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In geography, the antipode (/ ˈ æ n t ɪ ˌ p oʊ d, æ n ˈ t ɪ p ə d i /) of any spot on Earth is the point on Earth's surface diametrically opposite to it. A pair of points antipodal (/ æ n ˈ t ɪ p ə d əl /) to each other are situated such that a straight line connecting the two would pass through Earth's center.
Antipodes Islands The Antipodes Islands seen from the north Position relative to New Zealand and other outlying islands Geography Location 860 km southeast of Stewart Island Coordinates 49°40′48″S 178°46′48″E / 49.68000°S 178.78000°E / -49.68000; 178.78000 Archipelago Antipodes Islands Major islands Antipodes, Bollons Area 21 km 2 (8.1 sq mi) Highest elevation 366 m ...
An old castaway hut on the Antipodes Islands.. The islands constituting this ecoregion share a long history of isolation, both from other landmasses and each other. The isolation, combined with harsh climates characterised by low temperatures, strong westerly winds and few hours of sunlight in winter, have resulted in the evolution of many endemic plants and animals, though species richness is ...
Antipodes, points on the Earth's surface that are diametrically opposed; Antipodes Islands, inhospitable volcanic islands south of New Zealand; The Antipodes, a principally British term for Australia and New Zealand (or more broadly the area known as Australasia), based on a rough proximity to the antipode of Britain
The Antipodes, Auckland, Bounty and Campbell Islands are collectively designated the Antipodean Islands in the World Geographical Scheme for Recording Plant Distributions. The Snares Islands / Tini Heke are included with the South Island in New Zealand South under the scheme.
The point antipodal to a given point is called its antipodes, from the Greek ἀντίποδες (antípodes) meaning "opposite feet"; see Antipodes § Etymology. Sometimes the s is dropped, and this is rendered antipode , a back-formation .
The southern margin of the plateau was located next to the continental shelves of the eastern Ross Sea and Marie Byrd Land. [3] There are two systems of magnetic anomalies on the Campbell Plateau: the Stokes Magnetic Anomaly System (SMAS) and the Campbell Magnetic Anomaly System (CMAS). The origin and relationship of these anomalies remain unclear.
Like the North Magnetic Pole, the North Geomagnetic Pole attracts the north pole of a bar magnet and so is in a physical sense actually a magnetic south pole. It is the center of the 'open' magnetic field lines which connect to the interplanetary magnetic field and provide a direct route for the solar wind to reach the ionosphere.