(a) Outline the characteristics of sedimentary rocks.
(b) Describe two ways in which sedimentary rocks can be formed
(a) Characteristics of sedimentary rocks:
They are formed in layers (strata/beds) which are usually visible as bedding planes.
They are non-crystalline and generally softer than igneous rocks.
They frequently contain fossils of plants and animals buried during their formation.
They are made of compacted and cemented sediments (particles of pre-existing rocks or organic matter), and are often porous and permeable.
They are stratified and can be split along the layers.
(b) Two ways sedimentary rocks can be formed:
Mechanically (clastic/detrital formation): rocks are weathered and eroded into fragments; these sediments are transported by water, wind or ice, deposited in layers, then compacted and cemented over time into rock such as sandstone and shale.
Organically (biological formation): the remains of living things accumulate and are compacted, e.g. the shells and skeletons of sea organisms forming limestone/chalk, or plant remains forming coal. (Chemically formed sedimentary rocks, e.g. rock salt from evaporation, are also acceptable.)
They are formed in layers (strata/beds) which are usually visible as bedding planes.
They are non-crystalline and generally softer than igneous rocks.
They frequently contain fossils of plants and animals buried during their formation.
They are made of compacted and cemented sediments (particles of pre-existing rocks or organic matter), and are often porous and permeable.
They are stratified and can be split along the layers.
(b) Two ways sedimentary rocks can be formed:
Mechanically (clastic/detrital formation): rocks are weathered and eroded into fragments; these sediments are transported by water, wind or ice, deposited in layers, then compacted and cemented over time into rock such as sandstone and shale.
Organically (biological formation): the remains of living things accumulate and are compacted, e.g. the shells and skeletons of sea organisms forming limestone/chalk, or plant remains forming coal. (Chemically formed sedimentary rocks, e.g. rock salt from evaporation, are also acceptable.)