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National flag consisting of a red field (background) with a blue canton incorporating a white sun. The width-to-length ratio of the flag is 2 to 3.The first Chinese republic lasted from 1911 until 1928. Its national flag consisted of five equal horizontal stripes of red, yellow, blue, white, and.
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- Relief and drainage
Palau has three official languages: Palauan, Sonsorolese-Tobian, and English.
What is the official currency of Palau?
The U.S. dollar is the official currency of Palau, which does not have a central bank. In 1997 the country joined the International Monetary Fund. There is a heavy reliance on financial assistance from the United States.
When did Palau gain independence?
Palau became independent in October 1994 and joined the United Nations the following December.
What is the capital of Palau?
All but six of Palau’s islands lie within an expansive lagoon, enclosed by the barrier reef, that stretches northeast to southwest for almost 70 miles (115 km). Babelthuap, the largest island (153 square miles [396 square km]), is volcanic, mainly composed of andesite, and is bounded by thick mangrove forests broken occasionally by sandy beaches on the east coast. Its highest point, Ngerchelchuus, in the northwest, is 794 feet (242 metres) high. Babelthuap is essentially a rolling upland, part grassland and part jungle, that has been incised by stream action to form a well-developed drainage system of three rivers. With about 150 inches (3,800 mm) of rain annually, considerable erosion has taken place on Babelthuap in spite of the stability provided by laterite soils, clays, and vegetation. The Palauan practice of burning the grassy upland areas during the dry season has contributed to erosion.
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A steel bridge connects the islands of Babelthuap and Koror. Koror in turn is linked by causeway to Malakal Island, the site of Palau’s deepwater port, and to Arakabesan Island. The combined area of the three smaller linked islands is 7 square miles (18 square km). All are of volcanic origin. However, beginning adjacent to southern Babelthuap and eastern Koror and filling the huge lagoon for 28 miles (45 km) south to Peleliu are more than 300 verdant “rock islands.” These are uplifted reef structures of coralline limestone, each deeply undercut at sea level. Some of the rock islands are large, towering some 600 feet (180 metres); these can have interior brackish lakes, containing unique organisms, that are connected to the lagoon by subterranean channels. Plant growth is thick on the rock islands and, together with the chemical action of heavy rains, has sculpted and broken their surfaces, producing razor-sharp edges and points and broken rubble. The limestone islands have rich deposits of phosphate, and the more accessible ones have been mined.
The inhabited coral islands outside Palau’s reef-lagoon-island system sit on volcanic substructures and consist of the Kayangel Islands, 25 miles (40 km) north of Babelthuap, and Angaur, 6 miles (10 km) south of Peleliu. Angaur was heavily mined for its phosphate first by the Germans and later by the Japanese. Sonsorol, Pulo Anna, and Tobi, all with areas of less than 1 square mile (2.6 square km), are 180 miles (290 km) southwest of the Palau archipelago. All are flat platform structures with fringing reefs.
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