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  2. Cross-bedding - Wikipedia

    en.wikipedia.org/wiki/Cross-bedding

    Tabular cross-bedding, or planar bedding consists of cross-bedded units that are extensive horizontally relative to the set thickness and that have essentially planar bounding surfaces. [3] Trough cross-bedding, on the other hand, consists of cross-bedded units in which the bounding surfaces are curved, and hence limited in horizontal extent.

  3. Ripple marks - Wikipedia

    en.wikipedia.org/wiki/Ripple_marks

    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.

  4. Sedimentary structures - Wikipedia

    en.wikipedia.org/wiki/Sedimentary_structures

    These structures are within sedimentary bedding and can help with the interpretation of depositional environment and paleocurrent directions. They are formed when the sediment is deposited. Cross-bedding Cross-bedding is the layering of beds deposited by wind or water inclined at an angle as much as 35° from the horizontal. [1]

  5. Hummocky cross-stratification - Wikipedia

    en.wikipedia.org/wiki/Hummocky_cross-stratification

    Hummocky cross-stratification from the Book Cliffs, Utah. Hummocky cross-stratification from the Arisag Formation (Silurian), Nova Scotia. Hummocky cross-stratification is a type of sedimentary structure found in sandstones. It is a form of cross-bedding usually formed by the action of large storms, such as hurricanes. It takes the form of a ...

  6. Crossbedding - Wikipedia

    en.wikipedia.org/?title=Crossbedding&redirect=no

    Language links are at the top of the page across from the title.

  7. Category:Cross-bedding - Wikipedia

    en.wikipedia.org/wiki/Category:Cross-bedding

    A number of cross-bedding patterns are found in sediments, and reflect the currents that deposited them. Subcategories This category has only the following subcategory.

  8. Transfer portal creates bedlam & head coaches funding NIL ...

    www.aol.com/sports/transfer-portal-creates...

    On today's episode of The College Football Enquirer, Dan Wetzel, Ross Dellenger and SI's Pat Forde unpack the latest chaos created by the transfer portal. Specifically, they cover Penn State ...

  9. Esker - Wikipedia

    en.wikipedia.org/wiki/Esker

    Bedding may be irregular but is almost always present, and cross-bedding is common. [5] There are various cases where inland dunes have developed next to eskers after deglaciation. [7] These dunes are often found in the leeward side of eskers, if the esker is not oriented parallel to prevailing winds. [7]

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