Tool Marks Geology. Web a tool mark is a mark produced by the impact against a muddy bottom of a solid object driven by a current moving over the. Tool marks form when hard objects such as cobbles, bones, wood, or shells get bounced along the bottom of a body of. Objects drug by a moving current can make a variety of indentations into cohesive substrate. Web tool marks come from objects like sticks carried in the fluid downstream or embossed into the sediment layer, leaving a depression. They include long groove casts, where. Web tool marks are produced when larger particles in the current scoured out the underlying mud. Web groove casts and tool marks. Web tool marks are single grooves made in a stationary bed by an object impelled by a transporting agent. Web tool marks are made when an object, such as a stick, is dragged across sediment by a current and leaves behind what looks like scratches in the soft sediment (figure 4.14).
from serc.carleton.edu
Web tool marks come from objects like sticks carried in the fluid downstream or embossed into the sediment layer, leaving a depression. Web a tool mark is a mark produced by the impact against a muddy bottom of a solid object driven by a current moving over the. They include long groove casts, where. Web groove casts and tool marks. Web tool marks are single grooves made in a stationary bed by an object impelled by a transporting agent. Web tool marks are produced when larger particles in the current scoured out the underlying mud. Objects drug by a moving current can make a variety of indentations into cohesive substrate. Web tool marks are made when an object, such as a stick, is dragged across sediment by a current and leaves behind what looks like scratches in the soft sediment (figure 4.14). Tool marks form when hard objects such as cobbles, bones, wood, or shells get bounced along the bottom of a body of.
Sole Marks
Tool Marks Geology Web tool marks are produced when larger particles in the current scoured out the underlying mud. Web tool marks are produced when larger particles in the current scoured out the underlying mud. Objects drug by a moving current can make a variety of indentations into cohesive substrate. Web tool marks come from objects like sticks carried in the fluid downstream or embossed into the sediment layer, leaving a depression. Web tool marks are single grooves made in a stationary bed by an object impelled by a transporting agent. Tool marks form when hard objects such as cobbles, bones, wood, or shells get bounced along the bottom of a body of. Web tool marks are made when an object, such as a stick, is dragged across sediment by a current and leaves behind what looks like scratches in the soft sediment (figure 4.14). They include long groove casts, where. Web a tool mark is a mark produced by the impact against a muddy bottom of a solid object driven by a current moving over the. Web groove casts and tool marks.
