Fact sheet
14315 is a coherent breccia in which light clasts are dominant. The estimated percentage of clasts is 40 percent. The matrix is medium grey and appears to have an unusual fabric. Modelling of its bulk composition suggests it contains 45 % of a ferroan anorthosite component.
14315 weighed 115 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.