Ripple marks - wikipedia Ripple marks Ancient wave ripple marks in sandstone, Moenkopi Formation, Capitol Reef National Park, Utah In geology, ripple marks are sedimentary structures ( i.e. bedforms of the lower flow regime ) and indicate agitation by water ( current or waves ) or wind. Contents 1 Defining ripple cross-laminae and asymmetric ripples 2 Ripple marks in different environments 2.1 Wave - formed ripples 2.2 Ripple marks formed by aeolian processes 3 Definitions 4 See also 5 References 6 External links Defining ripple cross-laminae and asymmetric ripples Ripple marks in Cretaceous Dakota Formation, east side of Dinosaur Ridge. Scale bar on notebook is 10 cm. Ripple beds in the Wren 's Nest National Nature Reserve, Dudley, England Wave / symmetrical ripple, Nomgon, Mongolia Cross-section through asymmetric climbing ripples, seen in the Zanskar Gorge, Ladakh, NW Indian Himalaya. Ripples climb when sediment fluxes in the flow are very high. Current ripple marks, unidirectional ripples, or asymmetrical ripple marks are asymmetrical in profile, with a gentle up - current slope and a steeper down - current slope. The down - current slope is the angle of repose, which depends on the shape of the sediment. These commonly form in fluvial and aeolian depositional environments, and are a signifier of the lower part of the Lower Flow Regime. Ripple cross-laminae forms when deposition takes place during migration of current or wave ripples. A series of cross-laminae are produced by superimposing migrating ripples. The ripples form lateral to one another, such that the crests of vertically succeeding laminae are out of phase and appear to be advancing upslope. This process results in cross-bedded units that have the general appearance of waves in outcrop sections cut normal to the wave crests. In sections with other orientations, the laminae may appear horizontal or trough - shaped, depending upon the orientation and the shape of the ripples. Ripple cross-laminae will always have a steeper dip downstream, and will always be perpendicular to paleoflow meaning the orientation of the ripples will be in a direction that is ninety degrees to the direction that current if flowing. Scientists suggest current drag, or the slowing of current velocity, during deposition is responsible for ripple cross-laminae. Types Straight Straight ripples generate cross-laminae that all dip in the same direction, and lay in the same plane. These forms of ripples are constructed by unidirectional flow of the current. Sinuous Sinuous ripples generate cross-laminae that are curvy. They show a pattern of curving up and down as shown in picture. Sinuous ripples produce trough cross lamination. All laminae formed under this type of ripple dip at an angle to the flow as well as downstream. These are also formed by unidirectional flow of current. Catenary Catenary ripples generate cross-laminae that are curvy but have a unidirectional swoop. They show a pattern similar to what a repeated `` W '' would look like. Like the sinuous ripples, this form of ripple is created by unidirectional flow with the dip at an angle to the flow as well as downstream. Linguoid / Lunate Linguoid ripples have lee slope surfaces that are curved generating a laminae similar to caternary and sinuous ripples. Linguoid ripples generate an angle to the flow as well as downstream. Linguoid ripples have a random shape rather than a `` W '' shape, as described in the catenary description. Lunate ripples, meaning crescent shaped ripples, are exactly like linguoid ripples except that the stoss sides are curved rather than the lee slope. All other features are the same. Size ( scale ) Size Description Very small Very small cross-lamination means that the ripple height is roughly one centimeter. It is lenticular, wavy and flaser lamination. Small Small cross-bedding are ripples set at a height less than ten centimeters, while the thickness is only a few millimeters. Some ripples that may fit this category are wind ripples, wave ripples, and current ripples. Medium Medium cross-lamination are ripples with a height greater than ten centimeters, and less than one meter in thickness. Some ripples that may fit this category would be current - formed sand waves, and storm - generated hummocky cross stratification. Large Large cross-bedding are ripples with a height greater than one meter, and a thickness equivalent to one meter or greater. Some ripples that may fit this category would be high energy river - bed bars, sand waves, epsilon cross-bedding and Gilbert - type cross-bedding. Ripple marks in different environments Wave - formed ripples Tidal megaripples in the Random Formation Main article : Wave - formed ripple Also called bidirectional ripples, or symmetrical ripple marks have a symmetrical, almost sinusoidal profile ; they indicate an environment with weak currents where water motion is dominated by wave oscillations. In most present - day streams, ripples will not form in sediment larger than coarse sand. Therefore, the stream beds of sand - bed streams are dominated by current ripples, while gravel - bed streams do not contain bedforms. The internal structure of ripples is a base of fine sand with coarse grains deposited on top since the size distribution of sand grains correlates to the size of the ripples. This occurs because the fine grains continue to move while the coarse grains accumulate and provide a protective barrier. Ripple marks formed by aeolian processes See also : aeolian processes Wind ripples on crescent - shaped sand dunes ( Barchans ) in Southwest Afghanistan ( Sistan ). Normal ripples Also known as impact ripples, these occur in the lower part of the lower flow regime sands with grain sizes between 0.3 - 2.5 mm and normal ripples form wavelengths of 7 - 14 cm Normal ripples have straight or slightly sinuous crests approximately transverse to the direction of the wind. Megaripples These occur in the upper part of the lower flow regime where sand with bimodal particle size distribution forms unusually long wavelength of 1 - 25 m where the wind is not strong enough to move the larger particles but strong enough to move the smaller grains by saltation. Fluid drag ripples Also known as aerodynamic ripples, these are formed with fine, well - sorted grain particles accompanied by high velocity winds which result in long, flat ripples. The flat ripples are formed by long saltation paths taken by grains in suspension and grains on the ground surface. Definitions Crest and trough Crest The point on a wave with the maximum value or height. It is the location at the peak of the wave cycle as shown in picture to the right. Trough The opposite of a crest, so the minimum value or height in a wave. It is the location at the very lowest point of a wave cycle also shown in picture to right. Lee The lee side has a steeper slope than the stoss. The lee is always on the back side of the ripple, which is also on the opposite side of where the current flow meets the ripple. The current flows down the lee side. Stoss The stoss is the side of a wave or ripple that has a gentle slope versus a steeper slope. Current always flows up the stoss side and down the lee side. This can be used to determine current flow during the time of ripple formation. See also Capillary wave Giant current ripples Water on Mars - sedimentary ripple marks show indirect evidence of ancient water flows on our neighbor planet References Wikimedia Commons has media related to Ripple marks. Easterbrook, Don J. Surface processes and landforms. Upper Saddle River, N.J : Prentice Hall, 1999. Print. ISBN 0 - 13 - 860958 - 6 pp. 479 - 480. Greeley, Ronald, and James D. Iversen. Wind as a Geological Process On Earth, Mars, Venus and Titan ( Cambridge Planetary Science Old ). New York : Cambridge UP, 1987. ISBN 0 - 521 - 35962 - 7 pp. 153 - 154 Monroe, James S., and Reed Wicander. The Changing Earth : Exploring Geology and Evolution, 2nd ed. Belmont : West Publishing Company, 1997. ISBN 0 - 314 - 09577 - 2 pp. 114 - 15, 352. Jump up ^ Boggs Jr., Sam. ( 2006 ) Principles of Sedimentology and Stratigraphy, 4th ed. Jump up ^ Potter, Pettijohn. ( 1977 ) Paleocurrents and Basin Analysis Jump up ^ Nichols, Gary. ( 2009 ) Sedimentology and Stratigraphy, Wiley, ISBN 978 - 1405135924 Jump up ^ Stow, Dorrik A.V., ( 2009 ) Sedimentary Rocks in the Field : A Color Guide, Academic Press, ISBN 978 - 0123694515 Jump up ^ Tidal deposits of the Lower Cambrian Random Formation, eastern Newfoundland : facies and paleoenvironments. Richard N. Hiscott. Canadian Journal of Earth Sciences, 1982, 19 ( 10 ) : 2028 - 2042, https://doi.org/10.1139/e82-180... External links Ripple Marks and Uniformitarianism Unidirectional flow : Sand ripples and grain distribution 2D model Unidirectional flow : Sand ripples and topography 2D model Waves : Sand ripples and grain distribution 2D model Waves : Sand ripples and topography 2D model NDL : 00569398 Retrieved from `` https://en.wikipedia.org/w/index.php?title=Ripple_marks&oldid=819779416 '' Categories : Sedimentary structures Patterned grounds Talk Contents About Wikipedia Català Deutsch Eesti Español Euskara فارسی Français 한국어 Italiano עברית Nederlands 日本 語 Norsk nynorsk Polski Русский Svenska ไทย Türkçe Українська Edit links This page was last edited on 11 January 2018, at 06 : 34. Text is available under the Creative Commons Attribution - ShareAlike License ; additional terms may apply. By using this site, you agree to the Terms of Use and Privacy Policy. Wikipedia ® is a registered trademark of the Wikimedia Foundation, Inc., a non-profit organization. About Wikipedia

Question: what do ripple marks in sedimentary rock mean
Answer: agitation by water (current or waves) or wind