(b) Four differences between sedimentary and metamorphic rocks
Sedimentary rocks
Metamorphic rocks
Formed by the deposition and compaction/cementation of sediments.
Formed by the alteration of existing rocks by heat and pressure.
Usually arranged in layers (strata / bedding planes).
Often show foliation (banding) or are recrystallised, without simple bedding.
Generally soft and less compact, and may be porous.
Generally hard, compact and dense.
Often contain fossils of plants and animals.
Fossils are usually destroyed by the heat and pressure.
Additional difference: sedimentary rocks form at or near the surface at low temperature, while metamorphic rocks form deep within the crust under intense heat and pressure.
(b) Four differences between sedimentary and metamorphic rocks
Sedimentary rocks
Metamorphic rocks
Formed by the deposition and compaction/cementation of sediments.
Formed by the alteration of existing rocks by heat and pressure.
Usually arranged in layers (strata / bedding planes).
Often show foliation (banding) or are recrystallised, without simple bedding.
Generally soft and less compact, and may be porous.
Generally hard, compact and dense.
Often contain fossils of plants and animals.
Fossils are usually destroyed by the heat and pressure.
Additional difference: sedimentary rocks form at or near the surface at low temperature, while metamorphic rocks form deep within the crust under intense heat and pressure.