ABSTRACT 
      The Ganson Hill study area is located in the Giddings Brook Slice
      of the Taconic Allochthon. It contains rocks of Cambrian(?),
      Cambrian and Ordovician age. The predominant rock type is slate
      with subordinate lithologies including quartzite, limestone,
      micrite, arenite and graywacke. The lithostratigraphy identified
      in the Ganson Hill area extends from the basal Bomoseen wacke to
      the Poultney slate. A more precisely defined lithostratigraphy is
      derived from the study area by the occurrence and recognition of
      the Middle Granville Slate Formation and the documentation of a
      second Cambrian black/green boundary. Previous workers have
      included this formation in different places, in two different
      formations creating much confusion. 
      Three stages of deformation have been recognized in the Ganson
      Hill study area. They are: pre-slaty cleavage folding, slaty
      cleavage development with associated folding, and faulting and
      seen only sporadically, crenulation cleavage development with
      associated folding and faulting. Documented in this thesis is the
      Hubbardton Gulf Thrust Fault which places Cambrian green slate
      (Undifferentiated Bull Fm.) over black and gray slate with
      interbedded quartzite (Poultney Fm.). 
      An early Ordovician contourite deposit has been identified in the
      Poultney unit. The grain size, the composition and the lateral
      extent of the quartz-rich beds in the Poultney Formation in
      addition to sharp top and bottom bedding contacts and preserved
      sedimentary structures are distinguishing characteristics of the
      contourite deposit. Paleocurrent directions indicate northerly
      flowing bottom currents depositing and reworking material fed from
      the North American Platform adjacent to and south of the present
      area of the Taconics. 
Aparisi, M., 1985. Stratigraphy and structure of the Ganson Hill
      area: northern Taconic Allochthon. Unpublished MSc. thesis, State
      University of New York at Albany. 128 pp., +ix; 3 folded plates
      (maps) 
      University at Albany Science Library call number:  SCIENCE
      Oversize (*) QE 40 Z899 1985 A65
    
MS thesis scanned
        image pdf (10 MB)
      
      
          Plate 1 - Map
        of Occurrence of the Poultney Formation
              (uncoloured geological
      outline map, scale 1:250,000) - 1MB pdf file
      Geological Map and cross-sections 
          Plate 2 -  Geological
        Map of the Ganson Hill area - northern Taconic Allochthon
              (coloured outcrop map, scale
      1: 12,000) - 9 MB pdf file
          Plate 3 - Cross
        sections of the Ganson Hill area
              (uncoloured geological cross
      sections, scale 1: 12,000) - 1.5MB pdf file
    
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