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Pearl Shoal Waterfall

Pearl Shoal Waterfall
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Pearl Shoal Waterfall Facts

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Pearl Shoal Waterfall Physical Description

The staggering beauty of the Pearl Shoal Waterfall perfectly demonstrates one very specific and well-known principle. That’s the fact that beauty isn’t dependent upon physical size. That’s because of the fact that the wondrous cascade has a moderate height.

Nevertheless, Nature did bless the geological feature with other amazing vital statistics. These include boasting a very respectable total width. This breathtaking wonder of Nature possesses an upper level with an average width measuring about 550 ft (163 m).

That particular dimension, however, frequently changes within a small range. This variability naturally occurs due to the simple fact that rainfall amounts in the region vary. Its drop also merits a certain amount of respect, since it measures around 130 ft 940 m).

None of these are why Pearl Shoal Waterfall earns its fame. In fact, that originates with the action that happens as it descends. The water of the site flows over a series of uniquely placed outcroppings. This action creates an incredible interlocking pattern of flows.

The water flowing over the wonder appears crystal clear and turquoise in color, which contrasts beautifully with the greenery and the surrounding landscape. A number of terraced pools also appear at the bottom of the waterfall, accentuating its great beauty.

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Pearl Shoal Waterfall Location, Formation, and Ecology

It’s not surprising at all that the magnificent Pearl Shoal Waterfall formed in a region of the earth already renowned for numerous beautiful natural sites. That statement holds true due to the fact that this tantalizing flow of water formed on the continent of Asia.

Even more precisely, though, this waterfall resides in what now constitutes the region now known as the Sichuan Province. That area further lies within China. This magnificent marvel of geology also helps play a role of relative importance within its region.

The formation of this remarkable creation of time and natural processes spans a great deal of that time. It also combined numerous forces. Most of those, however, involved various forma and amounts of limestone and the unique hydrological conditions of the region.

The valley’s located in a region with significant geological activity, characterized by the presence of limestone. That’s a sedimentary rock that dissolves in slightly acidic water, leading to the formation of various karst features such as terraces and waterfalls.

It formed by the deposition of a porous rock. As water flowed over the bedrock, it picked up dissolved calcium carbonate. When this reached the surface and encountered changes in temperature, pressure, or chemical composition, it precipitated out calcium carbonate.

Over time, the deposits of this rock, called tufa, accumulated in layers. This created the terraces and cascades. These terraces give the attention-grabbing Pearl Shoal Waterfall its visually distinctive appearance of multiple streams flowing over a wide area.

The formation and shape of the fall also continued to be influenced by the hydrological conditions in Jiuzhaigou Valley, including the volume and flow rate of water, seasonal variations, and the inexorable erosion of the water over the limestone bedrock.

The stunning product of these forces also represents only a small portion of the equally incredible and expansive Yangtze River system. As a result, the stunning site forms a part of a natural system that has a truly vital impact on the region that it flows through.

The water flowing over the feature remains extremely rich in minerals, such as calcium carbonate, which gets deposited in quantity. This mineral build up is so strong that allows plants and even small trees to actually grow within the middle area of the falls themselves.

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