SILTY SHALE
SILTY SHALE
No, pebble conglomerate is more likely to form closer to the shoreline where high-energy water can transport and deposit large pebbles. Farther from the shoreline, sediments are usually finer-grained and form different types of rocks like shale or sandstone.
To determine which geological feature formed farthest from the shoreline, one would typically look for evidence of sediment deposition or volcanic activity that occurred in deeper water or offshore environments. Features such as deep-sea trenches, abyssal plains, or seamounts are likely candidates, as they are formed in oceanic regions far from land. Conversely, coastal features like beaches, estuaries, and deltas are formed much closer to the shoreline. Therefore, geological formations associated with oceanic processes are more likely to be found farther from the shore.
Because sandstone, silty shale, and shell limestone usually have origins of formation on or near shore, the pebble conglomerate is left. Pebble conglomerates are formed from deposition of water transported rocks of larger size than the smaller rock particles which compose sandstone and shale. The larger size indicates they were transported and deposited further from the shoreline.
Conglomerate rock is most likely formed from pebble-sized sediment deposited in shallow water at an ocean shoreline. As the pebbles accumulate, they cement together to form the rock.
Conglomerate rock is most likely formed from pebble-sized sediment deposited in shallow water at an ocean shoreline. The pebbles are typically rounded due to erosion in water, and they can become cemented together to form the conglomerate rock.
A bight is a wide bay formed by a bend or curve in a shoreline.
A shoreline of submergence
The Gulf of Mexico.
Rocky shorelines have rocks and cliffs, so when the waves crash against the rock fragments and sediments are formed along the shoreline.
Ripple marks likely indicate that a rock formed in a sedimentary environment, such as near a shoreline or in a river bed, where the movement of water created the distinct ripple pattern in the sediment before it hardened into rock. These marks provide information about the ancient depositional environment and the direction of water flow at the time of formation.
Rocky shorelines have rocks and cliffs, so when the waves crash against the rock fragments and sediments are formed along the shoreline.