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  2. Mahd adh Dhahab - Wikipedia

    en.wikipedia.org/wiki/Mahd_adh_Dhahab

    It is located in the Medina Province in the Hejaz in Saudi Arabia. Gold was first mined in Arabia c. 30th century BC. A second period of activity was during the Abbasid Caliphate between 750 and 1258. The latest activities, by the Saudi Arabian Mining Company began in 1936 using both open-pit and underground mines at Mahd adh-Dhahab. The Saudi ...

  3. Bir Hima Rock Petroglyphs and Inscriptions - Wikipedia

    en.wikipedia.org/wiki/Bir_Hima_Rock_Petroglyphs...

    It was then noted that the images on the rocks were inscribed with inset into the sandstone formation, dated 300–200 BC. [6] Its rich heritage of rock petroglyphs caught the attention of Saudi Arabia's Department of Antiquities only after 1976 when Jubba and other sites were investigated. One of the expedition members investigating this art ...

  4. Geology of Saudi Arabia - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Saudi_Arabia

    The geology of Saudi Arabia includes Precambrian igneous and metamorphic basement rocks, exposed across much of the country. Thick sedimentary sequences from the Phanerozoic [citation needed] (including sandstone, anhydrite, dolomite, limestone, chert and marl) dominate much of the country's surface and host oil.

  5. Arabian-Nubian Shield - Wikipedia

    en.wikipedia.org/wiki/Arabian-Nubian_Shield

    The Arabian-Nubian Shield (ANS) is an exposure of Precambrian crystalline rocks on the flanks of the Red Sea. The crystalline rocks are mostly Neoproterozoic in age. Geographically – and from north to south – the ANS includes parts of Israel, Jordan, Egypt, Saudi Arabia, Sudan, Eritrea, Ethiopia, Yemen, and Somalia.

  6. Tiger's eye - Wikipedia

    en.wikipedia.org/wiki/Tiger's_eye

    Tiger's eye (also called tiger eye) is a chatoyant gemstone that is usually a metamorphic rock with a golden to red-brown colour and a silky lustre.As members of the quartz group, tiger's eye and the related blue-coloured mineral hawk's eye gain their silky, lustrous appearance from the parallel intergrowth of quartz crystals and altered amphibole fibres that have mostly turned into limonite.

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