3 D slike
ASTRONOMY


SLIKE

Za to stran ima največ zaslug Mitja Šiška, ki je izbrskal revijo.



Oglej si 3D posnetke Lune.
Nekaj posnetkov iz
http://www.nasm.edu/apollo30th/moontheater/anaglyph.html



Misija Apollo 12.


A computer generated 3-D globe of the Moon, based upon a USGS airbrush map wrapped around a sphere. The Moon's dark "mare" areas are located mostly on its near side, the side we can see from Earth.


Much of the Earth-facing side of the Moon is covered in dark mare material consisting of volcanic basalt rock. Shallow raised wrinkle ridges and many winding sinuous rilles are evident in this photo. In the center is the 14 mile (22km) diameter crater, Krieger. The north-east trending sinuous rilles come from the direction of the Aristarchus plateau just outside the lower portion of the photo. (Apollo 15 Metric camera stereo photo AS2478 & 2479, orbit 70)


This is a computer-generated 3-D view of a digital elevation model, with an ortho-image overlaid, that was extracted from an Apollo 15 Metric camera oblique stereo pair (AS-15-M3-1445 & 1446, orbit 35). The outer western rim of Tsiolkovsky crater shows the remains of a huge landslide. The stereo effect has been greatly exaggerated here to enhance detail present in the feature.


This is a close-up view of the surface containing small lunar rocks, some of which are cracked. The Apollo 11 astronauts were equipped with a "walking stick" containing a close-up stereo flash camera that could photograph an area of the surface some 3x3 inches square (8x8 cm sq.). The Moon's surface has been heavily pitted with micrometeorite craters and covered by a layer of dust and debris from surrounding craters. The soils were found to be very powdery and contained some small shiny spherical particles.


The yellow dot shows the landing site of Apollo 17 - the last manned mission to the Moon. Apollo 17 landed on the floor of a deep narrow valley containing dark soil. The valley is bounded on three sides by highlands which form part of the eastern rim of the Serenitatis basin. Using the lunar rover, the crew traveled 19 miles (30km), a distance equivalent to the diameter of the partly buried Littrow crater, found half-way between the center and the upper-right corner of the photo. During the mission the astronauts discovered some orange soil that turned out to consist of colored glass beads which had been produced during volcanic eruptions. (Apollo 17 Metric stereo camera photo AS-17-M-446 & 447, orbit 13/14)


Some of the larger craters on the Moon have central peaks. Central peaks are thought to be due to rebound from stresses released after crater formation. Tsiolkovsky, the lunar far-side crater shown here, is 115miles (185km) in diameter. Basaltic lava has flooded the crater's floor giving it a dark smooth appearance. Material from landslides can be seen around the edge of the floor. (Apollo 15 Metric camera stereo photo AS 15-M3-2798 & 2799, orbit 74)




Za astronomski krožek: ZORKO Vičar


RFC-822: Zorko.Vicar@guest.arnes.si


Nazaj na domačo stran.