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Kudat formation is originated from deep marine environment. [3] [4] The peninsula is geologically high flanked by deep structural depressions with the northern terrane comprises thick-bedded sandstone with interbeds of silty mudstone and contains calcareous nannofossil of Early Eocene to Middle Eocene that were deposited in deep-water setting in contrast to shallow-marine environments declared ...
Langkawi, officially known as Langkawi, the Jewel of Kedah (Malay: Langkawi Permata Kedah), is a duty-free island and an archipelago of 99 islands (plus five small islands visible only at low tide in the Strait of Malacca) located some 30 km off the coast of northwestern Malaysia and a few kilometres south of Ko Tarutao, adjacent to the Thai border.
The tip as part of the Kudat Peninsula was formed through the Kudat formation in the Early Miocene age. The Kudat formation is divided into three major lithological unit, namely the lower, middle and upper units based on significant changes in the composition of the sediments. [3]
The former name of this river island was Peria Island, peria being the Malay word that means 'bittergourd', alluding to the shape of the island. The name was changed to Duyong, a Malay word that means 'mermaid', after the residents of the island were allegedly reported to see two mermaids landing on its shore.
The Cameron Highlands (Malay: Tanah Tinggi Cameron, Chinese: 金馬崙高原, Tamil: கேமரன் மலை) is a district in Pahang, Malaysia, occupying an area of 712.18 square kilometres (274.97 sq mi).
Kota Kinabalu Wetland Centre is 24 hectares (59 acres) of the only remains of mangrove forest that once existed extensively along the coastal region of Kota Kinabalu, Malaysia.
Minyak Beku Beach Minyak Beku in Batu Pahat District. Minyak Beku is a mukim in Batu Pahat District, Johor, Malaysia. [1]Kampung Minyak Beku is where the famous chiseled rock is located, a big rock about ten feet in size (beside the police station).
Uzbekistan's Variscan Paleozoic basement rock is divided into eight main zones. The Karakum-Tajik microcontinent has four tectonic zones in the metamorphic basement rock.The lower units of the southern Baysoon Unit are mainly late Proterozoic high-pressure metamorphic rocks—mainly meta-ultramafic or meta-acidic, gray and coarse.