Obtained by Mariner 10.
Appears yellowish-orange due to sulfur dioxide (SO2).
SO2 can combine with water to form sulfuric acid (H2SO4).
Average Orbit Radius: 0.72 astronomical units (au)
Receives approximately 1.9 times the solar radiation compared to Earth.
Orbital Period: 0.615 years (225 Earth days)
Lies between Mercury and Earth's orbital periods, consistent with Kepler’s third law.
Rotational Period: 243 Earth days
Venus rotates slowly; its day is longer than its year.
Axis Tilt: 177.4°
Spins retrograde (clockwise).
Hypothesis: A massive impactor may have flipped Venus and slowed its rotation.
Radius: 0.95 times that of Earth (RE);
Sometimes called sister planets with Earth due to size similarity but with notable differences.
Planet Mass: 0.82 times that of Earth (ME);
Compressed density is about 95% that of Earth.
Surface Temperature: Approximately 740 K (870 °F)
Uniform temperature day and night; similar across equator and poles.
Atmospheric Pressure: 92 times that of Earth.
Simplified as pVenus ≈ 100 pEarth.
Dense CO2 atmosphere prevents visible light observation; creates a runaway greenhouse effect.
Magnetosphere: Absent
Indicates Venus lacks a global magnetic field.
Over 40 spacecraft have explored Venus, notably:
Mariner 2 (1962): First spacecraft to provide surface temperature data.
Magellan (1989): Mapped the surface using radar (couldn't be seen in visible light due to clouds).
First to image entire surface, developed topological maps by measuring travel time of microwaves.
Mapped 95% of gravitational field and was destroyed to quantify atmospheric density at mission's end.
Conducted by the former Soviet Union (1961-1984)
16 spacecraft: 13 transmitted atmospheric data, 10 transmitted surface data.
Notable achievements:
First to enter another planet's atmosphere (Venera 4, 1967).
First to achieve a soft landing (Venera 7, 1970).
First to send images from the surface (Venera 9, 1975).
High-resolution radar mapping (Venera 16, 1983).
Surface conditions harsh; earlier probes survived from 30 minutes to 2 hours.
Many failed attempts were not recognized as Venera missions.
Venera 7: Overbuilt to withstand surface conditions, survived impact but encountered signal loss and internal failures.
Structure: Iron core, rocky mantle, and crust similar to Earth.
No consensus on the core's state: solid, molten, or partially molten.
Lack of a magnetosphere suggests a solid metal core.
Thin crust, likely fragmented, no plate tectonics.
Radar data reveals mountains, valleys, and craters from historical volcanism; surface 0.5-1 billion years old.
Only about 1,000 craters detected, mostly large due to:
Smaller craters covered by lava flows.
Dense atmosphere incinerates smaller meteoroids before reaching the surface.
Most abundant in the Solar System with over 1,600 large features.
All are shield volcanoes, flatter than Earth's with wider calderas and coronas.
Formation of coronas involves mantle material pushing crust upward, while calderas form from collapses above magma chambers.
Smallest continent-sized highland region on Venus, about the size of Australia.
Contains Lakshmi Planum, a high, flat lava-covered plateau, about 3.5 km above average radius.
Surrounded by mountains, including Maxwell Montes (tallest range on Venus at 11 km).
Composition: 96.5% CO2, 3.5% N2, trace amounts of H2SO4 and H2O.
Thickness: ~250 km, much thicker than Earth's atmosphere.
Atmospheric pressure approximately 100 times that of Earth's.
Opaque sulfuric acid clouds impede surface visibility; with a runaway greenhouse effect maintaining high surface temperatures.
Wind speeds vary drastically with altitude; upper atmosphere: 360 km/h, middle layer: >700 km/h, surface: slight breezes.
Lightning detected involving sulfuric acid vapor; no rainfall.
Both planets formed similarly, but differing solar distances led to stark atmospheric contrasts.
Increased solar energy caused more reactive atmospheric gases on Venus, inhibiting water vapor formation and contributing to greenhouse gases.
The prevailing hypothesis addresses water vapor loss; UV light breaks down H2O, allowing hydrogen to escape, possibly assisted by electric fields.
Replacement of escaping water vapor with inner atmosphere's water resulted in a dense CO2 environment, explaining current atmospheric conditions.