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English: An intrusion (Notch Peak monzonite) inter-fingers (partly as a dike) with highly-metamorphosed host rock (Cambrian carbonate rocks). From near Notch Peak, House Range, Utah. According to Utah Geological Survey, this is the Notch Peak Sill, a sill of quartz monzonite which, about 17 million years ago, intruded into the layers of white marble and grey argillite of the Marjum Formation. Reference: http://geology.utah.gov/surveynotes/geosights/notch_peak.pdf .
日期 (UTC) (Uploaded on Commons at 2011-03-27 09:48:29 (UTC)/Original uploaded at 2009-12-10 18:17:41)
來源 I (Matt Affolter (talk)) created this work entirely by myself. (Original uploaded on en.wikipedia)
作者 Matt Affolter (talk) (Transferred by Citypeek/Original uploaded by Qfl247)

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The original description page was here. All following user names refer to en.wikipedia.
  • 2009-12-10 18:17:41 Qfl247 3,648×2,736 (3.44 MB) ({{Information |Description = An intrusion ([[Notch Peak]] [[monzonite]]) inter-fingers (partly as a [[dike]]) with highly-metamorphosed host rock ([[Cambrian]] [[carbonate rock]]s). From [[Sawtooth Canyon]], near Notch Peak, [[House Range]], [[Utah]])
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Intrusion of Notch Peak monzonite with highly-metamorphosed host rock of Cambrian carbonate

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