| Caves in the alcove in Painted Rock are forming from the gradually 
      weathering of irregularly-cemented sandstone due to infrequent wetting and 
      drying. In the past, wind-blown dust and soil probably filled the alcove 
      to higher levels and chemical weathering associated with shallow groundwater 
      may have assisted in the development of the caves. The overhangs in and 
      around Painted Rock are some of the only natural shelter areas in a large 
      region and must have been attractive destinations to prehistoric peoples 
      utilizing the Soda Lake area. |