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Owakudani Volcanic Gas Vents Close-Up, Hakone Japan. Explore the active volcanic landscape of Owakudani in Hakone, Japan. Geothermal vents release sulfurous steam amidst rocky terrain and barren slopes.
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RAW
MP4

Resolution
Frame Rate
Codec
Gamma
LUT
Bitrate
6144 x 3456
50 fps
Blackmagic RAW 12-bit
BMD Film Gen 5 (Gamut 5)
No LUT applied
3 Gbps
1920 x 1080
24 fps
H.264 8-bit
Rec.709 (BT.709)
CanonLog2-to-BT2020_HLG-Vivid_65_FF_Ver2.0
25 Mbps

Clip Length
Camera
Lens
F-Stop
ISO
Color Temp
Focal Length
Location
01:02
Blackmagic Pocket Cinema Camera 6K G2
DZO Film Pictor
T2.8
250
5600 K
125mm
Owakudani, Hakone, Japan



  The stock video presents a captivating close-up view of the dynamic volcanic landscape found within Owakudani, a prominent geothermal valley in Hakone, Japan. The dominant features are the numerous vents actively releasing plumes of white, sulfurous steam and gases directly from the earth's surface. The terrain is markedly rugged, characterized by an abundance of fragmented rocks and boulders, primarily in shades of grey and an intriguing yellowish-ochre, indicative of mineral deposits and the effects of intense heat and acidic gases. The ground is largely barren in areas directly impacted by the vents, showcasing the harsh conditions that prevail. However, patches of resilient, dry, and light-brown vegetation can be observed clinging to the less volatile slopes, providing a subtle textural contrast against the stark rock formations. This particular scene vividly illustrates the intense geothermal activity for which Owakudani is famous. The steam rises with varying intensity, creating a misty, atmospheric effect that underscores the active nature of this volcanic region. The detailed perspective offered by the stock video allows for a clear appreciation of the geological processes at play, from the constant emission of gases to the weathering and alteration of the rock formations over time. Owakudani, often referred to as the "Great Boiling Valley," is a caldera formed after the eruption of Mount Hakone approximately 3,000 years ago. Today, it remains an active volcanic zone, continuously emitting volcanic gases, primarily hydrogen sulfide and sulfur dioxide, which contribute to the distinctive smell and unique appearance of the area. This close-up captures a moment in this ongoing geological spectacle, emphasizing the raw, powerful forces shaping the Earth's surface in this iconic Japanese location.

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