Introduction : formerly called Western Samoa, the Samoa is a fragment of a chain of islands the other half of which is called the American Samoa. The original people of the islands are the Tongan Polynesians. Samoa remained under New Zealand's dominion for 42 years; from after the World War-I in 1914 until it declared its independence in 1962.
Location of Samoa : the Samoa islands are located in the group of islands that are better known as Oceania. The water body encircling the Samoa islands is the South Pacific Islands. The closest land mass to Samoa is Hawaii and new Zealand.
Physical Map of Samoa : the Samoa islands are made up of two main islands: the Savaii and the Upolu, along with several other atolls. The islands being originally volcanic in origin, the terrain of the land masses are rugged, rocky and mountainous. The coastal regions, on the other hand, comprise of narrow plains. The main islands themselves are surrounded by coral reefs. The highest region on the islands is Mt. Sisisili.
Climate of Samoa : to describe the climatic conditions is of Samoa is to call it a tropical island. The summer months in the island are warm, wet and humid. It is during these months that the islands receive rainfall.
