{"id":8830,"date":"2022-09-20T13:55:37","date_gmt":"2022-09-20T13:55:37","guid":{"rendered":"https:\/\/rajaampatgeopark.com\/?page_id=8830"},"modified":"2025-12-24T17:13:29","modified_gmt":"2025-12-24T17:13:29","slug":"equator-monument","status":"publish","type":"page","link":"https:\/\/rajaampatgeopark.com\/id\/geopark-center\/equator-monument\/","title":{"rendered":"EQ Equator Monument"},"content":{"rendered":"
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EQUATOR MONUMENT <\/strong><\/h5>\n
OF RAJA AMPAT<\/strong><\/h5>\n<\/div>\n<\/div>\n<\/div>\n
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Lokasi<\/span><\/div>\n<\/th>\n
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Lenmakana Lake – South of Misool<\/span><\/p>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/td>\n<\/tr>\n

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01<\/span>o<\/sup>59\u20191.6\u201dS and 130<\/span>o<\/sup>30\u201954.0\u201dE<\/span><\/p>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/td>\n<\/tr>\n

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Rock association, geological process and history, biology<\/p>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<\/div>\n<\/div>\n<\/div>\n

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EQ<\/p>\n<\/div>\n<\/div>\n<\/div>\n

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Geology<\/p>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n

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Biology<\/p>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n

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Jellyfish Lake, Lenmakana – MIsool<\/em><\/p>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n

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Turbidites located at coordinates 01<\/span>o<\/sup>59\u20191.6\u201dS and 130<\/span>o<\/sup>30\u201954.0\u201dE and interpreted to be of Silurian-Devonian age is supposed to have experienced folding and metamorphosed during tectonic phase before Middle Triassic time. Folding was caused by break-up of the northern part of Gondwana Continent Slates, a low grade metamorphic rock, is scattered on western end of the southern coast of Misool, including some islets off the coast. The unit exposed at Aduwey Village which is called Ligu Metamorphics is the oldest rock exposed at Raja Ampat area.<\/span><\/p>\n<\/div>\n<\/div>\n<\/div>\n

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Kompleks kepulauan kars di tenggara pantai timur Pulau Misool merupakan bentang alam asal-pelarutan yang melibatkan Batu gamping Zaag yang berumur Eosen Tengah hingga Oligosen. Sebuah Atol yang terangkat pada akhir Plistosen membentuk laguna tua yang dikelilingi oleh bukit-bukit batu gamping berbangun kerucut. Selama kurun waktu yang panjang, laguna yang terisolir ini mengalami pengenceran oleh air hujan sehingga salinitas air laut menurun dan berubah menjadi payau. Ubur-ubur laut berwarna kuning yang tidak beracun atau stingless, telah berhabitat didalam laguna dan menyesuaikan diri dengan lingkungannya yang berair payau. Permukaan laguna yang berfluktuasi mengikuti pasang surut laut di perairan di luar laguna ini menunjukkan bahwa sistem percelah-retakan (kekar) yang berada di bawah permukaan laut telah menjaga sirkulasi air di laguna.<\/em><\/p>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n

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Previous Geosite<\/span><\/a><\/div>\n<\/div>\n
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BACK TO 29 GEOSITES CATALOG<\/span><\/a><\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/section>\n<\/div>\n

<\/p>","protected":false},"excerpt":{"rendered":"

EQUATOR MONUMENT OF RAJA AMPAT Location Lenmakana Lake – South of Misool Coordinate 01o59\u20191.6\u201dS and 130o30\u201954.0\u201dE Characteristics Rock association, geological process and history, biology EQ Geology Biology Tourism Jellyfish Lake, Lenmakana – MIsool Turbidites located at coordinates 01o59\u20191.6\u201dS and 130o30\u201954.0\u201dE and interpreted to be of Silurian-Devonian age is supposed to have experienced folding and metamorphosed … <\/p>\n

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