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There are five classes of amber, defined on the basis of their chemical constituents. Because it originates as a soft, sticky tree resin, amber sometimes contains animal and plant material as inclusions.

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It is generally understood to be the same as Abalus. Based on the amber, the island could have been Heligoland, Zealand, the shores of Bay of Gdansk, the Sambia Peninsula or the Curonian Lagoon, which were historically the richest sources of amber in northern Europe.

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It is assumed that there were well-established trade routes for amber connecting the Baltic with the Mediterranean known as the "Amber Road". Pliny states explicitly that the Germans export amber to Pannonia, from where it was traded further abroad by the Veneti.

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The ancient Italic peoples of southern Italy were working amber, the most important examples are on display at the National Archaeological Museum of Siritide to Matera. Amber used in antiquity as at Mycenae and in the prehistory of the Mediterranean comes from deposits of Sicily.

He also states that amber is also found in Egypt and in India, and he even refers to the electrostatic properties of amber, by saying that "in Syria the women make the whorls of their spindles of this substance, and give it the name of harpax [from?????? In Middle Low German, amber was known as berne- barn- b? It has a Mohs hardness of 5.

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Ilvaite is structurally related to lawsonite. It occurs in contact metamorphic rocks and skarn ore deposits. It also occurs less commonly in syenites. Ilvaite was first described in on the island of Elba and the name ilvaite from the Latin name ilva of the island. Sometimes referred to as yenite. Commonly encountered species and varieties: Brownish black to black—schorl Dravite species: The magnesium rich members of the solid solution series are common rock-forming minerals found in igneous and metamorphic rocks.

The intermediate composition, Mg,Fe SiO3, has historically been known as hypersthene, although this name has been formally abandoned and replaced by orthopyroxene. When determined petrographically or chemically the composition is given as relative proportions of enstatite En and ferrosilite Monoclinic cummingtonite is compositionally similar and polymorphic with orthorhombic anthophyllite, which is a much more common form of magnesium-rich amphibole, the latter being metastable.

Cummingtonite shares few compositional similarities with alkali amphiboles such as arfvedsonite, glaucophane-riebeckite. There is little solubility between these minerals due to different crystal habit and inability of substitution between alkali elements and ferro-magnesian elements within the amphibole structure.

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