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Explore the surface conditions of Venus, including its mostly smooth rolling plains, modest highlands and lowlands, and two elevated continent-sized regions known as Ishtar Terra and Aphrodite Terra, featuring the Cleopatra Crater and volcanic activity. Discover the unique topography and absence of small impact craters on Venus, as well as the dry and dusty surface conditions with no magnetic field protection.
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Surface Features • Mostly smooth, rolling plains. • Modest highlands and lowlands.
There are two elevated, continent-sized regions. They make up only 8% of the total surface area.
The Ishtar Terra is found in the northern hemisphere and is about the size of Australia.
One significant feature of the Ishtar Terra is the Cleopatra Crater, a volcanic crater that is 100 km across.
The other elevated region is the Aphrodite Terra. It is Africa-sized and is located along the equator.
Topographical map of Venus showing Ishtar and Aphrodite Terrae
Volcanic activityThe most common volcanoes are shield volcanoes.
Shield volcanoes are formed when lava wells up through a “hot spot”. Many successive lava flows build up high mountains.
The largest structures are coronae. These are upwellings of mantle material and are structures unique to Venus.
Some craters are meteorite impact craters. Some of these are oddly-shaped probably because the meteorite broke up in the harsh atmosphere.
There are no small impact craters. No small meteorite could make it through the atmosphere to the surface.
There is evidence of volcanism today. The levels of SO2 fluctuate greatly. There are also bursts of radio energy from the highlands. BUT...
The samples of crust tested were of two types: • Basalt - volcanic material formed later in the planet’s history. • Granite - the original crust material.
There is no magnetic field, probably due to the slow rotation rate. This means there is no magnetosphere, so there is no protection from the solar wind.