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    Thumbnail 1 of 7, Cap, Fault Line Ridge designed and sold by Beardeaux.
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    Cap, Fault Line Ridge designed and sold by Beardeaux
    ColorWhite

    Fault Line Ridge Cap

    Designed and sold by Jason Tompkins
    $20.15
    $25.19 (20% off)
    20% off ends soon
    Style
    Size
    $20.15
    $25.19 (20% off)
    • Super-easy returnsProblem? No problem. We’ll fix it, fast.

    Product features

    • Get your head in the game with this well-constructed baseball-style cap
    • Structured, medium-to-high-profile crown with curved bill and firm inner lining
    • Snapback closure for adjustable fit
    • 100% polyester, fabric weight 8.4 oz / 285gsm
    • Five-panel design with double-wide front panel for seamless printing
    • Sized for ages 13+
    • Spot clean with damp cloth
    • Since every item is made just for you by your local third-party fulfiller, there may be slight variances in the product received
    Artwork thumbnail, Fault Line Ridge by Jason Tompkins
    Fault Line Ridge
    In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust result from the action of plate tectonic forces, with the largest forming the boundaries between the plates, such as the megathrust faults of subduction zones or transform faults. Energy release associated with rapid movement on active faults is the cause of most earthquakes. Faults may also displace slowly, by aseismic creep. A fault plane is the plane that represents the fracture surface of a fault. A fault trace or fault line is a place where the fault can be seen or mapped on the surface. A fault trace is also the line commonly plotted on geologic maps to represent a fault. A fault zone is a cluster of parallel faults. However, the term is also used for the zone of crushed rock along a single fault. Prolonged motion along closely spaced faults can blur the distinction, as the rock between the faults is converted to fault-bound lenses of rock and then progressively crushed.

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