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Polymorphous :: Polymorphous (a.) Having, or occurring in, several distinct forms; -- opposed to monomorphic..

Isotrimorphous :: Isotrimorphous (a.) Having the quality of isotrimorphism; isotrimorphic.

Hemimorphic :: Hemimorphic (a.) Having the two ends modified with unlike planes; -- said of a crystal.

Pantamorphic :: Pantamorphic (a.) Taking all forms.

Heteronereis :: Heteronereis (n.) A free-swimming, dimorphic, sexual form of certain species of Nereis..

Allomorphic :: Allomorphic (a.) Of or pertaining to allomorphism.

Trimorphous :: Trimorphous (a.) Of, pertaining to, or characterized by, trimorphism; -- contrasted with monomorphic, dimorphic, and polymorphic..

Pleomorphic :: Pleomorphic (a.) Pertaining to pleomorphism; as, the pleomorphic character of bacteria..

Ichthyomorphic :: Ichthyomorphic (a.) Alt. of Ichthyomorphou.

Metamorphic :: Metamorphic (a.) Causing a change of structure.

Metamorphic :: Metamorphic (a.) Pertaining to, produced by, or exhibiting, certain changes which minerals or rocks may have undergone since their original deposition; -- especially applied to the recrystallization which sedimentary rocks have undergone through the influence of heat and pressure, after which they are called metamorphic rocks..

Ichthyomorphous :: Ichthyomorphous (a.) Fish-shaped; as, the ichthyomorphic idols of ancient Assyria..

Dimorphic :: Dimorphic (a.) Having the property of dimorphism; dimorphous.

Orphic :: Orphic (a.) Pertaining to Orpheus; Orphean; as, Orphic hymns..

Dimorphous :: Dimorphous (a.) Characterized by dimorphism; occurring under two distinct forms, not dependent on sex; dimorphic..

Nematogene :: Nematogene (n.) One of the dimorphic forms of the species of Dicyemata, which produced vermiform embryos; -- opposed to rhombogene..

Homomorphic :: Homomorphic (a.) Alt. of Homomorphou.

Isotrimorphic :: Isotrimorphic (a.) Isotrimorphous.

Boustorphic :: Boustorphic (a.) Boustrophedonic.

Metamorphism :: Metamorphism (n.) The state or quality of being metamorphic; the process by which the material of rock masses has been more or less recrystallized by heat, pressure, etc., as in the change of sedimentary limestone to marble..

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