The Most Beautiful Natural Wonders in Oceania
32 places in 3 countries · updated 14 October 2026
In short: By our ranking, the most beautiful natural wonders in Oceania are Uluru (Australia), Aoraki / Mount Cook (New Zealand) and Milford Sound / Piopiotahi (New Zealand). The list covers 32 natural wonders in 3 countries. New Zealand has the most, with 16. Last updated 14 October 2026.
Oceania joins two opposite kinds of land. Australia is the flattest and most weathered of the continents: with little mountain building for hundreds of millions of years, its landscape is made of what remains, isolated monoliths, eroded gorges and salt lakes, often glowing red with iron oxide. New Zealand sits on the active boundary between the Pacific and Australian plates, so its land is young and rising, with the Southern Alps, glaciers that descend towards rainforest, fjords and volcanoes.
At the heart of Australia, Uluru rises abruptly from the desert as a single mass of sandstone, sacred to the Anangu people and famous for changing colour at dusk. Kings Canyon cuts sheer walls into the same red country, and Kati Thanda–Lake Eyre, the lowest point in Australia, lies dry for years before rare floods turn it into an inland sea. The Three Sisters in the Blue Mountains, Cradle Mountain in Tasmania and the long galleries of the Jenolan Caves show the gentler, wetter east.
New Zealand answers with height and ice. Aoraki / Mount Cook is the country's highest peak, Franz Josef Glacier comes down almost to the coastal forest, and Milford Sound / Piopiotahi is a glacier-cut fjord walled by mountains. On the beach at Moeraki lie nearly spherical boulders, and Taranaki Maunga stands as a lone symmetrical cone above the western plains.
In this list
| # | Place | Type | Country | UNESCO |
|---|---|---|---|---|
| 1 | Uluru | Rock formation | Australia | |
| 2 | Aoraki / Mount Cook | Summit | New Zealand | |
| 3 | Milford Sound / Piopiotahi | Fjord | New Zealand | |
| 4 | Franz Josef Glacier | Glacier | New Zealand | |
| 5 | Three Sisters (Blue Mountains) | Rock formation | Australia | |
| 6 | Cradle Mountain | Mountain | Australia | |
| 7 | Jenolan Caves | Cave | Australia | |
| 8 | Kings Canyon | Canyon | Australia | |
| 9 | Moeraki Boulders / Kaihinaki | Rock formation | New Zealand | |
| 10 | Kati Thanda–Lake Eyre | Salt flat | Australia | |
| 11 | Wolfe Creek Crater | Impact crater | Australia | |
| 12 | Taranaki Maunga | Volcano | New Zealand | |
| 13 | Pancake Rocks | Rock formation | New Zealand | |
| 14 | Mount Yasur | Volcano | Vanuatu | |
| 15 | Doubtful Sound / Patea | Fjord | New Zealand | |
| 16 | Pinnacles Desert | Rock formation | Australia | |
| 17 | Mitre Peak | Summit | New Zealand | |
| 18 | Castle Hill | Rock formation | New Zealand | |
| 19 | Karlu Karlu / Devils Marbles Conservation Reserve | Rock formation | Australia | |
| 20 | Wave Rock | Rock formation | Australia | |
| 21 | Waitomo Glowworm Caves | Cave | New Zealand | |
| 22 | Pōhutu Geyser | Geyser | New Zealand | |
| 23 | Tnorala (Gosse Bluff) | Impact crater | Australia | |
| 24 | Ōpārara Arch | Natural arch | New Zealand | |
| 25 | Mount Ngauruhoe | Volcano | New Zealand | |
| 26 | Te Waikoropupū Springs | Karst spring | New Zealand | |
| 27 | Totem Pole, Tasmania | Stack | Australia | |
| 28 | Mount Sunday | Rock formation | New Zealand | |
| 29 | Bunda Cliffs | Cliff | Australia | |
| 30 | Pūtangirua Pinnacles | Rock formation | New Zealand |
01 Uluru
Australia25.345° S 131.036° E
Image by Walkerssk from Pixabay For the Aṉangu, the Pitjantjatjara and Yankunytjatjara people of the area, Uluru is not scenery but law. Its caves, waterholes and rock art are tied to Tjukurpa, the body of ancestral stories that governs land and conduct. Some sections of the rock are linked to ceremonies restricted to men or to women, and visitors are asked not to photograph them. European explorers reached the area in the 1870s.
Did you know? Archaeological finds east and west of the rock show that people were living in the area more than 10,000 years ago.
02 Aoraki / Mount Cook
New Zealand43.595° S 170.142° E
Image by kewl from Pixabay Aoraki is the mountain's name in the tradition of Ngāi Tahu, in which an early name for the South Island means Aoraki's canoe. The English name was given in 1851 by Captain John Lort Stokes in honour of James Cook, who never actually saw the peak. Under the Ngāi Tahu settlement of 1998 the official name became Aoraki / Mount Cook, the only one of the renamed places where the Māori name comes first.
Did you know? Under the 1998 settlement the Crown agreed to return the mountain to Ngāi Tahu, who would then gift it back to the nation, though neither transfer has yet taken place.
03 Milford Sound / Piopiotahi
New Zealand44.617° S 167.867° E
W. Bulach · CC BY-SA 4.0 Rain is part of its beauty. With an average of more than 6,400 mm a year, this is the wettest inhabited place in New Zealand, and after heavy rain hundreds of temporary waterfalls stream down the cliffs, some of them a thousand metres long; the smaller ones may be blown into spray before they ever reach the water. Two falls, Lady Bowen and Stirling, run all year.
Did you know? Lady Bowen Falls, at about 162 metres the taller of the two permanent waterfalls, honours the wife of Governor George Bowen, who sailed into the sound in 1871.
04 Franz Josef Glacier
New Zealand43.475° S 170.200° E
Image by RobO100 from Pixabay The reason is the sheer amount of snow and rain: up to fifteen metres of precipitation a year falls on the névé, and that fast supply of ice pushes the glacier far below the snowline. It also makes Franz Josef unusually quick to respond to climate. 5 km. Every few decades meltwater trapped in the ice breaks out in a sudden flood down the valley.
Did you know? When Haast first reached it, the glacier was far longer than today and its ice surface stood about 300 metres higher.
05 Three Sisters (Blue Mountains)
Three Sisters
Australia · 3.2 km from Katoomba33.736° S 150.314° E
Image by anncapictures from Pixabay They are what erosion leaves behind. The Blue Mountains are a raised plateau of Triassic sandstone, and wind, rain and rivers have been cutting it back for millions of years; the Sisters are fragments of the escarpment isolated as the cliff retreated, standing free above the valley.
Did you know? The steep Scenic Railway that carries walkers back up from the valley floor began life as a coal-hauling line for the Katoomba colliery.
06 Cradle Mountain
Australia41.685° S 145.951° E
Bjørn Christian Tørrissen · CC BY-SA 3.0 The country is wild and changeable. Open buttongrass moorland alternates with pockets of rainforest, and the colours change with the seasons: in late April and May the deciduous beech, the fagus – Australia's only native cold-climate deciduous tree, found nowhere but Tasmania – turns from rust to brilliant gold on the slopes.
Did you know? On the summit on 4 January 1910, Gustav Weindorfer declared that the area must become a national park for the people for all time.
07 Jenolan Caves
Australia · 30.4 km from Katoomba33.821° S 150.021° E
GrahamWitt · CC BY-SA 4.0 Long before any European arrived, the area mattered to the Gundungurra and Wiradjuri peoples. A Gundungurra creation story tells of a struggle between Gurangatch, a giant eel-like being, and Mirrigan, a native cat, which shaped the land here, and sick people were carried into the caves to bathe in the underground water. The European story begins around 1838, when James Whalan tracked a livestock thief into the valley.
Did you know? Souvenir collecting and graffiti were banned in 1872 after years in which early visitors damaged the formations with little protection.
08 Kings Canyon
Australia24.258° S 131.563° E
Image by walesjacqueline from Pixabay The rock tells a long story. The upper cliffs are Mereenie Sandstone, laid down roughly 400 million years ago; beneath them sits the older Carmichael Sandstone, and between the two runs a thin band of purple shale that records a change in the ancient environment.
Did you know? About 80 bird species have been recorded in the park, among them spinifex pigeons and zebra finches, along with perenties and rock wallabies.
09 Moeraki Boulders / Kaihinaki
New Zealand · 29.4 km from Oamaru45.345° S 170.826° E
Image by Simon from Pixabay What looks like the work of a sculptor is the work of chemistry. The boulders are septarian concretions: balls of mud, fine silt and clay that were cemented by calcite while they lay in the soft sediment of the sea floor during the Palaeocene, around 60 million years ago.
Did you know? The Katiki Boulders at Shag Point, 19 km to the south, include disc-shaped forms, and some contain bones of mosasaurs and plesiosaurs.
10 Kati Thanda–Lake Eyre
Australia28.667° S 137.167° E
Stephan Ridgway · CC BY 2.0 A true, near-complete fill has happened only three times in about 160 years of records. When it happens, the transformation is total: pelicans, banded stilts and other waterbirds detect the flood and fly in from hundreds of kilometers away, sometimes overnight, to breed explosively while conditions last, before the water disappears again and the boom-bust cycle resets.
Did you know? When more than 4 metres deep the lake is no saltier than the sea, but as the salt crust dissolves during a big flood, mass fish kills follow.
11 Wolfe Creek Crater
Australia19.172° S 127.796° E
Whinqinq Pom · CC BY-SA 2.0 Europeans only found the crater by accident, spotting it from the air in 1947 during a survey flight. Aboriginal people in the region had known it for a great deal longer. In the Djaru language it's called Kandimalal, and it appears in Dreaming stories about a pair of rainbow snakes crossing the desert — one of which is said to have burst up out of the ground at this spot, forming the circular crater as it emerged.
Did you know? The name comes from a nearby creek honouring Robert Wolfe, a prospector and storekeeper of the Halls Creek gold rush; early papers misspelled it Wolf Creek.
12 Taranaki Maunga
New Zealand · 26.7 km from New Plymouth39.296° S 174.065° E
Image by Browser from Pixabay It is a young and still active volcano. Activity here began about 200,000 years ago, and over the past nine thousand years small eruptions have come on average roughly every ninety years; the last took place around 1854. On its southern flank sits a secondary cone, Fanthams Peak or Panitahi, 1,966 metres high, while to the north-west lie the eroded remnants of two much older volcanoes, the Pouākai and Kaitake ranges.
Did you know? The mountain was confiscated from Māori by the colonial government in 1865 and formally returned to the iwi of Taranaki under an act of parliament in 1978.
13 Pancake Rocks
New Zealand42.117° S 171.327° E
Image by Makalu from Pixabay The limestone began as shell debris on the floor of a warm, shallow sea in the Oligocene, around 30 to 22 million years ago, when most of the continent of Zealandia lay underwater. Buried under later sand and mud, it was compacted and cemented into rock, then lifted above the sea by the same crustal movements that raised the Southern Alps.
Did you know? A local sag in the Earth's crust at Punakaiki preserved the limestone layers that erosion stripped from most of the surrounding region.
14 Mount Yasur
Vanuatu19.533° S 169.442° E
Rolf Cosar · CC BY 2.5 The volcano sits on the Vanuatu subduction zone, where the Indo-Australian Plate dives eastward under the Pacific Plate, and that steady supply of magma is why the glow never really goes out. The glow has a place in history too: it is thought to be what drew James Cook towards Tanna in 1774, on the first European visit to the island, and its reputation as the "lighthouse of the Pacific" comes from the same beacon seen from the sea.
Did you know? The crater floor holds three active vents, which take turns throwing out the glowing fragments seen from the rim.
15 Doubtful Sound / Patea
New Zealand45.345° S 167.030° E
Image by holgerheinze0 from Pixabay The main channel branches into three arms, Crooked Arm, Hall Arm and First Arm, walled by mountains that plunge straight into the water and are clothed in dense rainforest. Rain falls heavily here, three to six metres a year, and after a downpour hundreds of temporary waterfalls stream down the cliffs.
Did you know? Browne Falls, which tumbles into the sound, drops more than 600 metres down the mountainside.
16 Pinnacles Desert
The Pinnacles
Australia30.606° S 115.157° E
Image by Redkite from Pixabay The pillars are made of Tamala Limestone, a rock built ultimately from seashells: shell fragments broken up by the sea were blown inland as sand and cemented into limestone dunes. How exactly the pinnacles formed is still argued over.
Did you know? The Nambung River flows into the park and then disappears underground into a cave system within the limestone.
17 Mitre Peak
New Zealand44.633° S 167.856° E
Image by Julius_Silver from Pixabay The drama comes from the fiord itself. Milford Sound, known in Māori as Piopiotahi, runs about 15 km inland from the Tasman Sea between walls of granite that drop almost sheer into water nearly 300 metres deep.
Did you know? Donald Sutherland, Milford Sound's pioneer settler, had insisted that Mitre Peak could not be climbed and disputed Dennistoun's claim.
18 Castle Hill
New Zealand43.229° S 171.716° E
Michal Klajban · CC BY-SA 4.0 The stone was laid down on the floor of a shallow sea some 30 to 40 million years ago, when much of what is now New Zealand lay underwater. Later uplift raised the limestone into the mountains, and rain, frost and wind have since carved it into rounded towers, fins and overhangs. The result sits at around 700 metres, framed by the Torlesse and Craigieburn ranges, with tussock grassland running between the rocks.
Did you know? Nearby Flock Hill hosted the battle scenes of The Chronicles of Narnia: The Lion, the Witch and the Wardrobe (2005).
19 Karlu Karlu / Devils Marbles Conservation Reserve
Australia20.567° S 134.267° E
Iain Whyte ( Iainwhyte ) · CC BY-SA 2.5 The boulders are the exposed top of a large body of granite that formed underground and was later lifted and laid bare. Cracks split the granite into rough rectangular blocks, and over immense spans of time those blocks were rounded off by weathering. Desert extremes play a big part: the rock heats strongly by day and cools at night, and thin outer shells flake away like the skin of an onion, a process called exfoliation.
Did you know? Explorer John Ross reportedly called it the devil's country, joking that he had emptied his bag of marbles here.
More about Karlu Karlu / Devils Marbles Conservation Reserve →
20 Wave Rock
Australia32.444° S 118.898° E
DaHuzyBru · CC BY-SA 4.0 The overhang is a textbook "flared slope". Geologists read it as a shape made underground: the curve was weathered into the granite while it was still buried beneath a laterite-capped land surface, a process that began in the Cretaceous, more than 100 million years ago. When the land later lifted and tilted after Australia separated from Antarctica, erosion stripped the soft cover away and exposed the undercut face as a clean concave curve.
Did you know? More than 100,000 people come to see Wave Rock every year.
21 Waitomo Glowworm Caves
New Zealand38.261° S 175.104° E
Karora · Public domain The cave is formed in Oligocene limestone, laid down under the sea about 30 million years ago from shells, corals and other marine life. It has about 1,300 metres of passages on two levels, joined by a 16-metre shaft called the Tomo. On the upper, drier level are the Blanket, a stalactite sheet so thin that light shows through it, and the Cathedral, the largest chamber, 13 metres high with fine acoustics.
Did you know? Adult glowworm gnats are poor fliers and live only a few days, females up to about 76 hours and males up to about 96.
22 Pōhutu Geyser
New Zealand · 3.6 km from Rotorua38.164° S 176.254° E
Image by Makalu from Pixabay What you are watching is the Taupō Volcanic Zone working just below the surface. Pōhutu sits on Geyser Flat, a terrace of pale silica sinter where seven geysers cluster together, among more than five hundred hot springs in the valley. Its vent is narrow, only about half a metre across, which lets pressure and heat build until the water flashes into steam and bursts out.
Did you know? Nearby Waikite Geyser last erupted in March 1967; in June 1996 water suddenly refilled its vent, but it has not played since.
23 Tnorala (Gosse Bluff)
Gosses Bluff crater
Australia23.821° S 132.308° E
TerryT2 · CC BY-SA 4.0 That original crater has long since worn away. The ring visible today is the central uplift, the rock that rebounded upward at the moment of impact and has proved harder than the ground around it, so erosion has left it standing proud.
Did you know? The ring lies about 212 km north-east of Uluru as the crow flies.
24 Ōpārara Arch
New Zealand41.145° S 172.188° E
Stewart Nimmo · CC BY-SA 4.0 The arch lies in the Ōpārara Basin on the edge of Kahurangi National Park. Here a granite basement some 350 million years old is overlain by a relatively thin layer of limestone deposited around 35 million years ago. Rainfall of up to six metres a year, together with the roots of the dense beech and podocarp forest, has dissolved and broken that limestone into a karst landscape of caves, gorges and arches.
Did you know? Just downstream of the main tunnel stands a shorter but even taller rock arch, about 10 m long and roughly 10 m away from it.
25 Mount Ngauruhoe
New Zealand · 24.4 km from Tūrangi39.157° S 175.632° E
Image by BKD from Pixabay Its outline gives the whole Central Plateau its character. Ngauruhoe stands between Tongariro to the north and the broad snowy bulk of Ruapehu to the south, and from many points around the plateau the three volcanoes line up like a stage set. That stage was used: the cone stood in for Mount Doom in Peter Jackson's Lord of the Rings films.
Did you know? Its magma reservoir is thought to lie only about five kilometres beneath the surface.
26 Te Waikoropupū Springs
New Zealand40.848° S 172.769° E
Kieron Norfield · CC BY 2.0 The source is the Arthur Marble Aquifer beneath the Tākaka Valley, fed by a catchment of around 940 square kilometres that rises to 1,650 metres. Water moves slowly underground, is filtered by tiny aquifer-dwelling animals, and emerges almost free of organic matter.
Did you know? A 1974 television report claimed the springs' output of about 14,000 litres a second could supply a city the size of Boston.
27 Totem Pole, Tasmania
Totem Pole
Australia43.139° S 148.006° E
Ed Dunens · CC BY 2.0 The stack belongs to the dolerite coast of Tasman National Park, proclaimed in 1999, where columnar cliffs rise to around 300 metres above the sea and rank among the highest of their kind in the world. Dolerite is a volcanic rock that cooled slowly from molten magma, contracting into tall, many-sided columns; the sea, wind and salt have worked along these joints, isolating columns from the cliff until one stood alone.
Did you know? His return to complete the climb in 2016, 18 years after the accident, was filmed as Doing It Scared, which won numerous awards.
28 Mount Sunday
New Zealand43.548° S 170.893° E
Jeff Hitchcock from Vancouver, BC, Canada · CC BY 2.0 The hill is a roche moutonnée, a landform shaped by ice. During the Pleistocene the Rangitata Glacier repeatedly flowed down this valley, grinding smooth the upstream side of the rock and plucking away the downstream side, which is why Mount Sunday is gentle on one flank and steep and craggy on its south-eastern face.
Did you know? Samuel Butler ran sheep nearby in the 1860s and set his 1872 novel Erewhon in this landscape.
29 Bunda Cliffs
Australia31.950° S 130.233° E
Lindam333 · CC BY-SA 4.0 The beauty of the place is geological and very plain to read. The cliff face is a cross-section through the Eucla Basin, a thick pile of fossil-bearing limestone laid down on an ancient sea floor during the Cenozoic, now standing in pale horizontal bands above the dark water.
Did you know? The Bunda Cliffs are part of the Great Southern Scarp, which runs for about 820 kilometres along the southern edge of the Nullarbor.
30 Pūtangirua Pinnacles
New Zealand · 39.1 km from Upper Hutt41.447° S 175.246° E
Simeon W from Wellington, New Zealand · CC BY 2.0 Their raw material is old. Some seven to nine million years ago, when sea levels were higher, the Aorangi Range stood as an island, and rivers draining it built broad alluvial fans along its southern shore. The land was later drowned again, and only after the ice ages, as the sea fell back, were these fans of gravel exposed.
Did you know? Braindead, the 1992 zombie comedy that opens among the pinnacles, was directed by Peter Jackson years before he returned here for The Return of the King.
How this list is ranked
Places are chosen for how they look, not for how famous they are: each one has its own description and a photograph credited to its author. The order is a single world ranking that weighs the beauty of the place in curated photography together with how widely it is documented — the number of language editions of its encyclopedia article and how often that article is read in a year. The list is rebuilt as places are added, so the order and the counts on this page are always current.
Questions people ask
- What are the most beautiful natural wonders in Oceania?
- On our list, Uluru (Australia) ranks first, followed by Aoraki / Mount Cook (New Zealand) and Milford Sound / Piopiotahi (New Zealand).
- Which country has the most natural wonders in Oceania?
- In our collection, the most come from New Zealand (16), Australia (15) and Vanuatu (1).
- What is Uluru made of?
- Uluru is made of arkose, a coarse sandstone rich in feldspar. Its red colour comes from iron minerals oxidising on the surface; inside, the rock is grey.
- Is Milford Sound a sound or a fjord?
- Despite its name, Milford Sound / Piopiotahi is a fjord: it was carved by glaciers, not drowned river valleys as a true sound would be. Early European visitors named it before its glacial origin was understood.
- How often does Lake Eyre fill with water?
- Kati Thanda–Lake Eyre fills completely only a few times in a century, after exceptional rains in the interior. Smaller floods are more frequent, and they draw huge numbers of waterbirds to breed.
- How many natural wonders are on this list in Oceania?
- The list covers 32 natural wonders in 3 countries. New Zealand has the most, with 16.