{"id":4654,"date":"2026-09-01T10:34:16","date_gmt":"2026-09-01T08:34:16","guid":{"rendered":"https:\/\/www.minesparis.psl.eu\/musee\/?page_id=4654"},"modified":"2026-09-03T13:45:23","modified_gmt":"2026-09-03T11:45:23","slug":"meteorite-classification","status":"publish","type":"page","link":"https:\/\/www.minesparis.psl.eu\/musee\/en\/the-museum\/collections-eng\/meteorites\/meteorite-classification\/","title":{"rendered":"Meteorite classification"},"content":{"rendered":"\n<div class=\"container bloc-50-50\">\n\t<div class=\"row mt-4\">\n\t\t<div class=\"col-md-6\">\n\t\t\t<h2>How are meteorites classified?<\/h2>\n<p style=\"text-align: justify\">Meteorites are classified into two distinct groups, depending on the nature of the celestial body from which they originated: primitive meteorites (also called undifferentiated meteorites) and differentiated meteorites.<\/p>\n\t\t<\/div>\n\t\t<div class=\"col-md-6\">\n\t\t\t<p><img loading=\"lazy\" decoding=\"async\" class=\"alignnone wp-image-4339\" src=\"https:\/\/www.minesparis.psl.eu\/musee\/wp-content\/uploads\/sites\/29\/2026\/08\/821-Classification-Meteorites-544px-300x137.png\" alt=\"\" width=\"390\" height=\"178\" srcset=\"https:\/\/www.minesparis.psl.eu\/musee\/wp-content\/uploads\/sites\/29\/2026\/08\/821-Classification-Meteorites-544px-300x137.png 300w, https:\/\/www.minesparis.psl.eu\/musee\/wp-content\/uploads\/sites\/29\/2026\/08\/821-Classification-Meteorites-544px.png 544w\" sizes=\"auto, (max-width: 390px) 100vw, 390px\" \/><\/p>\n\t\t<\/div>\n\t<\/div>\n<\/div>\n\n\n<div class=\"container block-full-largeur\">\n\t<div class=\"row mt-4\">\n\t\t<div class=\"col-md-12\">\n\t\t\t<hr \/>\n\t\t<\/div>\n\t<\/div>\n<\/div>\n\n\n<div class=\"container bloc-50-50\">\n\t<div class=\"row mt-4\">\n\t\t<div class=\"col-md-6\">\n\t\t\t<h2>Primitive Meteorites<\/h2>\n<p style=\"text-align: justify\">Primitive meteorites (also called undifferentiated meteorites) originated from a primordial body that retained the original material from which all objects in the Solar System were formed. Grains of silicates and metal are found side by side within them. Chondrites are composed of small, more or less deformed spheres (chondrules) aggregated together. There are four main groups, the two most significant of which are:<\/p>\n<p style=\"text-align: justify\"><span style=\"color: #015d9e\"><strong>\u2013 \u201cordinary chondrites\u201d<\/strong><\/span>\nThey account for nearly 80% of chondrites and consist mainly of olivine, pyroxene, feldspar, iron, nickel, etc.<\/p>\n<p style=\"text-align: justify\"><span style=\"color: #015d9e\"><strong>\u2013 \u201ccarbonaceous chondrites\u201d<\/strong><\/span>\nThey consist of feldspar and carbonaceous elements, and sometimes contain very little iron.<\/p>\n\t\t<\/div>\n\t\t<div class=\"col-md-6\">\n\t\t\t<p><img loading=\"lazy\" decoding=\"async\" class=\"alignnone wp-image-4333\" src=\"https:\/\/www.minesparis.psl.eu\/musee\/wp-content\/uploads\/sites\/29\/2026\/08\/1513_Farmington-chondrite_web-300x225.jpg\" alt=\"\" width=\"590\" height=\"443\" srcset=\"https:\/\/www.minesparis.psl.eu\/musee\/wp-content\/uploads\/sites\/29\/2026\/08\/1513_Farmington-chondrite_web-300x225.jpg 300w, https:\/\/www.minesparis.psl.eu\/musee\/wp-content\/uploads\/sites\/29\/2026\/08\/1513_Farmington-chondrite_web-1024x768.jpg 1024w, https:\/\/www.minesparis.psl.eu\/musee\/wp-content\/uploads\/sites\/29\/2026\/08\/1513_Farmington-chondrite_web-768x576.jpg 768w, https:\/\/www.minesparis.psl.eu\/musee\/wp-content\/uploads\/sites\/29\/2026\/08\/1513_Farmington-chondrite_web.jpg 1200w\" sizes=\"auto, (max-width: 590px) 100vw, 590px\" \/><\/p>\n<p><em>\u201cFarmington\u201d meteorite: ordinary L5 meteorite. Close-up photo of the meteorite, showing visible chondrules (ENSMP 1513). \u00a9 Mus\u00e9e de Min\u00e9ralogie Mines Paris \u2013 PSL \/ L\u2019ECOLE des Arts Joailliers \/ Benjamin Chelly.<\/em><\/p>\n\t\t<\/div>\n\t<\/div>\n<\/div>\n\n\n<div class=\"container block-full-largeur\">\n\t<div class=\"row mt-4\">\n\t\t<div class=\"col-md-12\">\n\t\t\t<hr \/>\n\t\t<\/div>\n\t<\/div>\n<\/div>\n\n\n<div class=\"container bloc-50-50\">\n\t<div class=\"row mt-4\">\n\t\t<div class=\"col-md-6\">\n\t\t\t<h2>Differentiated meteorites<\/h2>\n<p style=\"text-align: justify\">\nThey originate from a differentiated body, meaning that the celestial body was large enough for its original material to melt and then separate into different layers. The Earth, for example, is a differentiated body with a crust, a mantle, and a core.<\/p>\n<p style=\"text-align: justify\"><span style=\"color: #015d9e\"><strong>\u2013 Achondrites<\/strong><\/span>\nThese are meteorites originating from the surfaces of large asteroids or planets. They resemble Earth\u2019s rocks.<\/p>\n<p style=\"text-align: justify\"><span style=\"color: #015d9e\"><strong>\u2013 Iron meteorites (siderites)<\/strong><\/span>\nThese are fragments of asteroid cores. They consist mainly of iron and nickel.<\/p>\n<p style=\"text-align: justify\"><span style=\"color: #015d9e\"><strong>\u2013 Lithosiderites<\/strong><\/span>\nThese are mixed meteorites composed of iron-rich parts (iron and nickel) and silicates. There are two types of lithosiderites: mesosiderites and pallasites.<\/p>\n\t\t<\/div>\n\t\t<div class=\"col-md-6\">\n\t\t\t<p><img loading=\"lazy\" decoding=\"async\" class=\"alignnone wp-image-4332\" src=\"https:\/\/www.minesparis.psl.eu\/musee\/wp-content\/uploads\/sites\/29\/2026\/08\/76760_Pallasite_Esquel_Benj_Chelly_Zoom-300x225.jpg\" alt=\"\" width=\"590\" height=\"443\" srcset=\"https:\/\/www.minesparis.psl.eu\/musee\/wp-content\/uploads\/sites\/29\/2026\/08\/76760_Pallasite_Esquel_Benj_Chelly_Zoom-300x225.jpg 300w, https:\/\/www.minesparis.psl.eu\/musee\/wp-content\/uploads\/sites\/29\/2026\/08\/76760_Pallasite_Esquel_Benj_Chelly_Zoom-1024x768.jpg 1024w, https:\/\/www.minesparis.psl.eu\/musee\/wp-content\/uploads\/sites\/29\/2026\/08\/76760_Pallasite_Esquel_Benj_Chelly_Zoom-768x576.jpg 768w, https:\/\/www.minesparis.psl.eu\/musee\/wp-content\/uploads\/sites\/29\/2026\/08\/76760_Pallasite_Esquel_Benj_Chelly_Zoom-1536x1152.jpg 1536w, https:\/\/www.minesparis.psl.eu\/musee\/wp-content\/uploads\/sites\/29\/2026\/08\/76760_Pallasite_Esquel_Benj_Chelly_Zoom-1300x975.jpg 1300w, https:\/\/www.minesparis.psl.eu\/musee\/wp-content\/uploads\/sites\/29\/2026\/08\/76760_Pallasite_Esquel_Benj_Chelly_Zoom.jpg 1601w\" sizes=\"auto, (max-width: 590px) 100vw, 590px\" \/><\/p>\n<p style=\"text-align: justify\">\u201cEsquel\u201d meteorite: a close-up of the pallasite, showing yellow-green olivine crystals in a metallic matrix (ENSMP 76760). <em>\u00a9 Mus\u00e9e de Min\u00e9ralogie Mines Paris \u2013 PSL \/ L\u2019ECOLE des Arts Joailliers \/ Benjamin Chelly.<\/em><\/p>\n\t\t<\/div>\n\t<\/div>\n<\/div>\n\n\n<div class=\"container block-full-largeur\">\n\t<div class=\"row mt-4\">\n\t\t<div class=\"col-md-12\">\n\t\t\t<hr \/>\n\t\t<\/div>\n\t<\/div>\n<\/div>","protected":false},"excerpt":{"rendered":"","protected":false},"author":4,"featured_media":4335,"parent":2820,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_acf_changed":false,"footnotes":""},"class_list":["post-4654","page","type-page","status-publish","has-post-thumbnail","hentry"],"acf":[],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v28.5 - 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