Introduction
Dongwu movement by the marine rise from affected areas of land, Permian Maokou limestone dissolution surface formed by one of the earliest Stone (stone teeth). Late Permian continental Emeishan basalt eruption, covering the early Stone Forest, followed by long-term erosion in the ramp-up raze state.
to a new generation of Paleocene most basalt cap layer was denuded Maokou, Xia handle groups and lime Devonian carbonate rocks and gradually exposed, so that development Stone stratigraphic bit increased soil erosion and surface reconstruction under the karren deepen the wide, stone teeth constantly exposed at the surface, the height of the pillars
beautiful scenic views (16)
increasing. Late Eocene, block movement to make a difference in Shilin area lift (lift liters movement), creating a mountain catchment basins and formation of ancient lake. Lake deposited PALAEOGENE clastic and carbonate rocks, while accelerating the process of the lake of Karst early carbonate rocks.Late Oligocene, the ancient Lake in south and finally disappeared. Under the influence of Tibetan Plateau uplift, since the new century to the Quaternary gradually increased to the current altitude above sea level. During this period, the formation of the Israeli-Palestinian River Valley as a base erosion, corrosion and erosion development newborn Shilin Stone Forest early transformation of the landscape pattern. Since the plurality of deepening experienced geological inheritance, so that different times Stone spatially overlap each other compositions, thus forming various types of pine rock karst topography.
area
pine rock scenic area of 10.25 square kilometers, it belongs to the same size Stone Forest karst scenery, but also characteristics of the two are not the same, such as multi-stone Forest pinnacle size is an isolated form, and pine pinnacle rock plurality of even into - body; stone stone Forest the size of the color is light gray, the color of the stone pine rock Scenic is gray and black.
Location
Pinus thunbergii Rock Scenic Area in Shilin Yi Autonomous County, Luliang County has historically been attached. Qing Emperor Kangxi "Luliang state records," said: "Shimen peak, forty miles along the southwest, names Shimen whistle."
Republic of China "Luliang County draft", said: "Pinnacle and Mount Station, solitary show tall, steep stone base line from all sides, like a lion squatting volts, one hundred thousand odd strange whenever snow. day, jade straight plug the sky, Yao Island, King Lam, natural drawing. "black pine forest rock appeared long before humans came to this world, so it should be said that people already know the" black pine rock "this strange stone, but when the subsistence livelihood for the people and busy time, could not find her ornamental value, as ornamental objects, digging her hair as wild places to eat and firewood for heating situation; cowboy up the mountain where cattle hide and seek . The train pulled into the history of the 20th century, Japan 80's, people solve the problem of food and clothing after, people suddenly found that once people disgust described as "Badlands" and "black pine rock", was originally a place as beautiful as paradise. So that it put aside the veil of Pinus thunbergii Rock Scenic Area, more people came to this ancient and pure side of the Holy Land.