The three main types of rocks are igneous, sedimentary, and metamorphic, distinguished by their mode of formation:
- Igneous Rocks (related to option a): Formed from the cooling and solidification of molten rock material (magma below the surface or lava on the surface). Examples: Granite, Basalt.
- Sedimentary Rocks (related to option b): Formed from the accumulation, compaction, and cementation (lithification) of sediments (e.g., rock fragments, mineral grains, shells, organic remains). Examples: Sandstone, Shale, Limestone. The compression of organic remains (option d) can lead to specific types of sedimentary rocks like coal.
- Metamorphic Rocks (option c): Formed when pre-existing rocks (igneous, sedimentary, or even other metamorphic rocks) are changed (metamorphosed) by exposure to high temperatures, high pressures, chemically active fluids, or a combination of these, without melting completely. This alteration changes the rock's mineralogy, texture, and sometimes chemical composition. Examples: Marble (from limestone), Slate (from shale), Gneiss (from granite or other rocks).
Therefore, the distinguishing characteristic of metamorphic rocks is that they are formed from the alteration (metamorphism) of pre-existing rocks. Option (a) describes igneous rock formation. Option (b) describes sedimentary rock formation. Option (d) describes the formation of specific organic sedimentary rocks (like coal). \[ \boxed{\text{They are formed from the alteration of pre-existing rocks}} \]