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Explore the geological section of Tinière Valley in Lubbock as studied by Adolf Morlot in 1896. Discover the Quaternary time measure through a diagrammatic section showing layers from Roman to Stone Age levels.
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AdolfMorlotthe Measure of Quarternary Time by Leonard G Wilson
Geological section of the Tinière valley in Lubbock, Scenery of Switzerland, 1896
Clarens Section Glacial clay containing limestone blocks Alluvium containing rounded pebbles
Beginning of railway cut at Villeneuve through the southern half of the Tinière cone.
Diagrammatic section throughTinière cone, showing Roman (Iron),Bronze, and Stone Age levels
Adolf Morlot 1820 - 1867 Sir Charles Lyell 1797 - 1875
Older and higher Tinièreconeabove and behind the modern cone