Kuchinoerabu-jima, is one of the Satsunan Islands, usually classed with the Ōsumi Islands belonging to Kagoshima Prefecture, Japan. The island, 38.04 km² in area, has a population of 147. The island can only be reached by boat as it has no airport. There is regular ferry service with Yakushima, which is about 15 km to the east. Travel time is approximately 1 hour. The islanders are dependent mainly on fishing, agriculture and seasonal tourism. The entire island is within the borders of the Kirishima-Yaku National Park.
Geography
Kuchinoerabu-jima is located south of Kagoshima. The island is of volcanic origin, and has an area of approximately with a length of and width of. The highest elevations on the island are Furudake, with a height of and Shindake, with a height of above sea level. There are numerous hot springs on the island. The island is an active volcano which has erupted several times during the modern period, including 24 December 1933, when several people were killed when lava masses buried several villages. In 1980, multiple explosion craters appeared along an north-south fissure on the slope east of Shindake. Shindake erupted again on 4 August 2014, generating a pyroclastic flow, but with no injuries or fatalities. The main crater erupted on the morning of29 May 2015, prompting a level 5 alert level and the evacuation of the island. The island’s climate is classified as subtropical, with a rainy season from May through September.
On May 18, 2015 Japanese scientists detected increased seismic activity and steam rising from the Shindake's crater, and on May 29, 2015 an eruption sent an ash cloud an estimated 30,000 feet into the sky. No deaths and only one minor injury were reported by the Japanese government. The island’s 140 residents were evacuated by Japan’s coast guard. Previous eruptions occurred in August, 2014 and in 1980. Shindake crater erupted on December 18, 2018, ejecting an ash cloud 2 kilometers into above cloud coverage. Thirty days later on January 17, 2019, Shindake erupted again, sending pyroclastic flows 1.5 kilometers to the southwest and northwest of the crater as well as an ash cloud 6 kilometers into the atmosphere.