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clasts Meaning in Bengali



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clasts's Usage Examples:

such as sand, silt, or clay, which fills the interstices between the clasts.


The clasts and matrix are typically cemented by calcium carbonate, iron oxide.


Clastic rocks are composed of fragments, or clasts, of pre-existing minerals and rock.


fractured or where it contains exposed bed planes, as this allows meltwater and clasts to penetrate more easily.


chert, with some sandstone, siltstone, and quartzite clasts also included.


Some of the chert clasts actually contained fossils.


Boulder-sized clasts are found in some sedimentary rocks, such as coarse conglomerate and boulder.


eroded through the action of glacial plucking and abrasion and the resulting clasts of various sizes will be incorporated to the glacier's bed.


At some places, clasts of various sizes are intermixed, with large amounts of sandy matrix; at others however, water-sorted clasts of similar size occur.


the finer-grained mass of material in which larger grains, crystals or clasts are embedded.


sedimentary rocks are composed of rock fragments (clasts) that have been cemented together.


The clasts are commonly individual grains of quartz, feldspar.


Less than ten percent of beach clasts have reflectance.


The meteoric iron occurs in clasts instead of a matrix.


Volcaniclastics are geologic materials composed of broken fragments (clasts) of volcanic rock.


Essentially, this law states that clasts in a rock are older than the rock itself.


recorded, consisting of limestone clasts mainly, but also with Millstone Grit, Pennant Sandstone, flint and chert clasts.


the products of phreatomagmatic eruptions contain juvenile (magmatic) clasts.


a primary depositional fabric consisting of a preferred orientation of clasts such that they overlap one another in a consistent fashion, rather like.


The clasts of Lombriz Formation are made.


pebbles or larger clasts in a matrix of sand, silt, or clay.


Metaconglomerate looks similar to conglomerate, although sometimes the clasts are deformed.


Hummocks may form as a result of clasts migrating to the surface through frost push and pull mechanisms.


As the clasts rise they push up on the ground.


from volcanic steam explosions and they are entirely made of accidental clasts.



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