Fact sheet
14312 is a coherent breccia with a moderate percentage of angular dark clasts which tend to blend with the light matrix. A very few light clasts are also present. It is composed of more matrix, and less clasts than other breccias from Apollo 14. Clasts in 14312 include, dark matrix breccias, Al-rich mare basalt, poikilitic impact melt, and individual minerals.
The sample weighed 299 grams before analysis. It has not been dated.
Further details of this and other Apollo samples are here: http://curator.jsc.nasa.gov/lunar/
The Apollo 14 landing site was in a region formed by impact-basin debris.
Most of the 42 kilograms of rocks and soil collected on Apollo 14 are breccias (rocks that are composed of fragments of other, older rocks). In some cases, the rock fragments that form a breccia are themselves breccias. Such rocks obviously have experienced complex histories with multiple generations of impact events. Some breccias were heated enough that some of the material in the rock was melted.
Apollo 14 was launched on 31 January 1971.