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.
A shoreline of submergence
The object farthest from the center in all three systems would likely be a distant galaxy due to the immense distances involved. Given the vast scale of the universe, galaxies are the most likely candidates for being farthest away from the centers of their respective systems.
The feature located nearest to a continent would likely be its coastline or shoreline.
The address of the Shoreline Library is: 345 Ne 175Th St, Shoreline, 98155 M
The address of the Shoreline Historical Museum is: Po Box 55594, Shoreline, WA 98155-0594
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 phone number of the Shoreline Library is: 206-362-7550.
The continental shelf begins at the shoreline.