They had various origins
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.
Pebbles do not naturally glow in the dark. However, some pebbles are coated with a phosphorescent material that absorbs light and glows in the dark after being exposed to light.
Most pebbles will sink in water because they are denser than water. Some types of pebbles may have air pockets that allow them to float briefly before sinking.
Most pebbles are not magnetic because they are typically composed of minerals like quartz, feldspar, and mica which are not magnetic. However, some pebbles may have traces of magnetic minerals like magnetite or hematite which can make them slightly magnetic.
In that scenario, you would most likely find the three basic types of clastic sedimentary rocks (conglomerate, sandstone, and shale) in the following order: conglomerate near the creek where larger sediment particles accumulate, sandstone in the transition zone between the creek and lake where medium-sized particles settle, and shale in the deeper parts of the lake where fine sediment particles settle.
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.
Conglomerate is made up of rounded pebbles cemented together. The pebbles have been rounded by the action of moving water. This could be from a river or stream or from waves on a long ago beach.Because they have been transported by water the pebbles may be from a wide variety of rock types. The size of these rock fragments is over 2 mm in diameter.After the pebbles have been deposited they are compacted by the sediments that pile up on top of them. Over very long periods of time the pebbles become cemented together by minerals. Silica, calcite, and iron oxides are the most common cementing minerals.The rounded rock particles in the conglomerate are easily visible to the naked eye.Conglomerate is often much harder and resistant than the sandstones and shales that surround it. Conglomerate is scientifically valuable because the individual stones are samples of the older rocks that were exposed as it was forming---important clues about the ancient environment.
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.
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Pebbles do not naturally glow in the dark. However, some pebbles are coated with a phosphorescent material that absorbs light and glows in the dark after being exposed to light.
sand
pebbles,
The three most common clastic sedimentary rocks are sandstone, shale, and conglomerate. Sandstone is composed of grains of sand cemented together. Shale is made of very fine particles like clay and mud. Conglomerate is a mix of larger rock fragments that are cemented together.
To provide assistance with this question, please provide the information from the table in question so I can help you identify the most clearly supported inference.
conglomerate
conglomerate
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