Kitt Peak Nightly Observing Program
Splendors of the Universe on YOUR Night!
Many pictures are links to larger versions.
Click here for the “Best images of the OTOP” Gallery and more information.
Copernicus is a large, conspicuous crater located in the Oceanus Procellarum (Ocean of Storms). It has extensive rays of ejecta spanning hundreds of kilometers from the rim of the crater. This crater is likely to be only hundreds of millions of years old—young for a lunar crater.
Because of its very smooth, dark floor, Plato is a very distinct crater, seen just north of Mare Imbrium. Plato is 101 km across, and the peaks of the rim rise 2,000 meters above the floor.
Apollo 15 landed in the Hadley plains, near Hadley Rille. This mission was the first long, more science-focused lunar landing mission. During this mission, a Lunar Roving Vehicle was used for the first time. One of the most exciting findings of Apollo 15 was a 4.1 billion year old rock, known now as the Genesis Rock. This is also the mission during which the famous hammer and feather experiment was conducted. Astronaut David Scott dropped a feather and hammer at the same time, demonstrating that objects fall at the same rate regardless of their mass. While air resistance on Earth would slow the feather down, the feather hit the ground at the same time as the hammer on the Moon. Though we cannot see anything left behind by the astronauts form Earth, the Lunar Reconnaissance Orbiter can see some of the items left behind at the landing site from orbit of the Moon.
The Mare Imbrium Impact Basin formed when a large object crashed into the Moon 3.9 billion years ago. subsurface lava rose to flood the giant crater, eventually solidifying into a younger, smoother terrain. Prominent features of Mare Imbrium include the crater Plato to the north, with a dark crater floor; Sinus Iridum (meaning Bay of Rainbows) to the northwest, with the Montes Jura mountain range forming a distinct C-shaped knob on the edge of the mare; and the 3 mountain ranges—Montes Alpes, Caucasus, and Apenninus—that mark the eastern edge of the mare.
West of the Montes Caucasus, in the Mare Imbrium, is the lonely Mons Piton. Though Mons Piton is a part of the Montes Teneriffe lunar mountain range, it is far seperated form the rest of the peaks in this range.
The mountain range Montes Alpes is one of the prominent mountain ranges along the eastern border of Mare Imbrium. The range is named for the Alps on Earth, and the peak Mons Blanc is named for the tallest peak in the Alps of Earth—though Mons Blanc is actually the 3rd tallest peak of the Lunar Alpes. The range culminates to the south in the Promontorium Agassiz. To the north, the range terminates just shy of dark-floored crater Plato.
The Montes Apenninus, named for the Apennine Mountains in Italy, is a mountain range along the southeastern rim of the Mare Imbrium Impact basin (Sea of Showers). The Montes Apenninus contain some of the tallest mountains on the Near Side of the Moon.
Amazingly, Apollo 15 landed between the the peaks of the Apennine Mountains to the east, and Hadley Rille to the west. Hadley Rille is a very sinuous rille, winding through the Apennine Mountains.
Vallis Alpes is a wide, 180 km long valley. It’s western end is in the Montes Alpes at the northeastern edge of the Mare Imbrium, and its western end terminates at the edge of the northern Mare Frigoris. This split in the lunar crust probably formed in response to the impact that created the Imbrium Basin. At the floor of the Alpine Valley is a long rille from which lava once erupted.
The web page for the program in which you just participated is at
Nightly Observing Program. Most of the above images were taken as
the Overnight Telescope Observing Program. For more information on this unique experience please visit Overnight Telescope Observing Program.
Copyright © 2020 Kitt Peak Visitor Center