The Oat Banner

Triton Geyser Height

CRYOVULCANIC PLUME MONITOR

GEYSER ACTIVITY:

Nitrogen Eruption

Triton's geysers shoot plumes of nitrogen gas mixed with dark dust into the thin atmosphere, reaching incredible heights before being carried away by high-altitude winds.

PLUME HEIGHT
8 KM

Vertical reach into the exosphere.

TEMPERATURE
-235°C

Surface temperature during eruption.

Geyser Height

Cryovolcanic Plumes. In Triton's weak gravity, pressurized nitrogen gas erupts through the ice, towering 8 kilometers above the frozen surface.

  • 📏 Vertical: 8,000 meters high.
  • ↔️ Horizontal: 150 km wind streaks.
  • ☀️ Driver: Subsurface Solar Greenhouse effect.
🌋
The Oat: PLUME_ALT
MAX HEIGHT:
8.0 KM
STATUS: ACTIVE_CRYO_VENT

Vertical Limit

8 Kilometers High. In Triton's near-vacuum and weak gravity, nitrogen plumes reach altitudes that dwarf Earth's highest mountains.

  • 📏 Vertical: 8 km straight-up ascent.
  • 🌬️ Horizontal: Drifts into 150 km streaks.
  • 📉 Gravity: Only 0.779 m/s² (8% of Earth).
📏
The Oat: ALT_LIMIT
CEILING:
8.0 KM
STATUS: PEAK_COLUMN_HEIGHT

Atmospheric Streaks

Horizontal Migration. High-altitude winds catch the dark geyser dust, dragging it across the icy plains to create 150km-long signatures of Triton’s climate.

  • 🏁 Range: Over 150 km from the source vent.
  • 🌪️ Velocity: 30–50 m/s high-altitude winds.
  • 🌑 Material: Dark carbon-rich "tholin" dust.
💨
The Oat: STREAK_SCAN
DRIFT LEN:
150 KM
STATUS: UNIFORM_WIND_DEPOSIT

Sub-Surface Pressure

The Greenhouse Explosion. Trapped solar heat sublimates nitrogen ice into high-pressure gas, turning Triton's crust into a ticking geological time bomb.

  • ☀️ Input: Solar penetration through nitrogen ice.
  • 💨 Process: Solid-to-gas sublimation.
  • ⚡ Result: Pressure-driven supersonic eruption.
💥
The Oat: PRESSURE_SYNC
CRUST TENSION:
CRITICAL
STATUS: VENT_RUPTURE_LIKELY

Paper

GEYSER LOG 🌋

Subject: Cryovolcanic Eruption. Target: South Polar Cap.

Sources

VERTICAL HEIGHT

Eruptions shoot nitrogen gas and dust plumes directly upward to an altitude of **8 kilometers** (5 miles).

NASA MISSION DATA
Max Height: 8 km

HORIZONTAL DRIFT

Once the plumes reach the thin atmosphere, they drift horizontally for over **150 kilometers** due to high-altitude winds.

VOYAGER IMAGERY
Drift: 150+ km

DRIVING FORCE

Subsurface nitrogen is heated by the Sun through a "greenhouse effect" in the ice, creating pressure that vents through cracks.

CRYOVOLCANO MATH
Energy: Solar Heating

Frozen Poles

Mapping the southern hemisphere's nitrogen ice sheet and streak deposits.

Cryo-Eruption

Visualizing sunlight heating subsurface nitrogen to trigger high-pressure plumes.

Voyager Data

Plume Height: ~8 km (5 miles)

Surface Age: Very young (Active resurfacing)

Discovery: Voyager 2 Flyby (1989)