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The Wushih Pi headland is part of Taiwan's Central Mountain Range which extends from Su-ao in the northeast to Eluanbi at the southern tip of the island, forming a ridge of high mountains and serving as the island's major watershed for rivers and streams. The mountains are predominantly composed of hard rock formations resistant to weathering and erosion, although heavy rainfall has deeply scarred the sides with gorges and sharp valleys. Taroko National Park, located on the mountainous eastern side of the island, has good examples of mountainous terrain, gorges and erosion caused by a swiftly flowing river.
The Wushih Pi headland is part of Taiwan's Central Mountain Range which extends from Su-ao in the northeast to Eluanbi at the southern tip of the island, forming a ridge of high mountains and serving as the island's major watershed for rivers and streams. The mountains are predominantly composed of hard rock formations resistant to weathering and erosion, although heavy rainfall has deeply scarred the sides with gorges and sharp valleys. Taroko National Park, located on the mountainous eastern side of the island, has good examples of mountainous terrain, gorges and erosion caused by a swiftly flowing river.
The Wushih Pi headland is part of Taiwan's Central Mountain Range which extends from Su-ao in the northeast to Eluanbi at the southern tip of the island, forming a ridge of high mountains and serving as the island's major watershed for rivers and streams. The mountains are predominantly composed of hard rock formations resistant to weathering and erosion, although heavy rainfall has deeply scarred the sides with gorges and sharp valleys. Taroko National Park, located on the mountainous eastern side of the island, has good examples of mountainous terrain, gorges and erosion caused by a swiftly flowing river.
The Wushih Pi headland is part of Taiwan's Central Mountain Range which extends from Su-ao in the northeast to Eluanbi at the southern tip of the island, forming a ridge of high mountains and serving as the island's major watershed for rivers and streams. The mountains are predominantly composed of hard rock formations resistant to weathering and erosion, although heavy rainfall has deeply scarred the sides with gorges and sharp valleys. Taroko National Park, located on the mountainous eastern side of the island, has good examples of mountainous terrain, gorges and erosion caused by a swiftly flowing river.
The Tang Dynasty (Chinese: 唐朝; pinyin: Táng Cháo; June 18, 618 – June 1, 907) was an imperial dynasty of China preceded by the Sui Dynasty and followed by the Five Dynasties and Ten Kingdoms Period. It was founded by the Li (李) family, who seized power during the decline and collapse of the Sui Empire. The dynasty was interrupted briefly by the Second Zhou Dynasty (October 8, 690 – March 3, 705) when Empress Wu Zetian seized the throne, becoming the first and only Chinese empress regnant, ruling in her own right.<br/><br/> The Tang Dynasty, with its capital at Chang'an (present-day Xi'an), which at the time was the most populous city in the world, is generally regarded as a high point in Chinese civilization—equal to, or surpassing that of, the earlier Han Dynasty—a golden age of cosmopolitan culture. Its territory, acquired through the military campaigns of its early rulers, rivalled that of the Han Dynasty. In two censuses of the 7th and 8th centuries, the Tang records estimated the population by number of registered households at about 50 million people.