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You think probable to a shale.
Shale
Hydrocarbons containing chlorine atoms are called chlorinated hydrocarbons. Hydrocarbons containing fluorine atoms are called fluorinated hydrocarbons. eg> CHCl3, CHF3 etc
Detrital sedimentary rock Chemical sedimentary rock Biological sedimentary rock
It began as an aggregat of unconsolidated sediment containing pebbles of various rock types. Upon lithification, it became the sedimentary rock called conglomerate.
You think probable to a shale.
Shale
Coal is a combustible sedimentary rock, composed mostly of carbon and hydrocarbons.
It consists of combustible black sedimentary rock composed of carbon and hydrocarbons.
Hydrocarbons containing chlorine atoms are called chlorinated hydrocarbons. Hydrocarbons containing fluorine atoms are called fluorinated hydrocarbons. eg> CHCl3, CHF3 etc
ORGANIC SEDIMENTARY ROCK`s : Is a type of sedimentary rock because sedimentary rock has three types of sedimentary rock called clastic , chemical , and organic sedimentary rock so yes ORGANIC SEDIMENTARY ROCK is a type of sedimentary rock..........................................
Clastic sedimentary rock.
Detrital sedimentary rock Chemical sedimentary rock Biological sedimentary rock
It began as an aggregat of unconsolidated sediment containing pebbles of various rock types. Upon lithification, it became the sedimentary rock called conglomerate.
== == The "coarseness" of a sedimentary rock refers to the rock's textural character, and more particularly, the size of grains contained within it. Thus, a conglomerate containing pebble or cobble clasts is coarser than a sandstone containing sand grains. In the same way, a conglomerate containing boulders is coarser than a conglomerate containing pebbles. Clastic sedimentary rocks are classified using the Wentworth Scale. The coarsest elements of this scale are the Rudites. Boulder rudites are conglomeratic rocks with grains of diameter greater than 256mm. They are the coarsest element described on the Wentworth Scale. There is no upper limit to the scale of sedimentary coarseness, since the size of clast which can be preserved in a sedimentary rocks is potentially very large. 'Olistolith' is a term which describes very large clasts often derived from the sub-sea collapse of oversteepened slopes such as are found at continental margins. Sediments containing olistoliths may reasonably be described as the coarsest sedimentary rocks.
Yes it is possible for a sedimentary rock to be changed into a different sedimentary rock.
When cemented together, clastic sedimentary rock.