mudflow |
undefined |
As a noun mudflow
is a type of landslide characterized by large flows of mud and water.
As an adjective undefined is
lacking a definition or value.
mudflow |
avalanche |
As nouns the difference between mudflow and avalanche
is that
mudflow is a type of landslide characterized by large flows of mud and water while
avalanche is a large mass or body of snow and ice sliding swiftly down a mountain side, or falling down a precipice.
As a verb avalanche is
to descend like an avalanche.
slump |
mudflow |
As nouns the difference between slump and mudflow
is that
slump is a heavy or helpless collapse; a slouching or drooping posture; a period of poor activity or performance, especially an extended period while
mudflow is a type of landslide characterized by large flows of mud and water.
As a verb slump
is to collapse heavily or helplessly.
mudflow |
creep |
As a noun mudflow
is a type of landslide characterized by large flows of mud and water.
As a proper noun creep is
(derogatory) the committee]] to re-elect the president, which raised money for [[w:richard nixon|richard nixon's campaign for 1972 reelection.
rockslide |
mudflow |
As nouns the difference between rockslide and mudflow
is that
rockslide is (geology) a type of landslide characterized by falling rocks while
mudflow is a type of landslide characterized by large flows of mud and water.
debris |
mudflow |
As nouns the difference between debris and mudflow
is that
debris is while
mudflow is a type of landslide characterized by large flows of mud and water.
mudflow |
midflow |
As nouns the difference between mudflow and midflow
is that
mudflow is a type of landslide characterized by large flows of mud and water while
midflow is a point in time during flow or fluency.
solifluction |
mudflow |
As nouns the difference between solifluction and mudflow
is that
solifluction is soil creep caused by waterlogged soil slowly moving downhill on top of an impermeable layer while
mudflow is a type of landslide characterized by large flows of mud and water.
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