Fact sheet
15529 is a very vesicular mare basalt that remains unstudied. It is similar to samples 15506 and 15056. Vesicles are 30% by volume; average 4mm, up to 7mm. Early reports suggest its composition is close to 50% plagioclase and 50% pyroxene, however large phenocrysts of olivine (see rotation 1) are present which must not have been seen earlier. The main accessory minerals are ilmenite, troilite and metallic iron.
The sample weighed 1531 grams before thin sections were made. It has not been dated.
Further details of this and other Apollo samples are here: http://curator.jsc.nasa.gov/lunar/
The Apollo 15 landing site was in the Apennine Highlands, and close to Hadley Rille — a long, narrow winding valley. Approximately 76 kg of lunar material, including soil, rock, core-tube and deep-core samples, were returned to Earth.
This mission was the first flight of the Lunar Roving Vehicle which allowed the astronauts to venture further from the Lunar Module than in previous missions. During three periods of extravehicular activity, or EVA, on July 31st, and August 1st and 2nd, Scott and Irwin completed a record 18 hours, 37 minutes of exploration, travelling 17.5 miles, in the first car that humans had ever driven on the Moon.
Apollo 15 was launched on 26 July 1971.