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  2. Mudrock - Wikipedia

    en.wikipedia.org/wiki/Mudrock

    Fine sediment is the most abundant product of erosion, and these sediments contribute to the overall omnipresence of mudrocks. [1] With increased pressure over time, the platey clay minerals may become aligned, with the appearance of parallel layering ( fissility ).

  3. Crossword

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  4. Off the Grid: Sally breaks down USA TODAY's daily crossword ...

    www.aol.com/off-grid-sally-breaks-down-060016881...

    USA TODAY’s Daily Crossword Puzzles Sudoku & Crossword Puzzle Answers This article originally appeared on USA TODAY: Crossword Blog & Answers for December 2, 2024 by Sally Hoelscher

  5. Pelite - Wikipedia

    en.wikipedia.org/wiki/Pelite

    A pelite (from Ancient Greek πηλός (pēlós) 'clay, earth') [3] or metapelite is a metamorphosed fine-grained sedimentary rock, i.e. mudstone or siltstone. The term was earlier used by geologists to describe a clay-rich, fine-grained clastic sediment or sedimentary rock, i.e. mud or a mudstone, the metamorphosed version of which would ...

  6. Boulder clay - Wikipedia

    en.wikipedia.org/wiki/Boulder_clay

    World War II pillbox on eroding boulder clay, Filey Bay, England Boulder clay cliffs in Gwynedd with Dinas Dinlle in the background. Boulder clay is an unsorted agglomeration of clastic sediment that is unstratified and structureless and contains gravel of various sizes, shapes, and compositions distributed at random in a fine-grained matrix.

  7. Play Daily Crossword Online for Free - AOL.com

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    Challenge your crossword skills everyday with a huge variety of puzzles waiting for you to solve. Play Daily Crossword Online for Free - AOL.com Skip to main content

  8. Bay of Fundy - Wikipedia

    en.wikipedia.org/wiki/Bay_of_Fundy

    The Bay of Fundy (French: Baie de Fundy) is a bay between the Canadian provinces of New Brunswick and Nova Scotia, with a small portion touching the U.S. state of Maine.It is an arm of the Gulf of Maine.

  9. Geology of Finland - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Finland

    Ice retreat was accompanied by the formation of eskers and the dispersal of fine-grained sediment deposited as varves. [2] As the ice sheet became thinner and retreated, the land began to rise due to post-glacial rebound. Much of Finland was under water when the ice retreated and was gradually uplifted in a process that continues today. [44]