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There are lots of different ways in
which fossils may be formed. Here are 9 examples.
1. Permineralization
or Mineralization

(Fossil Sharks Teeth)
Permineralization occurs when the pores of the plant or animal remains
are impregnated by minerals. When this happens, the original shape
of the object is not changed.
2. Petrifaction

(Pertified Wood)
Petrifaction is a type of permineralization. It occurs when the
organic matter is completely replaced by minerals and the fossil
turns to stone. Petrified wood is a common example of this.
3. Molds

(Fossil Fern leaf)
Molds types of fossils where the physical characteristics of organisms
have been impressed onto rocks. The bodies decayed, leaving molds
of the organism.
4. Casting

(Fossil Sea shells)
Internal molds form from hollowed structures when the interior of
an organism is filled with inorganic material. When the shell deteriorates,
an impression of the interior is left.
5. Impressions
 
(Dinosaur tracks and a leaf imprint)
Impressions are imprints of an organism. Impressions may be of plants
or animals, or of tracks left by animals. Impressions are formed
when mud or sediment in which they were made hardens into stone.
6. Desiccation,
or Mummification.

(Insects trapped in amber)
Bones and tissues of organisms can be preserved, even keeping their
natural colors. Desiccation occurs in areas void of moisture, such
as insects trapped in tree sap which hardens to a stone called amber.
7. Dehydration

(Marsupial Lion from dry cave)
Also the desert or a dry cave can perserve an entire organism like
this lion fossil. Dehydration occurs and the entire skeleton or
organism is preserved.
8. Preservation

(Baby Mastodon)
The La Brea tar pits provide excellent examples of fossils which
are of the whole organism. Numerous examples of organisms have been
preserved there by asphalt, which preserves only the hard parts
of the organisms. Bones, complete skeletons, insects, leaves, and
flowers have been reclaimed from this site.
9. Freezing

(Frozen Mammoth and Tusks)
Freezing preserves a fossil of the highest quality.
It preserves the organism with little alteration to the chemical
composition. The temperature prevents little, if any, change to
the organism.
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