This astronaut photograph shows the southern end of Paramushir Island after a snowfall. The western slopes of the mountains are brightly illuminated, while the eastern slopes are in shadow.
Four major volcanic centres create this part of the island. Fuss Peak (image centre left) is an isolated stratovolcano connected to the main island via an isthmus. Fuss Peak last erupted in 1854.
The southern tip of the island is occupied by the Karpinsky Group of three volcanic centres. A minor eruption of ash following an earthquake occurred on this part of the island in 1952.
The Lomonosov Group to the north-east (image centre) includes four cinder cones and a lava dome that produced several lava flows in the past, but there have been no eruptions from the Lomonosov Group in recorded history.
The most recent volcanic activity on Paramushir Island occurred in 2008 at the Chikurachki cone located along the northern coastline of the island at image top centre. The summit of this volcano [1,816 meters above sea level] is the highest on Paramushir Island.

Much of the Sea of Okhotsk visible in the image is covered with low clouds that often form around the islands in the Kuril chain. The clouds are generated by moisture-laden air passing over the cool sea/ocean water, and they typically wrap around the volcanic islands.
This astronaut photograph shows the southern end of Paramushir Island after a snowfall. The western slopes of the mountains are brightly illuminated, while the eastern slopes are in shadow. Four major volcanic centres create this part of the island. Fuss Peak (image centre left) is an isolated stratovolcano connected to the main island via an isthmus. Fuss Peak last erupted in 1854. The southern tip of the island is occupied by the Karpinsky Group of three volcanic centres. A minor eruption of ash following an earthquake occurred on this part of the island in 1952. The Lomonosov Group to the north-east (image centre) includes four cinder cones and a lava dome that produced several lava flows in the past, but there have been no eruptions from the Lomonosov Group in recorded history. The most recent volcanic activity on Paramushir Island occurred in 2008 at the Chikurachki cone located along the northern coastline of the island at image top centre. The summit of this volcano [1,816 meters above sea level] is the highest on Paramushir Island. Much of the Sea of Okhotsk visible in the image is covered with low clouds that often form around the islands in the Kuril chain. The clouds are generated by moisture-laden air passing over the cool sea/ocean water, and they typically wrap around the volcanic islands.

Paramushir

islandsvolcanoeshistorywildlifeKuril Islands
4 min read

The Ainu called it the broad island, and from the air the name makes sense. Paramushir stretches roughly rectangular across 2,053 square kilometers of the northern Kuril chain, its spine a continuous ridge of 23 volcanoes running southwest to northeast like the vertebrae of some enormous sleeping creature. At least five of those volcanoes remain active. Chikurachki, the tallest peak on the island and third highest in the Kurils, last sent ash drifting over the town of Severo-Kurilsk in August 2008. Only 11 kilometers of cold water separate Paramushir's northern tip from Cape Lopatka on the Kamchatka Peninsula, yet few places on Earth feel more thoroughly beyond the edge of civilization.

Fire Beneath the Tundra

Paramushir's geology reads like a catalog of volcanic ambition. Chikurachki has erupted repeatedly since 1690, its most recent outburst in 2008 sending a plume of ash trailing for hundreds of kilometers over the Sea of Okhotsk. Fuss Peak, a near-perfect conical stratovolcano, last erupted in 1934. Ebeko's central crater holds a caldera lake, and fumaroles still steam along its flanks. The Karpinsky Group last stirred in 1957. Between these peaks, the sub-arctic climate -- shaped by the chilling Oyashio Current flowing down from the North Pacific -- keeps vegetation low and stunted. Siberian dwarf pine and shrubby alder form dense copses in the valleys, while alpine tundra dominates the higher ground, producing lingonberry, Arctic raspberry, and crowberry in the brief summers.

Where Sea Otters Outnumber People

The narrow strait between Paramushir and neighboring Shumshu supports one of the densest populations of sea otters in the northwest Pacific. Brown bears roam the island's interior. Red foxes, Arctic hares, and ermine are abundant enough that the island's few human inhabitants still hunt them. In spring, crested auklets nest along the rocky coasts, and harbor seals haul out on the beaches. Most remarkably, North Pacific right whales -- among the rarest whale species on Earth -- have been spotted in the surrounding waters. Several species of charr and Pacific salmon spawn in Paramushir's rivers, particularly the Tukharka, the island's longest, threading its way through the volcanic landscape to the sea.

Traded Between Empires

When Russian fur traders first arrived in 1711, the Ainu had long inhabited Paramushir. The island had appeared on Japanese maps as early as 1644, part of the Matsumae Domain's claimed territories during the Edo period. Russian Orthodox missionaries built a church here in 1747, and the Treaty of Shimoda in 1855 initially confirmed Russian sovereignty. Twenty years later, the 1875 Treaty of Saint Petersburg handed the entire Kuril chain to Japan. The Japanese established Kashiwabara on the site of the largest Ainu village, transforming it into a commercial fishing port. During World War II, the Imperial Japanese Army's 91st Infantry Division headquartered there, and the military constructed four airfields across the island. American bombers flying from the Aleutians struck at these bases sporadically from 1943 onward.

The August Invasion and What Followed

On August 18, 1945 -- three days after Emperor Hirohito's surrender announcement -- Soviet troops landed on Paramushir as part of the invasion of the Kuril Islands. Fighting continued through August 23 before the surviving Japanese garrison surrendered. What followed was swift and final: the Soviets forcibly deported the remaining Japanese civilians and sent prisoners of war to labor camps. Kashiwabara was renamed Severo-Kurilsk, and the island was annexed in 1946. Japan formally relinquished sovereignty under the San Francisco Peace Treaty of 1951. Then, in November 1952, a massive tsunami obliterated Severo-Kurilsk entirely. The town was rebuilt at a different location, but the catastrophe accelerated a decline that the collapse of the herring fishery and the fall of the Soviet Union would deepen. By the 2002 census, only 2,592 people remained -- half the 1989 figure. Villages that once lined the coast stand empty, their buildings slowly claimed by wind and tundra.

From the Air

Paramushir lies at approximately 50.38N, 155.68E in the northern Kuril Islands. The volcanic spine is visible from altitude, with Chikurachki's cone being the most prominent landmark. Nearest airport is at Severo-Kurilsk (no ICAO code assigned to civilian traffic; military use). The island sits just south of the Kamchatka Peninsula across the First and Second Kuril Straits. Expect frequent fog, low cloud, and turbulence due to volcanic terrain and maritime weather. Petropavlovsk-Kamchatsky (UHPP) is the closest major airport, roughly 300 km to the north.