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A true form fossil is a fossil of the whole/entire body of the organism, like an actual animal or animal part. For example, True form fossils are formed when the animals soft tissues or hard parts did not decay over the years.

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A coprolite is fossilized feces. For example, Coprolites are classified as trace fossils as opposed to body fossils, as they give evidence for the animal's behaviour (in this case, diet) rather than morphology.

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A fossil trackway is a type of trace fossil, a trackway made by an organism. For example,  many fossil trackways were made by dinosaurs, early tetrapods, and other quadrupeds and bipeds on land. Marine organisms also made many ancient trackways (such as the trails of trilobites and eurypterids like Hibbertopterus).

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Petrified wood is the name given to a special type of fossilized remains of terrestrial vegetation. For example, it is the result of a tree or tree-like plants having completely transitioned to stone by the process of permineralization.

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The creation of a cast or mold is a common form of indirect preservation. Most fossils do not contain actual body parts but are impressions, molds or casts of the original organism. For example, Essentially, a mold fossil forms when the organic matter of the organism decomposes and leaves a cavity, or mold.

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multi-volume Principles of Geology, which states that, with sedimentary rocks, if inclusions (or clasts) are found in a formation, then the inclusions must be older than the formation that contains them. For example,  in sedimentary rocks, it is common for gravel from an older formation to be ripped up and included in a newer layer.

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geology that states that the geologic feature which cutsanother is the younger of the two features. For example, It is a relative dating technique in geology.

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Principle of original lateral continuity

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Principle of original lateral continuity

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states that layers of sediment initially extend laterally in all directions. For example, they are laterally continuous, as a result, rocks that are otherwise similar, but are now separated by a valley or other erosional feature, can be assumed to be originally continuous.

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states that layers of sediment are originally deposited horizontally under the action of gravity. It is a relative dating technique.For example, the principle is important to the analysis of folded and tilted strata.

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the superposition principle, also known as superposition property, states that, for all linear systems, the net response caused by two or more stimuli is the sum of the responses that would have been caused by each stimulus individually. For example, his principle has many applications in physics and engineering because many physical systems can be modeled as linear systems.

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The fundamental principle or doctrine that geologic processes and natural laws now operating to modify the Earth's crust have acted in the same regular manner and with essentially the same intensity throughout geologic time. For example, phenomena and forces observable today; the classical concept that 'the present is the key to the past.