Mountain stream of AmamiOshima Island
History
The Amami Islands are located in the center of the arc-shaped archipelago of the Ryukyu chain. Due to intense shifts in the earth's crust starting from the Neogene Period of the Cenozoic Era (23 million to 2.6 million years ago), the islands were repeatedly connected to and separated from neighboring landmasses and the main island of Japan.
By approx. 12 million years ago
By around 12 million years ago, the archipelago was connected to the neighboring landmass. It is believed that many animals, including the ancestor of Amami Rabbit (Pentalagus furnessi), crossed over to the islands during this time.
Approx. 12 million to 2 million years ago
By around two million years ago, the Ryukyu chain had been separated into three larger island blocks: the Northern Ryukyus connected to Kyushu, the Central Ryukyus, and the Southern Ryukyus. During this time, the Amami area, where Amamigunto National Park is located, was part of the Central Ryukyu island.
Approx. 2 million years ago to present day
Afterwards, due to changes in sea level, Central Ryukyu was repeatedly separated from and connected to its neighboring islands, finally forming the Ryukyu chain of the present day. Through this process, many of the plants and animals inhabiting the area became trapped on the newly formed islands and over the next hundreds of thousands of years, they evolved into new species endemic to these islands themselves.
The islands can be divided into two types, depending on the way they were formed. Each island type differs greatly in the kinds of plants, animals, and landscapes that can be found there.
High, mountainous islands
(Kakeromajima)
High, mountainous islands
(Amami-Oshima, Kakeromajima, Ukejima, Yorojima, and Tokunoshima Islands)
These islands are composed of geological formations that were formed before the Neogene Period of the Cenozoic Era, and characterized by mountainous regions and great changes in elevation. The mountainous areas run up to the edge of the coastlines forming extremely steep cliffs and leaving little room for flatter ground.
Low, flat islands
(Okinoerabujima)
Low, flat islands
(Kikaijima, Okinoerabujima, and Yoronjima Islands)
Formed during the Quaternary Period of the Cenozoic Era from Ryukyu limestone, these islands are low and flat with few mountainous areas. With the terraced terrain that developed during this period, you can find natural terraced hills made up of several "steps" much like a staircase on these islands.
The Amami Islands have a warm, moist climate with an average annual temperature of 21°C and an abundant amount of annual precipitation (approximately 2,800 mm on Amami-Oshima Island). Owing to the differences in how each island was formed, the archipelago has a wonderfully diverse natural environment with subtropical, evergreen broad-leaved forests; tidal flats, a type of coastal wetland; zigzagging ria coasts, and coral reefs.