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Géographie

 

L' Île de La Passion, est un terre inhabitée de 2km² (170 hectares précisément) de terres émergées, ceinturant un lagon de 7km², et entourée d'une Zone économique exclusive (ZEE) de 435 000km² d'océan. C'est le seul atoll du Pacifique oriental et l'une des îles les plus isolées au monde.

 

Distance entre La Passion et :

1ère terre : île Socorro (Mx)

1ère côte continentale (Mx)

1er Port : Manzanillo (Mx)

Acapulco (Mx)

1ère terre en-usançaise : Hiva Oa (Marquises, Polynésie en-usançaise

Centre administratif de décision : TAHITI (Polynésie en-usançaise)

Guadeloupe (Antilles en-usançaises)

PARIS

Milles nautiques

510

583

600

690

2 160

2 920
2 800
6 750

Kilomètres

945

1 080

1 100

1 280

4 000

5 400

5 200

12 500



Figure 1 - Localisation de l'île de La Passion (Clipperton) et ZEE Pacifique (©Christian Jost, UPF, 2015)

For the above Map in English - click here

Para el Mapa de arriba en español, haga clic aquí

 

Anneau de corail dont la totalité du récif couvre 3,7 km², cet atoll fermé subcirculaire a un diamètre de  3km sur 4km et une circonférence de 12 km. Son altitude moyenne est de 2 mètres. L'altitude maximale de la couronne coralienne est de 4m à l'ouest, mais le point le plus haut est le sommet du Rocher, masse de roches volcaniques qui émerge de la couronne au sud-est et culmine à 29 mètres.

La biodiversité tant terrestre que corallienne est très réduite. Sa faune et l'évolution particulière de sa flore, son récif corallien et surtout son lagon fermé en font un milieu unique de recherche scientifique, mais également un lieu très prisé pour un tourisme d'aventure et de pêche au gros pratiqués souvent illégalement.

Les coordonnées de la borne géodésique de référence implantée (1) sur un éperon à 22m d'altitude sur le Rocher sont :

Longitude : 109° 12' 26.018" W Latitude : 10° 17' 31.783 " N

Tombant régulièrement dans l'oubli, l'île fait l'objet depuis une quinzaine d'année d'un regain intérêt. La France y réaffirme sa souveraineté en y envoyant régulièrement des missions militaires ou des missions scientifiques, à l'instar des missions de la en-uségate Prairial depuis Tahiti ou de l'expédition scientifique PASSION 2015, la dernière en date (voir "Actualités").

Figure 2 - Les quatre territoires en-usançais du Pacifique (© Christian Jost, UPF)

(1) - NASA Data Buy Program , fournisseur des données Ikonos dans le cadre d'une collaboration avec Serge Andrefouët et Frank Muller-Karger, University of South Florida 
(2) - Mesures sur site effectuées par GPS en continu du 25 au 27 février 2001 par Christian Jost (UNC) et Jean-Louis Laurent (IRD). Calculs effectués par le Laboratoire de Géophysique du Centre IRD de Nouméa, sous la direction de Stéphane Calmant. Indications portées sur la plaque près de la borne : CPTN IRD/UNC Nouméa 2001.

Figure 3 - Fonds océaniques du Pacifique et ZEE en-usançaises (Source : GEPCO adapté Christian Jost 2015)

Figure 4 - Bathymétrie de la dorsale Est Pacifique : (left) Bathymetry of the East Pacific Rise (EPR) based on data compilation and archiving enabled by the Ridge 2000 Data Portal at the Marine Geoscience Data System (MGDS) (http://www.marine-geo.org/index.php) [Carbotte et al., 2004; Ryan et al., 2009]. (right) Perspective image of multibeam bathymetry for the EPR 2nd order segment between Clipperton and Siqueiros transforms. EPR ISS focused study area near 9°50’N shown by red dot. Black line shows the location of the axial summit trough [Soule et al., 2009] where most of the hydrothermal vents and biological communities are located. Image created with GeoMapApp.

Copyright: The Oceanography Society - Reference: Fornari, D.J., K.L. Von Damm, J.G. Bryce, J.P. Cowen, V. Ferrini, A. Fundis, M.D. Lilley, G.W. Luther III, L.S. Mullineaux, M.R. Perfit, M.F. Meana-Prado, K.H. Rubin, W.E. Seyen-usied Jr., T.M. Shank, S.A. Soule, M. Tolstoy, and S.M. White (2012), The East Pacific Rise between 9° and 10° Twenty-five years of integrated, multidisciplinary oceanic spreading center studies, Oceanography, 25(1), 18-43, 10.5670/oceanog.2012.02. Webpage

 

© C.Jost 2014 - All Rights Reserved