Geology Project - OF THE TURNS AND POINT BARS ALONG THE...

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MY GEOLOGIC EXPERIENCE
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PALOUSE FALLS
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A SLUMP OCCURS WHEN UNCONSOLIDATED SOIL RAPIDLY SLIDES ALONG A CURVED SURFACE
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THIS ALLUVIAL FAN WAS CREATED AS A RESULT OF THE SEDIMENTS TRANSPORTED AND DEPOSITED BY WATER FROM THE NARROW CHANNEL ABOVE
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THIS SEDIMENTARY STRUCTURE, KNOWN AS MUDCRACKS, OCCURS WHEN MUD DRIES
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THESE RIPPLE MARKS HAVE BEEN FORMED BY EITHER WIND OR WATER CURRENTS
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THESE TRACKS (MOST LIKELY FOOTPRINTS) HAVE BEEN PRESERVED AS SEDIMENTARY STRUCTURES
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MEANDERING RIVERS SUCH AS THIS ONE CREATE CUT BANKS ALONG THE OUTSIDE
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Unformatted text preview: OF THE TURNS AND POINT BARS ALONG THE INSIDE LEWISTON THESE FENCES WERE ONCE VERTICAL BUT A TYPE OF MASS WASTING KNOWN AS CREEP CAUSED THE UNCONSOLIDATED SOIL TO MOVE SLOWLY DOWN SLOPE UNDER THE INFLUENCE OF GRAVITY ANOTHER ALLUVIAL FAN!!! THIS ROCK FORMATION IS THE RESULT OF ROCKSLIDES THAT OCCUR ALONG THE PLANES OF WEAKNESS BIG SLUMPS IN LEWISTON!!! THIS IGNEOUS INTRUSION IS CALLED A SILL, AND IS QUITE COMMON IN THE PALOUSE A YOUNG RIVER STARTING TO MEANDER THE END...
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Geology Project - OF THE TURNS AND POINT BARS ALONG THE...

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