Conglomerate is the name of one type of rock, which is formed from a mixed source. The source rocks are commonly rounded pebbles. Often quite beautiful. And of course, the type of source rocks may be easily determined. Such a rock obviously originates from re-worked young gravels, - probably fresh water.
There is another common type of sedimentary rock, formed in marine shelf areas. Upon the shelf edge collapsing, some of the recent clays and silts will tear loose some of the more indurated older formation. The older rock is usually quite angular and is well cemented in the younger material. [Sorry - I forget the name!]
Quite differently, will be intrusive sills and dikeswhich will usually be either volcanic or granitic. You'll be able to spot the chilled margins of the intrusive - and the slightly re-heated margin in the host rock.
xenolith
It is a xenolith.
An example of a fragment of one kind of rock found within another kind of rock is xenoliths, which are pieces of pre-existing rock engulfed by magma and then incorporated into igneous rocks as they form. These fragments provide insights into the composition and history of the lithosphere.
another name for moon soil. breccia. a kind of rock found on the moon that is made up of older rocks stuck together.
No every rock is able to change into anther
No.
a rockasouraus
For a variety of reasons, most fossils are found in sedimentary rock.
The idea that pieces of rock found in another rock are older than the rock they are found in is stated in the law of superposition. This principle helps geologists determine the relative ages of different rock layers.
A metamorphic rock used to be a different rock type, typically sedimentary.
You would say the rock has been metamorphized.
Neodymium is not a rock but a metallic element which is found in some rocks.