Occurrence of Attributes in Original Text

The text related to the cultural heritage 'South China Karst' has mentioned 'Stone' in the following places:
Occurrence Sentence Text Source
UNESCOInscription No Name 1248-001 Shilin Karst - Naigu Stone Forest (xe4xb9x83xe5x8fxa4xe7x9fxb3xe6x9ex97) Shilin Yi Autonomous County 1248-002 Shilin Karst xe2x80x93 Suogeyi Village (xe6x89x80xe5x90x84xe9x82x91xe6x9dx91) Shilin Yi Autonomous County 1248-003 Libo Karst xe2x80x93 Xiaoqijong (xe5xb0x8fxe4xb8x83xe5xadx94) Libo County 1248-004 Libo Karst xe2x80x93 Dongduo (xe6xb4x9exe5xa4x9a) Libo County 1248-005 Wulong Karst xe2x80x93 Qingkou Giant Doline (Tiankeng) (xe7xaex90xe5x8fxa3xe5xa4xa9xe5x9dx91) Wulong County 1248-006 Wulong Karst xe2x80x93 Three Natural Bridges (xe5xa4xa9xe7x94x9fxe4xb8x89xe6xa1xa5) Wulong County 1248-007 Wulong Karst xe2x80x93 Furong Cave (xe8x8ax99xe8x93x89xe6xb4x9e) Wulong County 1248-008 Guilin Karst xe2x80x93 Putao Fenling Yangshuo County 1248-009 Guilin Karst xe2x80x93 Lijiang Fengcong Yangshuo County 1248-010 Shibing Karst Shibing County 1248-011 Jinfoshan Karst Chongqing 1248-012 Huanjiang Karst Huanjiang Maonan Autonomous County
The Shilin (Stone Forest) South China Karst formations scenery Karst limestone stalactites in the Furong Cave.
The Shilin Karst component is in Yunnan province and contains stone forests with sculpted pinnacle columns and is considered the world reference site for pinnacle karst.
The region can be considered the global type-site for three karst landform styles: fenglin (tower karst), fengcong (cone karst), and shilin (stone forest or pinnacle karst).The landscape also retains most of its natural vegetation, which results in seasonal variations and adds to the outstanding aesthetic value of the area.
It includes the stone forests of Shilin, superlative natural phenomena which include the Naigu stone forest occurring on dolomitic limestone and the Suyishan stone forest arising from a lake, the remarkable fengcong and fenglin karsts of Libo, and the Wulong Karst, which includes giant collapse depressions, called Tiankeng, and exceptionally high natural bridges between them, with long stretches of deep unroofed caves.
The stone forests of Shilin developed over 270 million years during four major geological time periods from the Permian to present, illustrating the episodic nature of the evolution of these karst features.