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2018年4月15日 星期日

東平洲

Geography field study trip 3

Ping Chau formation
Early Tertiary sedimentary rocks between approximately 65 and 50 million years old. The Ping Chau Formation is the youngest pre-Quaternary rock unit in Hong Kong.Thinly-bedded dolomitic and calcareous siltstone with rare chert interbeds. The sedimentary rocks of the Ping Chau Formation are interpreted as lacustrine in origin.

香港最年輕的沉積岩–東平洲

[東極海陸之旅] 東平洲環島遊

東平洲oasis trek

海岸生物

東平洲海膽






























2015年4月19日 星期日

東平洲2015 Mirs Bay

東平洲
 

BLUFF HEAD FORMATION -Db  (CEDD)

The oldest stratum in Hong Kong, as proven by existing fossil evidence, is a bed of Devonian sedimentary rock. It is mainly outcropped on both sides of Tolo Channel. Sedimentary pyroclastic rocks found around Pak Sha Tau and Wong Chuk Kok Tsui on the northern shore are called Wong Chuk Kok Tsui Formation. They are primarily sandstone, pebbly sandstone and conglomerate. The best outcropped areas of this formation can be found around Wong Chuk Kok Tsui at the northern tip of the channel. Influenced by the folding and staggering action of geological movements, the beddings are almost vertical. It is a breathtaking sight.

The rich Devonian fossils found in Tolo Channel provide a strong basis for determining geological age and sequence stratigraphy. They also help us understand how Hong Kong's natural environment evolved during that time.  (HK GLOBAL GEOLOGY PARK)



Ping Chau, or Tung Ping Chau to differentiate from Peng Chau, sits in Mirs Bay of the northeastern waters. It is the easternmost outlying island of Hong Kong. This crescent-shaped island, measuring 600 metres long and 200 metres wide, is renowned for strange rock formations. Unlike most other rock types across the territory, the island is made up of sedimentary rock including siltstone, dolomitic siltstone, mudstone and chert. This sedimentary rock strata is known as Ping Chau Formation. 

Many extremely well preserved fossils have been found within the formation. Fossil studies, investigations of rock properties and regional geophysics, as well as research in climatic changes during ancient times have confirmed that this formation is the product of sedimentation which took place in Early Tertiary. Layer upon layer of rock form a bewildering structure. The strata looks just like a huge book, guarding great mysteries of geological history within its numerous pages. Since no sediments after Early Tertiary have successfully solidified into enduring rock, Ping Chau Formation is the youngest rock in Hong Kong's geological history. Tung Ping Chau is a popular holiday destination. Its many fascinating attractions, such as wave erosion landscape, the shale that resembles a layered sponge cake and the unusually flat lay of the island itself, have drawn thousands of visitors to the island.












































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