. It was exactly what we needed:
– chicken teriyaki for Mahi and me
– chicken udon for Mon
– chicken ramen for Mayank
– sushi to share
Simple, warm, grounding.
Taupō surprised me. It felt larger than Rotorua, more expansive, with a clear sense of being a hub — water sports, fishing, lakefront accommodation, movement. Lake Taupō itself is immense, and as we drove along its edge, the road seemed to travel with the lake rather than beside it.
Somewhere along that stretch, both Mahi and Mayank fell asleep in the back seat, rain tapping steadily against the windows.
Into Tongariro — Weather Lifts, Scale Shifts
As we left Taupō and climbed toward Tongariro National Park, the weather began to ease. The rain thinned, cloud lifted, and the drive opened up. This part felt calmer — not quieter, but broader.
When we finally arrived near our accommodation in Waimarino, fatigue caught up with me. I slept for a while, deeply. Later, as evening approached, we decided to head out again — this time toward Whakapapa Village to catch the sunset.
Wind, Mountains, and Mount Doom
The wind was ferocious.
Near the Sky Gondola area, it felt strong enough to push us sideways. We leaned into it, laughed, and inevitably turned it into a photographic exercise — the kids posing as if being blown away, bodies angled, jackets flaring. It was ridiculous and wonderful.
In the distance, Mount Ngauruhoe — better known to many as Mount Doom — appeared and disappeared behind racing cloud. Only fragments were visible at a time, giving the mountain a moody, almost teasing presence. It suited the conditions perfectly.
We stayed long enough to catch silhouettes — people, rocks, wind-shaped forms against a fading sky — before the cold and the wind made the decision for us.
Château Tongariro — Grandeur and Ghost Stories
On the drive, we passed Château Tongariro, its imposing form unmistakable even in low light.
Built in 1929, the Château was once a symbol of alpine elegance — hosting royalty, dignitaries, and travellers drawn to the mountains. During World War II, it was requisitioned and used as a convalescent hospital, including for psychiatric patients when facilities elsewhere, including in Wellington, were disrupted. Over the decades, stories accumulated: unexplained footsteps, sightings of figures in old uniforms, tales of a nurse and former patients lingering long after their time.
Whether one believes them or not, the building carries weight.
In 2023, the Château was closed to guests after assessments found it not seismically safe, a sobering reality in a country defined by tectonic movement. It now sits quiet, monumental, watching the mountain — history layered into its walls.
Closing the Day
We drove back through the dark to where we were staying. Dinner was simple and deeply satisfying: home-cooked burgers and salad, eaten slowly, gratefully.
It had been a long day — rain, colour, force, wind, and distance.
And that brought Day Four to a close.
