Topographic relief of Fuji Volcano combined with geological map, showing NW-SE trending lateral cones around the main cone. The lava flowed not only from the summit but also from these lateral cones

Aerial view of Fuji Volcano and Hoei Craters as seen from the SE.

Fuji Volcano and Omuroyama Scoria Cone in the left center viewed from the NW (Lake Motosu-ko).

View of the Fuji Volcano from the E. Kansuyama Scoria Cone at the left end.

Mt. Fuji viewed from the N, Yanagisawa-toge Pass.

Hoei Crater of Fuji Volcano viewed from the SSE. Many dikes crop out at the wall.

Summit crater viewed from the SW, Kenga-mine. A shrine, Sengen-taisha Okunomiya on the right end

Aerial view of Fuji Volcano as seen from the S, showing the Hoei craters with Mt. Hoei on the right slope.

The southwest wall of the summit crater, with the meteorological observatory above the highest point (Kengamine). The radar dome for meteorological observation was dismantled in September 2001

Topographic relief around Hakone Volcano.

Aerial view of Hakone Volcano as seen from the SSE. Central cones (lava domes and stratovolcanoes) inside the caldera

Kanmurigatake Lava Dome and fumarolic activity at Owaku-dani viewed from the N

Kanmurigatake Lava Dome from the N (Owaku-dani).

Kamiyama Volcano (stratovolcano) viewed from the W. Lake Ashinoko was formed by the collapse of the northwestern part of Kamiyama, about 3,000 years ago. The peak (Kanmurigatake) on the left side of the summit is a volcanic spine formed in the scarp

Central cones of Hakone Volcano viewed from the south of Lake Ashinoko. Futagoyama (right) consists of two lava domes, and Komagatake Lava Dome on the shoulder of Kamiyama Volcano (stratovolcano) .

Aerial view of Omuroyama Scoria Cone and its lava flows as seen from the E.

Aerial view of Omuroyama Scoria Cone as seen from the SW, showing a small crater on the mountain slope. Lava flows spilled from Omuroyama around.

Hachinoyama Scoria Cone viewed from the W.

Omuroyama Scoria Cone viewed from the W.

Yahazuyama Lava Dome (center) and Ananoyama Lava Dome (right) viewed from the E, crater rim of Omuroyama

Topographic relief of Sambesan area combined with geological map. Sambe lava domes comprise the Sambe Caldera (4 x 6 km) including Osambesan Lava Dome. Muronouchi Crater in the center and Okunoyu Crater in the south. Most of the caldera floor was covered by talus deposits (greenish yellow) that are underlain by ignimbrite (green) along the valley outside the caldera

Topographic relief of Sambesan area combined with geological map (tilted by 30° from the W to the E). Sambe lava domes located in the Sambe Caldera (4 x 6 km in diameter). Muronouchi Crater rim comprise Osambesan (left), Mesambesan (back side) and Kosambesan (middle). Most of the caldera floor was covered by talus deposits (greenish yellow, A).

View of Osambesan (left) and Kosambesan (center) from the W

Osambesan (left) and Kosambesan (right), viewed from the pond of Ukinunoike

Oblique aerial view of Osambesan (center), Mesambesan (on the right with pylon) and Kosambesan (left), as seen from the E