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Hornfels is not a rock that is "deposited". Instead it is a rock type that forms when an existing rock is metamorphosed. The original rock that was metamorphosed is usually referred to as the "parent rock" or "protolith". Answer to Match the name of the metamorphic rock with its parent rock.

Metaconglomerate parent rock

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The same types of clasts found in the rock or parent material, it is monomictic conglomerates. Here, Mono means single and same.

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It consists of colorful flint pebbles in a white to brown silicate matrix. This type of rock is found at many locations in Hertfordshire County, England. Image by John Cancalosi / Alamy Stock Photo.

Metaconglomerate parent rock

metacon Teknologi som omvandlar biogas till vätgas, el och värme

Metaconglomerate parent rock

Volatiles are those chemical substances, including water and carbon dioxide, that easily turn into gas or fluid and are mobile enough to move in and out of solid rock inside the earth. Start studying Metamorphic rocks parent rocks.

Conglomerates form by the … Parent Rocks and Protoliths. Hornfels is not a rock that is "deposited". Instead it is a rock type that forms when an existing rock is metamorphosed. The original rock that was metamorphosed is usually referred to as the "parent rock" or "protolith". Metaconglomerate rock (commercially known as marinace; if anyone knows why, please comment below). Mr. Phelps writes: I originally became interested in this rock after reading this blog post.
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Metaconglomerate parent rock

Mini Me Geology has a great selection of metamorphic rock samples which show the change from one rock type (the parent rock) to another. Metamorphic rock is classified by texture and composition. The texture can be foliated or nonfoliated.

Such conditions  Every metamorphic rock has a parent rock from which it was formed. Examples - metaconglomerate: Once spherical pebbles heated and flattened into  Probably origin is german word Gneis that mean “spark” (rock glitters).
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Foliated metamorphic rocks appeared banded or layered. Foliated rocks can be ordered in terms of increasing metamorphism. In the chart below notice how each of the first three rocks become the parent rock for the next. Metamorphic rocks are complex because they have been derived from either pre existing igneous, sedimentary or metamorphic rocks.


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Foliated metaconglomerate is created under the same metamorphic conditions that produce slate or phyllite, but with the parent rock being conglomerate, rather than clay. [2] The metaconglomerates of the Jack Hills of Western Australia are the source rocks for much of the detrital zircons that have been dated to be as old as 4.4 billion years. Foliated metaconglomerate is created under the same metamorphic conditions that produce slate or phyllite, but with the parent rock (protolith) being conglomerate, rather than clay.