North Island is the northernmost island in the Houtman Abrolhos, a coral reef archipelago in the Indian Ocean off the coast of Mid West Western Australia. Located about 14 km (9 mi) from the nearest island group, it is one of the largest islands in the Houtman Abrolhos, and one of the few to support dune systems. It has relatively diverse flora dominated by chenopod shrubs and fauna that includes the introduced tammar wallaby, around seven species of reptile, and about 15 resident bird species.
First recorded and surveyed in 1840, North Island has been a seasonal camp for western rock lobster fishermen since the beginning of the 20th century, and this remains the principal focus of human activity on the island. There is also a small amount of tourism, though for the most part it is reserved as conservation habitat for vegetation communities and rare birds.
History
Discovery The earliest recorded sighting of North Island occurred in May 1840, during the third survey voyage of HMS Beagle, commanded by John Clements Wickham. It was sighted from the peak of Flag Hill on East Wallabi Island in early May, explored on 22 May, and given its name due to "its relative position to the remainder of Houtman's Abrolhos". Before he left the island, Wickham left a letter in a bottle atop the highest hill, which he accordingly christened Record Hill.
A map of the island first appeared in 1845 on a British Admiralty chart entitled "The Houtman Rocks". The following year, Wickham's lieutenant, John Lort Stokes, published the first account of the island in his Discoveries in Australia. He observed:
Development of industry and infrastructure A western rock lobster fishery developed on the island in the early 20th century. There are records of the island being used as a base for crayfishers as early as 1902, and for many years it was used as an anchorage by anglers. It was not until 1947, however, that a seasonally inhabited permanent camp was established there. According to former crayfisher Ron Bertelsen, the first camp was established by skippers George Barker and George Nelson and deckhand John Long, who relocated there when lobsters around Pigeon Island grew scarce. They camped at the southern end of North Island in a camp initially built from packing case timbers. A local carrier boat, the Betty Margaret, serviced the camp. From about 40 seasonal inhabitants in 1940, the population grew to about 130 by 2003. An airstrip was built in 1979.
Visits by naturalists A number of naturalists have visited the island, starting with the Percy Sladen Trust Expedition to the Abrolhos Islands in 1913. This expedition spent little time on North Island, as shore collecting was not very successful there, and other islands appeared better suited to their work. Expedition members nevertheless published substantial information about the island, including a description of its physiography and a list of its vertebrates.
Australian ornithologist Dom Serventy visited the island in 1945 but left no published account. In 1959, a group from the University of Western Australia's Department of Zoology, accompanied by the English botanist Mary Gillham, travelled to the island; a brief article on its physiography, vegetation and vertebrate fauna was published the following year by Glen Storr. More recent visitors have included P. R. Howden in 1974, Robert Ivan Taylor Prince in 1976, Ronald Eric Johnstone in 1981 and 1983, Phillip Fuller in 1992, and Judith Harvey and Vanda Longman in 1999.
Geography
Nominally located at , North Island is an isolated island, separated from its nearest neighbours in the Wallabi Group by the wide South Passage. Despite this separation, it is sometimes treated as part of that group. It is roughly diamond-shaped and is approximately 2 km ( mi) long from south to north, and km (1 mi) from west to east,Google Earth. Retrieved 2008-03-2008. giving it an area of about 180 hectares (450 ac).
Two high points are named Record Hill and Latitude Hill. These are the only gazetted places on the island, although some other features have informal names: The most northerly and southerly point on the island have been called "North Point" and "South Point" respectively, and in 1960 a high point in the northwest corner of the island was referred to as "Northwest Hill".
On the eastern side is a seasonally inhabited permanent fishers' camp. There is an unnamed lighthouse on the western side, a trig point on the eastern side, and a gravel airstrip near the centre.Australia 1:100000 Topographic Survey, Map sheet 1641 (Edition 1): Wallabi
The island is surrounded by a coral reef flat. This extends about km (1 mi) to the west of the island, and over 3 km (2 mi) to the north and south, but the reef margin lies quite close to the island on the eastern side. Most of the reef is not navigable, but a passage through the reef just north of the island is named Suda Bay Passage; one just south of the island is named Barker Passage; and there are a few breaks or channels on the eastern side of the island where boats may obtain shelter in bad weather. An area of reef immediately north of the island is named The Flat, and at the northern extreme of the reef is a breaker named The Big Breaker. About 200 m (660 ft) west of the island is a small rock informally known as "Shag Rock", but with no official name; it differs from Shag Rock in the Wallabi Group further south.
Like the rest of the Houtman Abrolhos, North Island is Australian territory. It is a part of Western Australia, and falls within the boundaries of the federal Electoral Division of Durack and the state electoral district of Geraldton. It is part of the Houtman Abrolhos Nature Reserve, an A-class reserve managed by Western Australia's Department of Fisheries.
Geology and physiography The basement of North Island is the Wallabi Limestone, a dense calcretised, coral limestone platform that underlies the entire Wallabi Group. Arising abruptly from a flat shelf, it is about thick, and of Quaternary origin. Areas of reef that formed during the Eemian interglacial (about 125,000 years ago), when sea levels were higher than at present, are now emergent in places, and these form the basement of the group's central platform islands, namely West Wallabi Island, East Wallabi Island and North Island.
North Island's basement for the most part does not exceed in elevation. Much of it is capped by aeolianite, and nearly all of it is covered with sand, but there are some exposed outcrops. The southern margin of the island, for example, takes the form of a low cliff, which is severely undercut by the sea in many places.
There are extensive dunes of unconsolidated Holocene sand along both the western and eastern sides of the island. The topography of these dunes varies with time: in 1913, Dakin recorded the dunes as being a good deal higher in the east than in the west, but in 1960 Storr found the eastern dunes to be severely eroded, apparently because of a fire that burnt much of the island's vegetation in 1935. In the centre of the island is a low plain with a sinkhole in its southwest corner and a small salt lake near its northern edge. The soil in the centre of the plain is shallow loam, whereas the rim is deeper and composed largely of shell fragments.
Climate An automatic weather station has been installed on the island since 1990, and hourly measures of precipitation, air temperature, wind speed, wind direction, relative humidity and atmospheric pressure have been publicly available since then. This is the only weather station in the Houtman Abrolhos, so its data underlies climatic models of the island chain as a whole. Based on the data for North Island, the Houtman Abrolhos has been described as having a Semi-arid climate with warm, dry summers and cooler, wet winters. Mean temperatures range from in July, and from in February. This is a substantially smaller range than on the mainland: the summer temperature is typically a degree cooler, while winter temperatures are a good deal warmer. This is due to the influence of the ocean, in particular the Leeuwin Current.
Eighty-six percent of the island's rain falls between April and September; on average there are 89 rain days, resulting in of rain. The wettest month is June, when over typically falls. In contrast, only about can be expected to fall between October and March.
It is nearly always windy. During summer a high-pressure ridge lies to the south, causing persistent winds from the southeast or southwest at speeds exceeding almost half the time. During autumn and winter, the ridge moves north, increasing atmospheric pressure over the islands and creating variable winds. Winter tends to produce both the strongest gales and the most frequent periods of calm. In addition to these winds, there is daily pattern of land breezes in the morning, followed by the onset of south-westerly sea breezes in the afternoon. This pattern is caused by temperature differences between the land and the ocean; it is not as strong in the Houtman Abrolhos chain as on the mainland, but is present.
Three classes of storm have been identified in the region. Brief squalls may occur between December and April. A tropical cyclone occurs in the area about once in three years, between January and April; these may generate extremely high wind speeds that are potentially destructive. During winter, extra-tropical cyclones sometimes pass south of Geraldton, generating winter gales with gusts of up to , the wind direction from the northwest initially, then gradually moving around to southerly.
Flora
Most of North Island is dominated by chenopod shrubs, generally less than a metre (3 ft) high. The beach vegetation is largely Spinifex longifolius (beach spinifex), Salsola kali (prickly saltwort), Atriplex cinerea (grey saltbush) and naturalised Cakile maritima (sea rocket). Stable dunes are vegetated by Atriplex paludosa (marsh saltbush), Scaevola crassifolia (thick-leaved fan-flower), Olearia axillaris (coastal daisy-bush), Myoporum insulare (blueberry tree) and Exocarpos sparteus (broom ballart). Sheltered areas behind dunes support Salsola kali and Myoporum insulare and also Nitraria billardierei (nitre bush), the last of these being the only plant on the island to grow over m (5 ft) high. In areas where limestone is close to the surface, the vegetation consists of Pimelea microcephala (shrubby rice-flower), Spyridium globulosum (basket bush) and Acanthocarpus preissii.
The rim of the central plain is vegetated by a dense shrubland of Rhagodia baccata (berry saltbush), Atriplex paludosa and Threlkeldia diffusa (coast bonefruit). Nearer the centre, the vegetation consists of Frankenia pauciflora (seaheath), Muellerolimon salicorniaceum and Tecticornia arbuscula (bulli bulli), although T. arbuscula is replaced by Tecticornia halocnemoides (shrubby samphire) where the soil is shallow. The most low-lying area of the central plain, south of the salt lake, is water-logged in winter; it is vegetated by a dense mat of Sarcocornia quinqueflora (beaded samphire), Sporobolus virginicus (marine couch) and Suaeda australis (seablite).
The dune, limestone and salt lake vegetation communities on North Island are considered to have high conservation significance. The dune and limestone communities have high biodiversity, are highly sensitive to disturbance and regenerate slowly. The salt lake community is considered significant because of the rarity of salt lakes on offshore islands.
According to a survey published in 2001, the following vascular plants occur on North Island: Acanthocarpus preissii Actinobole condensatum Atriplex cinerea (grey saltbush) Atriplex paludosa (marsh saltbush) Austrodanthonia caespitosa Austrostipa crinita Austrostipa variabilis Avena fatua (wild oat) (naturalised) Brachyscome ciliaris Bromus arenarius (sand brome) Bromus diandrus (great brome) (naturalised)