1. Enlarge level, glue paper and sifted soil photos using PhotoShop, or Paint.Net to show X and Y coordinates of fallen particles by pixel no. Common red ochre, charcoal and black manganese dioxide are easily seen in light soil or sand; yellow ochre and other pigments less so. Level and glue paper particle coordinates that do not match are counted separately,
  2. Petroglyph particles are fine dust. Hammerstone fragments are much larger and of different rock.2Some dust retains the dark outer manganese patina in desert art; some, the light-coloured rock interior. Where exterior and interior rock colour is similar, hammerstone fragments are used to define art levels.
  3. Table in columns by photo number; level; X and Y particle coordinates in level surface, glue paper, sifted soil photos and glue paper microscopy.
  4. Do particle locations match in level surface and inverted glue paper jpgs?
  5. Add distinct particle locations in part 25 to sifted level jpg locations. Total.
  6. Select bottom level with particles. Check glue sheet for AMS material.
  7. Remove particles with water-saturated Q-tip, place in gel caps, send to lab.
  8. As rock art sites were revisited in the past, upper particle levels can be dated. Particles falling from weathering are fewer than those from art application.

Petroglyph Dating Method