mudcrack

navigate by keyword : base becomes below channel contracts cracks developed driedup enough filled form formcastsover forming individual interconnected join large later layer material may mudcrack mudcracks muddy naturally network polygonal relieve same sediment sedimentdries shrinks size spread start stays strain surface top upand wet

Mudcrack texture top view Royalty Free Stock Photo
Shoeprint or foot print on mudcrack surface Royalty Free Stock Photo
Shoeprint or foot print on mudcrack surface Royalty Free Stock Photo
mudcrack a pattern of cracks that form in dried mud as it shrin Royalty Free Stock Photo
mudcrack a pattern of cracks that form in dried mud or clay k h Royalty Free Stock Photo
Texture background / ground and flooring Royalty Free Stock Photo
Texture background / ground and flooring Royalty Free Stock Photo
Mudcrack
Dry mudcrack pond Royalty Free Stock Photo
Mud crack Royalty Free Stock Photo
Texture background / ground and flooring Royalty Free Stock Photo
Nature Canvas - The Artistry of Grietas Mudcrack Royalty Free Stock Photo
From Where I Stand Royalty Free Stock Photo
Mudcrack Royalty Free Stock Photo
Mudcrack Texture Royalty Free Stock Photo
Naturally forming mudcracks start as wet, muddy sediment dries up and contracts. A strain is developed because the top layer shrinks while the material below stays the same size. When this strain becomes large enough, channel cracks form in the dried-up surface to relieve the strain. Individual cracks spread and join up, forming a polygonal, interconnected network. These cracks may later be filled with sediment and form castsover the base.


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