no it is able to be found way under water
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.
The rock is likely a conglomerate, which is a type of sedimentary rock composed of rounded pebbles or larger grains cemented together by smaller particles. Conglomerates are formed through the process of sedimentary deposition and lithification. These rocks are often found in environments with high-energy river or coastal settings.
Sedimentary rocks, such as sandstone, shale, or conglomerate, are likely to be found in an ancient riverbed on the Earth's surface. These rocks are formed from the accumulation and compaction of sediments carried by rivers over time.
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.
SILTY SHALE
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.
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.
SILTY SHALE
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.
sand
A shoreline of submergence
The conglomerate rock you're describing likely formed from the deposition of large, angular fragments that were transported by water or ice and then fused together during the lithification process. The angular nature of the fragments suggests that they were not significantly transported from their source, indicating a nearby origin for the rock.
Shale and sandstone are fine-grained sedimentary rocks that compact well to preserve fossils due to their low porosity and permeability. Conglomerate, being a coarse-grained rock with larger particles and higher porosity, tends to have more spaces for organic material to decompose or be destroyed before preservation can occur.
The rock is likely a conglomerate, which is a type of sedimentary rock composed of rounded pebbles or larger grains cemented together by smaller particles. Conglomerates are formed through the process of sedimentary deposition and lithification. These rocks are often found in environments with high-energy river or coastal settings.
Sedimentary rocks, such as sandstone, shale, or conglomerate, are likely to be found in an ancient riverbed on the Earth's surface. These rocks are formed from the accumulation and compaction of sediments carried by rivers over time.