Hoang Tung Stone Garden
Hoang Tung Stone Garden
Hoang Tung Stone Garden
Hoang Tung Stone Garden

Introdution

Price: Free

Phone: (0206) - 3854 211

Time to visit a place: 120 phút

Open Time: 7:00 AM - Close Time: 6:00 PM

Email: sovhtt@caobang.gov.vn

Address: Hoang Tung, Hoa An, Cao Bang Xã Hoàng Tung, Huyện Hoà An, Tỉnh Cao Bằng

Stone Garden is located in Hoang Tung commune, Hoa An district. It is called so because the limestone here has been dissolved and eroded in a special manner. The area contains a multitude of sharp peaks more than 20m high and 10m wide, which are covered by the younger red-brown terrigenous volcanic rocks of Song Hien Formation (T1sh). Hoang Tung stone garden illustrates a piece of the long geological history of the area. Continental spreading during the Triassic period (c.250 million years ago) led to the formation of the so-called intra continental rift (a sort of narrow, elongated sea like the Red Sea at the border between the present day Asia and Africa), resulting in numerous sub-marine volcanoes and sediment deposition, forming thus the so called terrigenous-volcanic rocks on top of the older limestone. These sedimentary-volcanic rocks have helped scientists confirm the existence of the above-mentioned rift. Subsequent weathering and erosion-denudation processes have removed part of these cap rocks while the sharp peaks were formed by flowing water over a long period in the underlying fractured limestone. These special features provide both aesthetic and scientific values to be enjoyed by visitors to the Stone Garden. View more

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Introdution

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Stone Garden is located in Hoang Tung commune, Hoa An district. It is called so because the limestone here has been dissolved and eroded in a special manner.
The area contains a multitude of sharp peaks more than 20m high and 10m wide, which are covered by the younger red-brown terrigenous volcanic rocks of Song Hien Formation (T1sh).
Hoang Tung stone garden illustrates a piece of the long geological history of the area. Continental spreading during the Triassic period (c.250 million years ago) led to the formation of the so-called intra continental rift (a sort of narrow, elongated sea like the Red Sea at the border between the present day Asia and Africa), resulting in numerous sub-marine volcanoes and sediment deposition, forming thus the so
called terrigenous-volcanic rocks on top of the older limestone. These sedimentary-volcanic rocks have helped scientists confirm the existence of the above-mentioned rift.
Subsequent weathering and erosion-denudation processes have removed part of these cap rocks while the sharp peaks were formed by flowing water over a long period in the underlying fractured limestone.

These special features provide both aesthetic and scientific values to be enjoyed by visitors to the Stone Garden.
 

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