Help Shape the Future of Space Exploration

Join The Planetary Society Now  arrow.png

Join our eNewsletter for updates & action alerts

    Please leave this field empty
The Bruce Murray Space Image Library

A lunar basalt (Apollo 11 sample 10062)

Filed under explaining science, the Moon, NASA lunar missions before 2005, geology, mineralogy and petrology

Go Back

A lunar basalt (Apollo 11 sample 10062) Color photograph of Apollo 11 Sample 10062. The ruler is marked in centimeters. The rock is a high-titanium basalt, and very old, 3.8 billion years old, dating to the time of the Late Heavy Bombardment.

NASA

According to the Lunar Sample Compendium, Apollo 11 sample 10062 is "an old, low-K, high-Ti basalt from Apollo 11. Based on texture and composition, James and Wright (1972) termed 10062 an ophitic ilmenite basalt, whereas Gamble et al. (1978) describe the texture as subophitic (figure 1).  At 3.8 b.y., basalt 10062 is one of the oldest lunar mare basalts (other than those found as clasts in breccias).  It has been exposed to cosmic rays for 90 m.y. (the apparent age of West Crater)."

"The texture is ophitic, with radiating lath-like and acicular crystals of plagioclase, intergrown with tabular and skeletal crystals of ilmenite, irregular grains of zoned clinopyroxene and olivine (figure 2).  Late stage silica, fayalite, ulvöspinel, troilite and apatite are present in the mesostasis. The abundance of ilmenite is striking, with some grains as large as ~ 1 mm.  Some ilmenite has relict cores of armalcolite, which appears to have been replaced and overgrown by ilmenite."

Original image data dated on or about January 24, 1969

 

Other Related Images

Comments:

Leave a Comment:

You must be logged in to submit a comment. Log in now.

Space in Images

Pretty pictures and
awe-inspiring science.

See More

Join the New Millennium Committee

Let’s invent the future together!

Become a Member

Connect With Us

Facebook! Twitter! Google+ and more…
Continue the conversation with our online community!