Japan's Mt. Fuji

Japan's Mt. Fuji

File photo taken from a Kyodo News helicopter above Mishima, Shizuoka Prefecture, on Feb. 18, 2019, shows Mt. Fuji, Japan's highest mountain. (Kyodo) ==Kyodo

  • Product Code
  • ILEA000162128
  • Registered date
  • 2019/6/01 03:00:00
  • Credit
  • Kyodo / Kyodo News Images
  • Media source
  • 2019 Kyodo News
  • Media size
  • 3968 × 2668 pixel
  • Resolution
  • 240 dpi
  • Deployment size
  • 1.38(MB)*
  • Special instruction

*File size when opened in Photoshop, etc.

Similar Images & Videos
    Endangered leopard cat released on western Japan island

    Endangered leopard cat released on western Japan island

    A juvenile male leopard cat, an endangered species, looks around upon being released into the wild on a mountain in the southwestern Japan island of Tsushima, Nagasaki Prefecture, on April 22, 2024, after being treated at a protection center for injuries from a car accident and completing reintroduction training.
      Endangered leopard cat released on western Japan island

      Endangered leopard cat released on western Japan island

      A juvenile male leopard cat, an endangered species, looks around upon being released into the wild on a mountain in the southwestern Japan island of Tsushima, Nagasaki Prefecture, on April 22, 2024, after being treated at a protection center for injuries from a car accident and completing reintroduction training.
        Zhada Tulin Scenery in Tibet

        Zhada Tulin Scenery in Tibet

        NGARI, CHINA - FEBRUARY 27, 2024 - Aerial photo taken on February 27, 2024 shows the weathered Zhada Tulin, one of the most typical and largest Tertiary formations in the world in Ngari Prefecture, Tibet, China. It is understood that the "soil mountain forest" landform is formed by the sediment layer of the lake basin in the ancient time under the influence of the Himalayan orogeny, with the decrease of the water level and the elevation of the lake basin, after billions of years of weathering and denudation.
          Zhada Tulin Scenery in Tibet

          Zhada Tulin Scenery in Tibet

          NGARI, CHINA - FEBRUARY 27, 2024 - Aerial photo taken on February 27, 2024 shows the weathered Zhada Tulin, one of the most typical and largest Tertiary formations in the world in Ngari Prefecture, Tibet, China. It is understood that the "soil mountain forest" landform is formed by the sediment layer of the lake basin in the ancient time under the influence of the Himalayan orogeny, with the decrease of the water level and the elevation of the lake basin, after billions of years of weathering and denudation.
            Zhada Tulin Scenery in Tibet

            Zhada Tulin Scenery in Tibet

            NGARI, CHINA - FEBRUARY 27, 2024 - Aerial photo taken on February 27, 2024 shows the weathered Zhada Tulin, one of the most typical and largest Tertiary formations in the world in Ngari Prefecture, Tibet, China. It is understood that the "soil mountain forest" landform is formed by the sediment layer of the lake basin in the ancient time under the influence of the Himalayan orogeny, with the decrease of the water level and the elevation of the lake basin, after billions of years of weathering and denudation.
              Zhada Tulin Scenery in Tibet

              Zhada Tulin Scenery in Tibet

              NGARI, CHINA - FEBRUARY 27, 2024 - Aerial photo taken on February 27, 2024 shows the weathered Zhada Tulin, one of the most typical and largest Tertiary formations in the world in Ngari Prefecture, Tibet, China. It is understood that the "soil mountain forest" landform is formed by the sediment layer of the lake basin in the ancient time under the influence of the Himalayan orogeny, with the decrease of the water level and the elevation of the lake basin, after billions of years of weathering and denudation.
                Zhada Tulin Scenery in Tibet

                Zhada Tulin Scenery in Tibet

                NGARI, CHINA - FEBRUARY 27, 2024 - Aerial photo taken on February 27, 2024 shows the weathered Zhada Tulin, one of the most typical and largest Tertiary formations in the world in Ngari Prefecture, Tibet, China. It is understood that the "soil mountain forest" landform is formed by the sediment layer of the lake basin in the ancient time under the influence of the Himalayan orogeny, with the decrease of the water level and the elevation of the lake basin, after billions of years of weathering and denudation.
                  Zhada Tulin Scenery in Tibet

                  Zhada Tulin Scenery in Tibet

                  NGARI, CHINA - FEBRUARY 27, 2024 - Aerial photo taken on February 27, 2024 shows the weathered Zhada Tulin, one of the most typical and largest Tertiary formations in the world in Ngari Prefecture, Tibet, China. It is understood that the "soil mountain forest" landform is formed by the sediment layer of the lake basin in the ancient time under the influence of the Himalayan orogeny, with the decrease of the water level and the elevation of the lake basin, after billions of years of weathering and denudation.
                    Zhada Tulin Scenery in Tibet

                    Zhada Tulin Scenery in Tibet

                    NGARI, CHINA - FEBRUARY 27, 2024 - Aerial photo taken on February 27, 2024 shows the weathered Zhada Tulin, one of the most typical and largest Tertiary formations in the world in Ngari Prefecture, Tibet, China. It is understood that the "soil mountain forest" landform is formed by the sediment layer of the lake basin in the ancient time under the influence of the Himalayan orogeny, with the decrease of the water level and the elevation of the lake basin, after billions of years of weathering and denudation.
                      Zhada Tulin Scenery in Tibet

                      Zhada Tulin Scenery in Tibet

                      NGARI, CHINA - FEBRUARY 27, 2024 - Aerial photo taken on February 27, 2024 shows the weathered Zhada Tulin, one of the most typical and largest Tertiary formations in the world in Ngari Prefecture, Tibet, China. It is understood that the "soil mountain forest" landform is formed by the sediment layer of the lake basin in the ancient time under the influence of the Himalayan orogeny, with the decrease of the water level and the elevation of the lake basin, after billions of years of weathering and denudation.