1485 feet

It was another full day of processing core for us, down to 1485 ft.  Much of the core was highly fractured, and there was even some fine-grained sediment in some of the runs that we looked at.  The sediment occurred in two different styles: 1) unconsolidated and mixed with other, larger rock over a distinct depth interval within a run, or 2) strongly compacted into a fracture and giving the appearance of solid rock.  I'll try and get a good photo of the latter style (fracture fill) to post on the blog tomorrow.