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  1. Strained metaconglomerate that crops out in a stream in Klingle Valley, DC. Note the prominent granite intrusion. PINK = Granite contact BLUE = Sericite after staurolite pseudomorphs YELLOW = Outlines of stretched clasts within the metaconglomerate GREEN = Edges of lichens growing on the surface of the outcrop ...

  2. Strained metaconglomerate that crops out in a stream in Klingle Valley, DC. Note the prominent granite intrusion. Compare with this annotated view: gigapan.com/gigapans/128969 Or view them both simultaneously in the comparative viewer from GIGAmacro.com: www.gigamacro.com/gigamacro_viewer/gigama Will open in a new tab or window...

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      Explore Score
      32

  3. Strained metaconglomerate that crops out in a stream in Klingle Valley, DC. Retrograde metamorphism is apparent, with sericite-after-starulote pseudomorphs.

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      119
      Explore Score
      34

  4. Strained metaconglomerate that crops out in a stream in Klingle Valley, DC.

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      109
      Explore Score
      27

  5. Strained metaconglomerate that crops out in a stream in Klingle Valley, DC. This is a slightly higher-resolution shoot of the same scene depicted here: gigapan.com/gigapans/128504

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      100
      Explore Score
      35

  6. Strained metaconglomerate that crops out in a stream in Klingle Valley, DC. A slightly lower-positioned, closer version of this same outcrop is imaged in this second GigaPan: gigapan.com/gigapans/128509

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      127
      Explore Score
      38

  7. Strained metaconglomerate that crops out in a stream in Klingle Valley, DC.

    • Order Print

    • Stats

      Favorites
      0
      Comments
      Snapshots
      Total Views
      132
      Explore Score
      27

  8. The contact between the metasedimentary Fauquier Formation (uppermost marble member) and the overlying metavolcanic Catoctin Formation is exposed in an abandoned quarry north of Aldie, Virginia, across Goose Creek from Lime Kiln Road. The nature of this contact (is it conformable? does it show primary or tectonic struc...

  9. The contact between the metasedimentary Fauquier Formation (uppermost marble member) and the overlying metavolcanic Catoctin Formation is exposed in an abandoned quarry north of Aldie, Virginia, across Goose Creek from Lime Kiln Road. The nature of this contact (is it conformable? does it show primary or tectonic struc...

  10. The contact between the metasedimentary Fauquier Formation (uppermost marble member) and the overlying metavolcanic Catoctin Formation is exposed in an abandoned quarry north of Aldie, Virginia, across Goose Creek from Lime Kiln Road. The nature of this contact (is it conformable? does it show primary or tectonic struc...

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