Page 190 - Laboratory Manual in Physical Geology
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SEDIMENTARY STRUCTURES


                                    ILLUSTRATIONS                           DESCRIPTIONS          ENVIRONMENTS

                           Raindrop                                     RAINDROP
                          impressions                                   IMPRESSIONS:           Raindrop impressions
                                                                        Tiny craters formed by  occur on muddy land
                                                                        raindrops as they impact  surfaces.
                                                                        bedding plane surfaces.




                                                                                               Horizontal strata occur
                                                        Horizontal      HORIZONTAL             where sediments settle
                                                         strata
                                                                        STRATA:                from a standing body of
                                                                        Relatively flat beds   water or air; or where
                                                                        (≥ 1cm thick) and      currents travel parallel to the
                                                                        laminations (< 1cm thick).  surface on which sediments
                                                                                               are accumulating.


                                                                                               Graded beds form when
                                                                        GRADED BED:            a turbulent body of
                                                                        Stratum that contains  water full of sediment
                                                                        different sizes of sedimentary  (flood, wave, river)
                                                                        grains arranged from largest  suddenly loses energy
                        Graded beds
                                                                        at the bottom of the bed to  and calms down. Large
                                                                        smallest at the top.   particles settle out
                                                                                               before small.
                                                Flow direction
                            Current ripple
                              marks              (air or water)
                                                                        CURRENT                Current ripple marks form
                                                                        RIPPLE MARKS:          in any environment where
                                                                        Asymmetrical ripple marks.  wind or water travels in
                                                                        The steep slope faces down  one direction for some of the
                                                                        current, and the gentle slope  time: rivers, ocean currents,
                                                                        faces up current.      wind blowing sand dunes.

                   Cross-bedding


                                                                        CROSS-BEDDING:         Cross-bedding forms
                                                                        Inclined beds or       wherever there are wind
                                                                        laminations.           or water currents.
                             inclined
                               to
                              right
                     Bimodal
                      cross-
                     bedding
                             inclined
                               to                                       BIMODAL                Bimodal cross bedding
                               left                                     CROSS-BEDDING:         forms in environments
                                                                        Sequence of cross-bedding  where currents of wind
                                                                                               or water flow back and
                                                                        in which cross-bedding of   forth in opposite
                                                                        current ripple marks is
                                      Oscillation back and forth (water)                       directions. It is common
                    Wave                                                inclined in opposite   in environments with tides.
                    ripple                                              directions.
                    marks
                                                                                               Wave (symmetrical) ripple
                                                                                               marks form in any body of
                                                                        WAVE RIPPLE MARKS:     water where gentle waves
                                                                        Symmetrical ripple marks.  barely touch bottom, or
                                                                                               where weak currents move
                  Cross-bedding                                                                back and forth (oscillate) in
                                                                                               shallow water.



                 FIGURE 6.12    Sedimentary structures.




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