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Lord Howe Island

The island is 375 miles (600 km) east of the continent of Australia and near the boundary between the Lord Howe Rise and the Tasman Basin. The Lord Howe Rise is made of continental crust that was rafted eastward as volcanism at a mid-ocean ridge formed new seafloor and opened the Tasman Basin. Seafloor spreading was active from 80 to 60 million years ago. The Lord Howe seamount chain, defined by coral-capped guyots, continues to the north for 600 miles (1000 km) and is probably the result of the Australia plate moving northward over a stationary hot spot. The Tasman Basin is greater than 4,000 m deep. The Lord Howe Rise is defined by the 2,000 m depth contour. Map from McDougall and others, 1981.

There are often more fish and bird species on Lord Howe Island than people, including visitors. Inscribed on the World Heritage list in December 1982 for its rare collection of plants, birds, marine life and exceptional natural beauty this gem in the Pacific is approximately 2 hours flight from Sydney and Brisbane and one of a handful of places in the world, and one of just four island groups, to be awarded a World Heritage listing.

 
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Lord Howe Island

Located 700 kilometres north-east of Sydney and covering an area of 146 300 hectares, the Lord Howe Island Group comprises Lord Howe Island, Admiralty Islands, Mutton Bird Islands, Ball's Pyramid, and associated coral reefs and marine environments.

Nearly seven million years ago geologic movement of the Lord Howe Rise (an underwater plateau) gave birth to a large shield volcano on its western edge. Over time the sea eroded 90 per cent of the original volcano, leaving the islands that today comprise the Lord Howe Island Group.

Lord Howe Island has a spectacular landscape with the volcanic mountains of Mount Gower (875 m) and Mount Lidgbird (777 m) towering above the sea. The central low-lying area provides a marked contrast to the adjacent mountains and northern hills.

There are 241 different species of native plants, of which 105 are endemic to Lord Howe Island. Most of the island is dominated by rainforests and palm forest. Grasslands occur on the more exposed areas of Lord Howe Island and on the offshore islands. Most of the main island and all of the offshore islands are included in the Lord Howe Island Permanent Park Preserve.

The islands support extensive colonies of nesting seabirds and at least 168 bird species have been recorded either living at, or visiting, the islands. A number of these are rare or endangered.

The endangered woodhen is one of the world's rarest bird species. During this century the population of woodhens experienced a significant decline in numbers as a result of hunting by humans, habitat loss and disturbance by feral animals. Over the last few years a successful captive breeding program and other conservation measures have increased the numbers of these small flightless birds to around 220.

The islands are one of two known breeding areas for the providence petrel, a species that is also found nesting on Phillip Island, near Norfolk Island. They also contain probably the largest breeding concentration in the world of the red-tailed tropicbird, and the most southerly breeding colony of the masked booby.

The waters surrounding Lord Howe Island provide an unusual mixture of temperate and tropical organisms. The reef is the southern most coral reef in the world and provides a rare example of the transition between coral and algal reefs. A marine national park was declared by the State of New South Wales in 1999 to increase protection of the marine environment.

Europeans apparently discovered Lord Howe Island when the island was sighted in 1788 from the British colonial naval vessel HMS Supply, en route from Sydney to the penal colony on Norfolk Island. The first landing was made two months later on the return voyage to Sydney.

By the 1830s there was a small permanent settlement in the lowland area of the main island. The settlers made a living by hunting and fishing, and by growing vegetables, fruit and meat for trade with passing ships.

Pigs and goats, which were introduced to Lord Howe Island for food, later went wild and caused extensive vegetation and habitat changes, threatening populations of native species. Rats arrived on the island in 1918 from a wrecked ship, and have since been responsible for the extinction of five bird species. Over the last decade there have been intensive efforts to control these feral animals and the wild pigs have been successfully eradicated.

Lord Howe Island and its associated islands are under the care, control and management of the Lord Howe Island Board. When carrying out its functions, the Board is required to have particular regard to the World Heritage status of the area and to conserve those values for which the area was listed as a World Heritage property.

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Lord Howe Island
  • Strolling through native Kentia palm and Banyan tree forests or over white-sand beaches.
  • Cycling. Bicycles are the usual way of getting about – who’s in a hurry?
  • Snorkelling over pristine coral reefs, right off the beach.
  • Trekking up Mt Gower, a gruelling but rewarding eight-hour exercise described as one of the best one-day hikes in the world.
  • Exploring the reef. At low tide, grab a pair of sandshoes and walk out on the rock platform to see the coral and fish in the rock pools at Ned's or Middle Beach.
  • Scuba diving. More than 50 sites – teeming with fish, colourful coral and green turtles – attract diving enthusiasts from around the world.
  • Mounts Gower is made of the same caldera-filling, horizontal lava flows that define Mount Lidgbird. The lavas are basaltic in composition. Flows range in thickness from a few meters to 100 feet (30 m). If volcanism associated with the hot spot that created the Lord Howe seamount resumes it will be about 250 miles (400 km) to the south. VolcanoWorld wishes to thank Julian Bielewicz for generously sharing his photographs.
  • Mount Lidgbird (2,548 feet; 777 m) is made of caldera-filling, horizontal lava flows. The caldera wall passes through the northern flanks of the mount. Many of the flows have columnar jointing. The rocks record the rapid filling of a large caldera about 3 miles (5 km) in diameter. The caldera was filled with the lava flows about 6.4 million years ago. This was the most recent volcanic event at Lord Howe Island. Photo courtesy of Julian Bielewicz.
  • Lord Howe Island and Balls Pyramid cap a seamount that rises more than 5,900 feet (1,800 m) from the ocean floor. The seamount has an elliptical-shaped summit that trends to the north-northwest and is about 40 miles (65 km) long. The island is about 6 miles (10 km) long and about 1 mile (1.5 km) wide. A coral reef and lagoon are protected inside the crescent-shape of the island. Map from McDougall and others, 1981.
  • Lord Howe Island is the erosional remnant of a 6.9 million-year old shield volcano. Mount Gower (right) and Mount Lidgbird (left) dominate the south end of the island. Photo courtesy of Julian Bielewicz.
  • Welcome to a small, vibrant community of just over 300 people. Add to this a maximum of 400 tourist beds and Lord Howe is never crowded … with people anyway. But take a short stroll or swim and life positively teems with exotic flora and fauna, much to the delight of human visitors.  
  • Born from avolcanic eruption some seven million years ago, it has the southern-most coral reef in the world. The Island is 11 kms long and barely 2 kms at its widest point. Two-thirds of the island is covered in natural forests, Banyan trees and Kentia palms. The waters are crystal clear, the beaches are pristine, there is no pollution, birds and marine life abound.
  • The pristine waters surrounding world-heritage Lord Howe Island are home to 500 species of fish and 90 species of coral. Its sparkling lagoon is protected by the world's southern-most coral reef creating a spectacular line of white surf against a blue backdrop of the South Pacific ocean. A State Marine Park was declared in 1998 and a Commonwealth Marine Park in 1999.
  • The towering peaks of Mt Lidgbird and Mt Gower dominate the southern tip of the Island. The Last Paradise awaits you.
 
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Getting There

Situated in the South Pacific Ocean, 700km north-east of Sydney, Australia.
Qantaslink operate 32-seat Bombardier Dash 8 aircraft to Lord Howe Island (LDH). Flight time is less than 2 hours from Sydney (SYD) or Brisbane (BNE) (a seasonal service also operates from Port Macquarie) A strict 14kg luggage limit per person applies on all Lord Howe Island flights.
Capella Reservations can assist with flight bookings.
Bombardier Dash 8 aircraft have been operating to Lord Howe Island since 1991 they are one of the few commercial aircraft in Australia capable of landing on the Island’s picturesque but short airstrip.

 
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