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  2. Wabash Valley seismic zone - Wikipedia

    en.wikipedia.org/wiki/Wabash_Valley_Seismic_Zone

    Locations of quakes magnitude 2.5 or greater in the Wabash Valley (upper right) and New Madrid (lower left) Seismic Zones. The Wabash Valley seismic zone (also known as the Wabash Valley fault system or fault zone) is a tectonic region located in the Midwestern United States, centered on the valley of the lower Wabash River, along the state line between southeastern Illinois and southwestern ...

  3. Sandwich Fault Zone - Wikipedia

    en.wikipedia.org/wiki/Sandwich_Fault_Zone

    The Sandwich Fault Zone is a fault zone that runs northwest from Oswego to Ogle County, transecting Lee County in Northern Illinois. The fault has generally not been active, although a minor earthquake was reported in 2002 and 2010. [ 1 ]

  4. Template:Infobox fault - Wikipedia

    en.wikipedia.org/wiki/Template:Infobox_fault

    Template: Infobox fault. ... Download as PDF; Printable version; ... This template formats a right-side infobox to be used in articles about faults and fault zones.

  5. Des Plaines crater - Wikipedia

    en.wikipedia.org/wiki/Des_Plaines_crater

    The crater is buried beneath 75 to 200 feet (23–60 m) of glacial till and can only be seen as a series of faults and deformations in well logs and seismic surveys. [3] Faulting in the structure has produced as much as 600 feet (180 m) of vertical displacement. [3]

  6. 1968 Illinois earthquake - Wikipedia

    en.wikipedia.org/wiki/1968_Illinois_earthquake

    Scientists eventually realized, though, that the cause was a then-unknown fault, the Cottage Grove Fault, a small tear in the Earth's rock in the Southern Illinois Basin near the city of Harrisburg, Illinois. The fault, which is aligned east–west, is connected to the north–south-trending Wabash Valley Fault System at its eastern end. [15]

  7. Megathrust earthquake - Wikipedia

    en.wikipedia.org/wiki/Megathrust_earthquake

    A thrust fault is a type of reverse fault, in which the rock above the fault is displaced upwards relative to the rock below the fault. This distinguishes reverse faults from normal faults , where the rock above the fault is displaced downwards, or strike-slip faults , where the rock on one side of the fault is displaced horizontally with ...