2021-07-08

Ball’s Pyramid: Australia’s Striking Volcanic Sea Stack

Out in the Tasman Sea, far from Australia’s mainland, a dark column of rock rises sharply from the water. It looks almost too steep and isolated to be real. This is Ball’s Pyramid, a spectacular volcanic sea stack belonging to the Lord Howe Island Group. The first sight of Ball’s Pyramid is particularly difficult to forget. There is no broad shoreline or gentle slope around it. Instead, the rock rises abruptly from the ocean, making it look like a giant piece of the ancient landscape was left standing after everything around it disappeared.

Ball’s Pyramid rising dramatically from the Tasman Sea near Lord Howe Island, Australia
Ball’s Pyramid rises sharply from the Tasman Sea as part of the Lord Howe Island Group World Heritage Area.

Ball’s Pyramid is also part of the Lord Howe Island Group World Heritage Area, which was added to the UNESCO World Heritage List in 1982. UNESCO describes the group as an outstanding example of oceanic islands formed through volcanic activity, with Ball’s Pyramid rising dramatically from the sea.

Where Is Ball’s Pyramid?

Ball’s Pyramid lies in the Tasman Sea, southeast of Lord Howe Island and about 600 kilometres from the New South Wales coast. It is part of the Lord Howe Island Group, a collection of islands, islets and rocky outcrops surrounded by protected marine environments. The NSW Government says the Lord Howe Island Marine Park covers about 460 square kilometres and includes Balls Pyramid and South East Rock. The park was established in February 1999, with its zoning and management rules coming into effect in 2004. The remote location is one reason the pyramid has such a wild appearance. There are no buildings, roads, or developed tourist facilities on the rock itself. From the water, it looks more like an isolated piece of a much larger mountain than an ordinary island.

How Tall Is Ball’s Pyramid?

Ball’s Pyramid rises roughly 550 metres above the ocean, with many references giving a height of about 562 metres. Its steep sides make the rock appear even taller when seen from the surrounding water. The name can be slightly misleading. Ball’s Pyramid is not a pyramid in the geometric sense but rather a steep volcanic sea stack. It is a steep volcanic sea stack, formed as part of the geological history of the Lord Howe Island region.

A Remnant of an Ancient Volcano

The Lord Howe Island Group developed from volcanic activity beneath the ocean. Over a very long period, erosion removed much of the original volcanic structure, leaving behind the islands and rocky remnants seen today. UNESCO describes Ball’s Pyramid as part of an island system developed from submarine volcanic activity and says the landscape demonstrates an advanced stage in the destruction of a large shield volcano. That geological story makes Ball’s Pyramid more interesting than its unusual shape alone suggests. What looks like a solitary rock in the middle of the Pacific is actually a surviving piece of a much older volcanic landscape.
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Ball's Pyramid: World's Largest Volcanic Stack
Ball’s Pyramid — The tallest volcanic sea stack in the world

Ball’s Pyramid and Lord Howe Island

Ball’s Pyramid is closely connected to Lord Howe Island, which is about 23 kilometres away. The two places are part of the same World Heritage landscape. The region is particularly important because of its unusual combination of tropical and temperate environments. Warm and cool ocean currents meet around Lord Howe Island, supporting a remarkably varied marine ecosystem.

The NSW Government notes that the marine park contains more than 500 fish species and over 90 coral species, along with many other marine animals. For this reason, Ball’s Pyramid is not simply an impressive rock. It forms part of a much larger natural environment that has scientific and conservation importance.

Like Lord Howe Island and Lord Howe's Subterranean Mountains, Ball's Pyramid is also located on Lord Howe Ridge and is part of the continent of Zealandia. Around it are several small sites: Observatory Rock and Wheatsheaf are located approximately 800m west-northwest of the island. The shelf is 20 kilometres long and 10 kilometres wide on average, lying at an average depth of 50 metres below sea level. It is separated by a 500-metre-deep underground gorge and another shelf, where Lord Howe Island is located. The walls of the Remnant Block continue to extend below the surface of the water until the shelf.

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Ball's Pyramid: World's Largest Volcanic Stack
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The Strange Story of the Lord Howe Island Phasmid

One of the most fascinating stories connected with Ball’s Pyramid involves a large stick insect called the Lord Howe Island phasmid (Dryococelus australis). The insect was once found on Lord Howe Island but disappeared from the island after rats were introduced in 1918. For years, the species was considered extinct. Then Ball’s Pyramid changed the story.

In the 1960s, climbers discovered dead phasmids on the rocky outcrop. Decades later, researchers found living insects there. Australia’s Department of Climate Change, Energy, the Environment and Water records that live Lord Howe Island phasmids were found on Ball’s Pyramid in 2001, living on the Lord Howe Island tea tree (Melaleuca howeana).

This discovery turned the isolated rock into an important refuge for one of the world’s most unusual insects. UNESCO also highlights the Lord Howe Island phasmid as an iconic species of the World Heritage area and notes its rediscovery on Balls Pyramid.

Can You Visit Ball’s Pyramid?

Ball’s Pyramid is not the kind of place where visitors simply arrive and walk around. Its steep rock faces, remote position and sensitive environment make access very different from visiting a normal island attraction. The Lord Howe Island Marine Park protects the surrounding waters, and management rules govern activities in the area. NSW Government information also identifies Balls Pyramid among the marine park’s protected locations.

Divers can explore parts of the underwater environment around Ball’s Pyramid. The NSW Government notes that Balls Pyramid is among the dive sites associated with the Lord Howe Island Marine Park, where underwater trenches, caves and volcanic drop-offs can be found. For most people, however, seeing Ball’s Pyramid from the sea is the more realistic way to appreciate this remarkable landmark.

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Why Ball’s Pyramid Is So Unusual

What makes Ball’s Pyramid memorable is the combination of shape, isolation and natural history. It rises almost vertically from the ocean and appears completely separate from the surrounding landscape. Yet it is connected to the geological history of Lord Howe Island and forms part of a World Heritage area known for its unusual plants, animals and marine ecosystems.

The story of the Lord Howe Island phasmid adds another layer. A rock that looks barren from a distance became a refuge for a species that had disappeared from its original home. That contrast is perhaps the most striking thing about Ball’s Pyramid. From a distance, it looks like nothing more than a giant piece of volcanic rock. Look closer, and it becomes part of a much bigger story about geology, evolution and survival.

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Ball pyramid
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Frequently Asked Questions About Ball’s Pyramid


What is Ball’s Pyramid?

Ball’s Pyramid is a steep volcanic sea stack in the Tasman Sea and part of the Lord Howe Island Group World Heritage Area.

Where is Ball’s Pyramid located?

It is located about 23 kilometres southeast of Lord Howe Island, off the New South Wales coast of Australia.

How tall is Ball’s Pyramid?

Ball’s Pyramid rises roughly 550 metres above the ocean, with commonly cited measurements placing its height at about 562 metres.

How was Ball’s Pyramid formed?

It is a remnant of the ancient volcanic system that formed the Lord Howe Island Group. Erosion gradually removed much of the original volcanic structure, leaving isolated formations such as Ball’s Pyramid.

What is Ball’s Pyramid famous for?

Apart from its dramatic shape, Ball’s Pyramid is famous for its connection with the Lord Howe Island phasmid, a rare stick insect that was rediscovered alive there in 2001.

Is Ball’s Pyramid part of a World Heritage site?

Yes. Ball’s Pyramid is included within the Lord Howe Island Group World Heritage property, which was inscribed by UNESCO in 1982.

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Pyramid ball
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Ball Pyramid Map

 
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Balls pyramid
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Insect Balls
Ball's pyramid stick insect
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Climbing the pyramids

The Rare Insect of Ball’s Pyramid

Ball’s Pyramid is home to one of the world’s rarest insects, the Lord Howe Island phasmid (Dryococelus australis), a large, flightless stick insect. The species was once common on Lord Howe Island but was thought to have disappeared after black rats arrived there in 1918. Dead phasmids were discovered on Ball’s Pyramid in the 1960s, but scientists did not find living ones until 2001, when three individuals were located on a small Melaleuca howeana shrub.

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Balls pyramid insect

The discovery was especially important because the phasmid had been feared extinct for decades. Today, the species remains critically endangered and survives in the wild on the isolated volcanic outcrop of Ball’s Pyramid. The Australian Government describes it as the world’s largest stick insect, growing to about 12 cm long. Its extremely small natural habitat makes the species particularly vulnerable to habitat changes, invasive species, and other disturbances.

Conclusion

Ball’s Pyramid is one of those places that looks almost unreal when you first see it. A tall wall of volcanic rock rises straight from the Tasman Sea, with no large island surrounding it and very little to soften its outline.

But the rock has a story that goes well beyond its unusual appearance. It is a surviving part of an ancient volcanic landscape and belongs to the protected Lord Howe Island World Heritage area. Its connection with the Lord Howe Island phasmid makes it even more remarkable. From a distance, Ball’s Pyramid may look like an isolated rock in the ocean. In reality, it is a small but important part of a much larger story involving volcanoes, wildlife and the long natural history of Lord Howe Island.

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