Class 11: Discussion Notes

Strata and Maps

Maps

  • Various efforts in geognosy tradition, capped by Cuvier and Brongniart (1808, 1811)
  • Smith’s map of Britain
    • Essentially completed around 1803, published 1815
    • Unique shading
    • Formation names: locality + lithology
    • Not readily comparable to parallel efforts elsewhere
    • Recognition of characteristic fossils of specific formations
  • Webster’s map and sections of the Isle of Wright Basin (1814)
    • Uppermost Secondary (Chalk) and lowest Tertiary strata
    • Both deformed (folded)
    • Attempted to match Tertiary beds to Paris Basin using lithology

Formation Issues

  • Shift from gebrige to formation
    • Gebrige: lithology/mineralogy, dip, position, altitude
    • Formation: lithology, position in sequence
  • Correlation
    • Criteria tried: rock type, structural position, dip, altitude, fossils
    • By 1820, rock type still predominate one
    • Fossil info noted but not yet primary criteria
    • International correlations emerge by early 1820s

Ideas on Geology around 1820

  • Examples
    • London: London Basin
    • Milan-Turin: Po Valley
    • Naples: Volcanic fields
    • Edinburgh: Scottish Lowlands and Southern Uplands
    • Zurich: High Alps and Tertiary lowland (Swiss Plain)
  • General ideas
    • Tertiary
      • Isolated basins
      • Identify and map formations; include fossils
      • Attempt to correlate basins
      • Work out relation of sediments to adjacent uplands
    • Secondary
      • Section more regular across Europe (i.e., Coal Measures to Chalk)
      • Need to add fossil data and map new areas (Scotland, Switzerland, etc.)
    • Primary and Volcanics
      • Work on relationships between these and stratified units (ex: dikes)
      • Recall problems of origin of basalt and magmas
      • Examine dip and altitude of crystalline rocks
    • Sea level fall (classic model) versus uplift (new idea)
      • Need to figure this out
      • Tertiary sections high in the Alps (?)
    • Correlation
      • By this time, rock type is the most useful
      • Other geognost criteria fail
      • Need to test fossils as tools