unconformity$506209$ - definizione. Che cos'è unconformity$506209$
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Cosa (chi) è unconformity$506209$ - definizione

THE HUGE GAP IN GEOLOGY
Powell’s Unconformity
  • An exposure of Powell's Great Unconformity, west of Montezuma, New Mexico
  • foliated]] and veined [[schist]]s  of the [[Vishnu Basement Rocks]] truncated at the base of the Tonto Group
  • upright=1.35
  • 250px

Great Unconformity         
Of the many unconformities (gaps) observed in geological strata, the term Great Unconformity is frequently applied to either the unconformity observed by James Hutton in 1787 at Siccar Point in Scotland,Rance, H (1999) Historical Geology: The Present is the Key to the Past. QCC Press, New York or that observed by John Wesley Powell in the Grand Canyon in 1869.
Unconformity         
  • Angular unconformity
  • Disconformity
  • John Clerk]] in 1787 and photographed in 2003.
  • Nonconformity
  • Paraconformity
DISTORTED SEDIMENT DEPOSITION
Unconformity (geology); Angular unconformity; Noncomformity; Disconformity; Tilt sequence; Unconformable; Paraconformity; Discomformity; Unconformably; Unconformities; Uncomformities; Hiatus (stratigraphy); Hiatus (geology); Unconformable surface; Disconformity (geology)
·noun Want of parallelism between strata in contact.
II. Unconformity ·noun Want of conformity; incongruity; inconsistency.
Unconformable         
  • Angular unconformity
  • Disconformity
  • John Clerk]] in 1787 and photographed in 2003.
  • Nonconformity
  • Paraconformity
DISTORTED SEDIMENT DEPOSITION
Unconformity (geology); Angular unconformity; Noncomformity; Disconformity; Tilt sequence; Unconformable; Paraconformity; Discomformity; Unconformably; Unconformities; Uncomformities; Hiatus (stratigraphy); Hiatus (geology); Unconformable surface; Disconformity (geology)
·adj Not conformable; not agreeable; not conforming.
II. Unconformable ·adj Not conformable; not lying in a parallel position; as, unconformable strata.

Wikipedia

Great Unconformity

Of the many unconformities (gaps) observed in geological strata, the term Great Unconformity is frequently applied to either the unconformity observed by James Hutton in 1787 at Siccar Point in Scotland, or that observed by John Wesley Powell in the Grand Canyon in 1869. Both instances are exceptional examples of where the contacts between sedimentary strata and either sedimentary or crystalline strata of greatly different ages, origins, and structure represent periods of geologic time sufficiently long to raise great mountains and then erode them away.