Venus is the hottest world in the solar system. Although Venus is not the planet closest to the sun, its dense atmosphere traps heat in a runaway version of the greenhouse effect that warms up the Earth. As a result, temperatures on Venus reach 870 degrees F (465 degrees C), more than hot enough to melt lead. Probes that scientists have landed there have survived only a few hoursbefore getting destroyed.
Venus has a hellish atmosphere as well, consisting mainly of carbon dioxide with clouds of sulfuric acid, and scientists have only detected trace amounts of water in the atmosphere. The atmosphere is heavier than that of any other planet, leading to a surface pressure 90 times that of Earth.
The surface of Venus is extremely dry. There is no liquid water on its surface because the scorching heat would cause any to boil away. Roughly two-thirds percent of the Venusian surface is covered by flat, smooth plains that are marred by thousands of volcanoes, ranging from about 0.5 to 150 miles (0.8 to 240 kilometers) wide, with lava flows carving long, winding canals up to more than 3,000 miles (5,000 kilometers) in length, longer than on any other planet.
Six mountainous regions make up about one-third percent of the Venusian surface. One mountain range, called Maxwell, is about 540 miles (870 kilometers) long and reaches up to some 7 miles (11.3 kilometers) high, making it the highest feature on the planet.
Venus also possesses a number of surface features unlike anything on the Earth. For example, Venus has coronae, or crowns — ringlike structures that range from roughly 95 to 360 miles (155 to 580 kilometers) wide. Scientists believe these formed when hot material beneath the crust rises up, warping the planet’s surface. Venus also has tesserae, or