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" ... At the same time, our visit to Pluto with the New Horizons spacecraft has revealed to us exactly what this distant dwarf planet is like. The world is geologically fascinating, with its own atmosphere complete with hazes, ice mountains and plains that float atop a thick liquid ocean, snowy weather patterns, and a complex and varied surface that evolves over time. In many ways, it’s more complex and has more potential for interesting chemical reactions — possibly even including biological activity — than bona fide planets such as Mercury. ... "
" ... For a long time the Moon was considered a geologically inactive body, too small to hold enough interior heat to drive tectonics or feed volcanism. Only with the first crewed Moon landings and the installation of a network of seismometer stations, researchers discovered that the Moon is surprisingly active, with small earthquakes happening there all the time. Also, the Moon's surface is not as dead at its appears on a first superficial glimpse. ... "
" ... Leonardo da Vinci studied rocks and landscapes not only to satisfy his personal curiosity, but also to improve his paintings. The layers in his sketch, shown above the waterfall, are geologically correct. Turbidite layers, formed by submarine avalanches and later pushed by tectonic forces above the sea, are commonly spotted in rocky outcrops of the Apennines and are thin at the bottom and thick on the top, a result of the different rates of sedimentation under water. ... "
" ... The Earth has an ever-changing, geologically complex crust, whose intricacies can variably transmit and absorb seismic energy. Conversely, the moon’s volcanic crust is old and cold; seismic waves love to travel uninterrupted through this sort of rigid material, bouncing around all the cracks and crevasses without getting quickly soaked up by any water-bearing minerals or bodies of water. Unlike earthquakes, moonquakes can last for hours, with the entire pale orb ringing like a colossal bell. ... "
" ... The deepest point of Earth's continents has been identified in Queen Mary Land, East Antarctica. The canyon buried under the ice of the Denman Glacier reaches 11,500 feet (3.5 kilometers) below sea level, for comparison, the lowest exposed land on Earth, the Dead Sea in the Jordan Rift Valley, is just 1,355 feet (413 meters) below sea level. The Mariana Trench in the western Pacific Ocean is still the deepest point on Earth with 36,037 feet (10.9 kilometers), but is geologically speaking part of the ocenic crust. ... "