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Sedimentary rocks record;

1. Time (Age) of formation.

2. Environment of formation.

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12y ago

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What are sedimentary rocks shaped like?

No two sedimentary rocks are shaped the same, there are many different shapes


What are two types of organic rocks?

sedimentary and metamorphic rocks


What are two examples of sedimentary rocks?

Limestone or Sandstone are two examples of sedimentary rocks. Two examples of sedimentary rocks are slate (fine silt) and chalk (shell remains of sea creatures).


What are two things that sediments may change to?

Sediments can change into sedimentary rocks through processes like compaction and cementation. They can also be eroded and transported to new locations by forces like wind and water.


What are the two main types of sedimentary rocks?

The two main types of sedimentary rocks are clastic (detrital) rocks, which are made of pre-existing rock fragments cemented together, and chemical rocks, which form from minerals that precipitate out of solution.


What are different types of sedimentary rock?

Coal and Sandstone are two types of sedimentary rocks.


What two kinds of rocks are formed from all thre kind of rocks?

Sedimentary and metamorphic rocks.


What are sedimentary rocks form from dissolved minerals called?

They are called chemical sedimentary rocks. Rock salt and rock gypsum are two examples.


What two things make possible sedimentary and metamorphic rocks to form deep underground?

High pressure and high temperature deep underground make it possible for sedimentary rocks to undergo metamorphism, which leads to the formation of metamorphic rocks. These conditions cause the existing minerals in sedimentary rocks to recrystallize and form new minerals, changing the rock's texture and composition.


What are two examples of rocks?

sedimentary rock and igenous rock.


What are two major divisions of sedimentary rocks?

mechabic and organic


What two things can change sedimentary rocks and igneous rocks into metamorphic rocks?

Sedimentary and igneous rocks can be transformed into metamorphic rocks through two primary processes: heat and pressure. Elevated temperatures, often due to tectonic activity or proximity to magma, can alter the mineral composition and structure of the rocks. Additionally, intense pressure, typically from overlying rock layers or tectonic forces, can cause physical and chemical changes, resulting in metamorphism. Together, these processes create new mineral assemblages and textures characteristic of metamorphic rocks.