MarketHauraki Gulf
Company Profile

Hauraki Gulf

The Hauraki Gulf is a coastal feature of the North Island of New Zealand. It has an area of 4000 km2, and lies between, in anticlockwise order, the Auckland Region, the Hauraki Plains, the Coromandel Peninsula, and Great Barrier Island. Most of the gulf is part of the Hauraki Gulf Marine Park.

Geography
viewed from Waiheke Island The gulf is part of the Pacific Ocean, which it joins to the north and east. It is largely protected from the Pacific by Great Barrier Island and Little Barrier Island to the north, and by the 80-kilometre-long Coromandel Peninsula to the east. It is thus well protected against all but northern winds. Three large channels join the gulf to the Pacific. Colville Channel lies between the Coromandel Peninsula and Great Barrier, Cradock Channel lies between the two islands, and Jellicoe Channel lies between Little Barrier and the Northland Peninsula. To the north of Auckland several peninsulas jut into the gulf, notably the Whangaparāoa Peninsula. Tiritiri Matangi Island is near the end of this peninsula. Further north, Kawau Island nestles under the Tāwharanui Peninsula. Numerous beaches dot the shores of the gulf, many of them well known for swimming and surfing. During the last glaciation period the gulf was dry land, with the sea level being around 100–110 m (300 ft) lower than at present. During this period, the area was home to two river systems. The first of these was a river formed by two tributaries, the Mahurangi River and Waitematā Harbour (then a river). This river flowed north-east between modern day Little Barrier Island and Great Barrier Island, and emptied into the Pacific Ocean north of Great Barrier Island. The second was a stream formed by the major Hauraki Plains rivers: the Waihou River, Piako River and Waitakaruru River. The Hauraki Plains rivers were met by two tributaries, the Wairoa River to the west from modern-day Clevedon and the Umangawha Stream to the east, at Colville, Coromandel Peninsula. This river flowed north, along the plains, turning east and exiting towards the Pacific Ocean along the modern-day Colville Channel between the Coromandel Peninsula and Great Barrier Island. Firth of Thames At the southern end of the gulf is the wide, relatively shallow Firth of Thames. Beyond this lie the Hauraki Plains, drained by the Waihou River and the Piako River. The Hunua Ranges and hills of the Coromandel Peninsula rise on either side of the Firth. ==History==
History
Traditional Tāmaki Māori histories describe the naming of the gulf. The migratory canoes Tainui and Arawa left Raʻiātea at similar times, and both explored the Bay of Plenty area. The crew of both canoes met at Horuhoru Rock (Gannet Rock), where a ceremony was held in memory for the relatives they had lost on the journey. During the ceremony, a mauri stone brought with them on their voyage named Tīkapa was placed on the island. The name Tīkapa Moana was adopted for the surrounding ocean, and became the name of the gulf. An early visitor to the coast near the Thames was the 150-ton brig Fancy, under the command of Captain Thomas Dell, in December 1795. After three months in the area, the vessel returned to Sydney on 15 March 1795 with a cargo of flax and 200 spars. ==Ecology==
Ecology
Species swims in Waitematā Harbour, with Auckland CBD in the background. Some particular common or known animals include bottlenose and common dolphins, the latter sometimes seen in "super schools" of 300-500 animals or more, while various species of whales and orcas are a relatively common sight. Nearly a third of the world's marine mammal species live in or visit the Marine Park. with a watching vessel.Among larger cetaceans, Bryde's whales are residents and relatively common in the Gulf, and their presence in these busily travelled waters leads to a large number of ship strikes, with sometimes several of the whales dying each year from collisions with shipping vessels or sport boats. The population remaining is estimated to be between 100-200. In recent years, increases in numbers of migrating baleen whales are confirmed long after the end of hunting era. These are humpback whales, southern blue whales, pygmy blue whales, and southern minke whales. Less frequently, fin whales and sei whales are seen as well. For southern right whales, these whales will possibly become seasonal residents in the gulf as the populations recover (one of two of the first confirmed birth records on New Zealand's main islands since after commercial and illegal whalings were recorded at around Milford and Browns Bay in 2012). Sperm whales visit occasionally. Many of the islands are official or unofficial bird sanctuaries, holding important or critically endangered species like kiwi, takahē, brown teal and grey-faced petrel. Centred on the main conservation island of Tiritiri Matangi and Little Barrier Island, numerous bird species that were locally extinct have been reintroduced in the last decades, while there have also been some naturally occurring bird "re-colonisations", especially after introduced pests were removed from breeding and nesting grounds. Environmental damage The gulf is a vibrant natural environment, which has seen significant damage during the 20th and early 21st century from human use. Although major study by the Hauraki Gulf Forum in 2011 found that all environmental indicators were still worsening or stable at problematic levels, voluntary coast clean-up groups have collected about 450,000 litres of litter from the shoreline, although further conservation efforts are required to maintain the environmental integrity of the gulf. Particularly damaging were the introduction of industrialised fishing, with for example snapper fishing peaking in the 1970s at more than 10,000 tonnes a year (though even in the 2000s, private fishing of this species is also a considerable factor, weighing in at 400–800 tonnes a year). This severe overfishing, which unbalanced the marine environment by the removal of a main predator in the food chain, led to further degradation, such as a widespread disappearance of kelp beds as they were overtaken by kina barrens. Other exploitation such as the dredging of the mussel beds of the Firth of Thames, reaching its height in 1961 with an estimated 15 million mussels taken (shortly before collapse of the industry) have led to damage which has not been recovered from forty years later, possibly due to the dredging having destroyed the seafloor, and sediment drainage from the agriculture in the Firth of Thames affecting the mussel's viability. Numerous beaches dot the shores of the gulf, many of them well known for swimming and surfing. Although environmental problems exist around urban areas, with 14 out of 52 beaches in the Auckland Region at least occasionally showing unsafe pollution levels (mostly because of untreated sewage) for bathing, environmental groups are working to clean the beaches and restore their vitality. ==Marine Park==
Marine Park
The Hauraki Gulf was declared a marine park in 2000 by legislative statute. This was accompanied by the formation of the Hauraki Gulf Forum, whose membership includes representatives of local iwi and local authorities in the area surrounding the Hauraki Gulf. The park is distinctly different from other conservation areas of New Zealand not only by being a marine environment, but because it is home to more than one million people along its shores and on its islands. It also contains a number of (above-water) wildlife sanctuaries. == Campaigns ==
Campaigns
LegaSea, a non-profit environmental organisation based in New Zealand, is involved in campaigns to restrict destructive fishing methods in the Hauraki Gulf Marine Park, stretching from Te Ārai, Bream Bay to Waihi Beach, opposing fishing methods such as bottom trawling, Danish seining, and scallop dredging. In 2022, LegaSea established the Hauraki Gulf Alliance, a coalition of environmental organisations and community groups advocating the removal of these practices from the Hauraki Gulf. ==References==
tickerdossier.comtickerdossier.substack.com