Safe. This movie tells about an excellent fighter who must deal with double-mission. He must rescue a 12-year-old girl kidnapped by the Triads and find a good.

With Jim Carrey, Gerry Becker, Greyson Erik Pendry, Brittany Colonna. Man on the Moon is a biographical movie on the late comedian Andy Kaufman. Kaufman, along with. The Moon has fascinated mankind throughout the ages. By simply viewing with the naked eye, one can discern two major types of terrain: relatively bright highlands and.

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The Moon. The Moon. I had the ambition to not only go farther than man had gone before. Captain Cook. Copyright © 1. Rosanna L. Hamilton.

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Moon Introduction. Additional Resources. Apollo Mission Publications.

Apollo Lunar Surface Journal. Apollo 1. 1. The Moon has fascinated mankind throughout the ages. By simply viewing with the naked eye, one can discern. By the middle of the. Galileo and other early. It has. also been known for more than a century that.

Moon is less dense than the Earth. Although a. certain amount of information was ascertained about the Moon before the. Current knowledge of the Moon. Earth. This lends to a greater understanding of geologic processes and further. On July 2. 0, 1. 96. Neil Armstrong became the first man to step onto the. Moon. He was followed by Edwin Aldrin, both of the Apollo.

They and other moon walkers experienced the effects of no. Radio communications were used because sound waves can only. The lunar sky is. The astronauts also experienced gravitational differences. The moon's. gravity is one- sixth that of the Earth's; a man who weighs 1.

Earth weighs only 3. Moon. (The equivalent. Newton, where 4. 4. Newtons equal one pound- force.).

The Moon is 3. 84,4. Earth. Its. diameter is 3,4. Both the rotation of the Moon and. Earth takes 2. 7 days, 7 hours, and 4. This. synchronous rotation is caused by an unsymmetrical distribution of mass.

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Earth's gravity to keep one lunar. Earth. Optical librations have. Very. small but real librations (maximum about 0°. Sun's gravity and the eccentricity of Earth's orbit. Moon's orbit and allowing cyclical preponderances of. Four nuclear powered seismic stations were installed during the Apollo.

Moon. There. is only residual tectonic activity due to cooling and tidal forcing, but. Lunar Module into the moon. The results have shown the Moon to have a crust. If this crust is uniform over the Moon, it would. Moon's volume as compared to the less than. Earth. The seismic determinations of a crust and mantle on. Moon indicate a layered planet with differentiation by igneous.

There is no evidence for an iron- rich core unless it were a. Seismic information has influenced theories about the. Moon. The Moon was heavily bombarded early in its history. Watch Jingle All The Way Online Jingle All The Way Full Movie Online on this page. Meteoritic. impacts brought a variety of "exotic" rocks to the Moon. The impacts also.

Moon rocks of great depth and distributed their fragments. The underlying crust was also thinned and cracked, allowing molten basalt. Because the Moon has. Earth. Rocks more than 4 billion years old still exist. Earth. Geological activity on the Moon consists of. It is thus considered geologically dead.

With such an active early. Moon is considered fossilized in time. The Apollo and Luna missions returned. Micrometeorite bombardment has thoroughly pulverized the. The. regolith, or lunar soil, is unconsolidated mineral grains, rock fragments.

It is found over the entire Moon, with the exception of steep. It is 2 to 8 meters. The dark, relatively lightly cratered maria cover about 1. Moon, mostly within. This concentration may be explained by the fact that the.

Moon's center of mass is offset from its geometric center by about. Earth, probably because the crust is thicker on the. It is possible, therefore, that basalt magmas rising from the.

Mare rocks are basalt and most date from. Some fragments in highland breccias date to. The maria average only a few hundred meters in thickness but are.

The relatively bright, heavily cratered highlands are called terrae. The craters and basins in the highlands are formed by meteorite impact. The dominant rock type in this region contain high contents of. Most. terrae breccias are composed of still older breccia fragments.

Other. terrae samples are fine- grained crystalline rocks formed by shock. Nearly all of the. The intense bombardment began 4. Moon's origin. Moon Statistics.

Mass (kg)7. 3. 49e+2. Mass (Earth = 1)1. Equatorial radius (km)1,7. Equatorial radius (Earth = 1)2. Mean density (gm/cm^3)3. Mean distance from Earth (km)3. Rotational period (days)2.

Orbital period (days)2. Average length of lunar day (days)2. Mean orbital velocity (km/sec)1. Orbital eccentricity.

Tilt of axis (degrees)1. Orbital inclination (degrees)5. Equatorial surface gravity (m/sec^2)1.

Equatorial escape velocity (km/sec)2. Visual geometric albedo. Magnitude (Vo)- 1. Mean surface temperature (day)1. CMean surface temperature (night)- 1.

CMaximum surface temperature. CMinimum surface temperature- 2.

CInterior of the Moon. This artist's conception shows the interior of the moon based off of new. NASA. The moon contains 5 major divisions in its interior. It possesses a solid, iron- rich inner core with a radius of nearly 1.

It has a partially molten boundary layer around the core estimated to. The moon's crust varies from tens of kilometers in depth (under mare basins) to. Copyright 2. 01. 1 Calvin J.

Hamilton)Lunar Nearside Spectacular! For two weeks in mid- December 2.

LRO spacecraft remained nadir looking (straight down) so that the LROC Wide Angle Camera (WAC) could acquire ~1. LROC team to construct this spectacular mosaic. As the Moon rotated under LRO's orbit, the ground track progressed from east to west (right to left in this mosaic), and the incidence angle at the equator increased from 6.

Courtesy NASA/GSFC/Arizona State University)Water Around a Fresh Crater. These images show a very young lunar crater on the side of the moon that. Earth, as viewed by NASA's Moon Mineralogy Mapper on the.

Indian Space Research Organization's Chandrayaan- 1 spacecraft. On the left. is an image showing brightness at shorter infrared wavelengths.

On the. right, the distribution of water- rich minerals (light blue) is shown around. Both water- and hydroxyl- rich materials were found to be.

Courtesy ISRO/NASA/JPL- Caltech/USGS/Brown Univ.)2. Lunar Eclipse. On Wednesday October 2. Earth's shadow for more. It began at 9: 1. EST with totality beginning at 1. The eclipse passed out of Earth shadow at 0. Copyright Calvin J.

Hamilton)Apollo 1. Whole Moon View. This full disc of the Moon was photographed by the Apollo 1. Earth coast homeward following a successful lunar landing. December 1. 97. 2.

Mare seen on this photo include Serentatis. Tranquillitatis, Nectaris, Foecunditatis and Crisium. Courtesy NASA)Moon - False Color Mosaic. This false- color photograph of the Moon was taken by the Galileo. December 8, 1. 99. The false- color processing used to.

Areas appearing red generally correspond to the lunar. Bluer mare areas contain more titanium than. Mare Tranquillitatis, seen as a deep blue patch on. Mare Serenitatis, a slightly smaller.

Mare. Tranquillitatis. Blue and orange areas covering much of the left side of. Moon in this view represent many separate lava flows in Oceanus. Procellarum. The small purple areas found near the center are pyroclastic. The fresh crater Tycho.

Far Side of the Moon. This image was taken by Apollo 1.

It shows a portion. Moon's heavily cratered far side. The large crater is. The rugged terrain seen here is typical of the farside of the Moon. Courtesy NASA)Lunar South Pole. This mosaic is composed of 1,5. Clementine images.

Moon. The top half of the mosaic. Earth. Clementine has revealed what appears to be a major.

This depression probably is an. A. significant portion of the dark area near the pole may be in permanent. The impact basin Schrodinger (near the 4 o'clock position) is a. Moon. The center of Schrodinger is flooded by lavas. A volcanic vent seen in the floor of Schrodinger is one of. Moon. (Courtesy Naval Research Laboratory.)Apollo 1. The Apollo 1. 1 Lunar Module (LM).

Astronauts Neil A. Armstrong. and Edwin E.

Aldrin Jr. aboard, is photographed from the Command and. Service Module (CSM) during rendezvous in lunar orbit. The LM. was making its docking approach to the CSM. Astronaut Michael Collins. CSM in lunar orbit while the other two crewmen explored. The large, dark- colored area in the background is.

Smyth's Sea, centered at 8. This view looks west. The Earth. rises above the lunar horizon. Courtesy NASA)Apollo 1.

Flag. Astronaut Edwin E.