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.
hard
Conglomerate is a rock that has pieces of other rocks glued together to form one larger chunk. Therefore, they have a coarse-grained texture
Conglomerate rocks have a clastic sedimentary texture, meaning they are composed of rounded or angular rock fragments cemented together. These rock fragments can vary in size, creating a texture that resembles a cobblestone street.
the meta conglomerate is a metamorphic rock it's mineral composition is from quartz & it has a non- foliated texture, it's formed via temprature (the agent of metamorphism) & the type of metamorphism is said to be "thermal" & the pre-metamorphic rock is conglomerate.
Shale typically has a fine-grained texture, appearing smooth and often layered or fissile, allowing it to split easily into thin sheets. In contrast, conglomerate consists of larger, rounded clasts or pebbles embedded in a finer matrix, giving it a more coarse and variable texture. Sandstone, on the other hand, is composed primarily of sand-sized grains and has a more granular appearance, often with visible individual grains. Overall, shale is distinct due to its finer texture and layered structure compared to the coarser, more variable textures of conglomerate and sandstone.
There are two kinds od Conglomerate rocks, Paraconglomerates and Orthoconglomerates; Paraconglomerates are one of two varieties of conglomerate rock defined by texture consisting of a matrix supported rock that consists of at least 15% sand sized grains (<2 mm); the rest being larger grains of varying sizes. Orthoconglomerates are defined by texture. They are a grain supported rock that consists primarily of gravel sized grains (~256 mm) and less than 15% matrix grains (<2 mm, ie. Sand and finer particles).
Conglomerate is a type of sedimentary rock that forms from large sediments like rocks and pebbles. These sediments are cemented together by smaller particles like sand and mud to create a rock with a clastic texture. Conglomerate is often found in areas where there has been significant water movement, such as riverbeds and alluvial fans.
conglomerate is a sedimentary rock
A meta-conglomerate is a large corporation made up of multiple conglomerates and operating in diverse industries, while a conglomerate is a corporation that owns multiple smaller companies in different industries. Essentially, a meta-conglomerate is a conglomerate of conglomerates.
features of conglomerate
Conglomerate is a sedimentary rock.
A conglomerate is often referred to simply as a "conglomerate."