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The oldest continental crustal rocks on Earth have ages in the range from about 3.

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Some zircon with age as great as 4. A theoretical protoplanet named "Theia" is thought to have collided with the forming Earth, and part of the material ejected into space by the collision accreted to form the Moon.

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The cumulate rocks form much of the crust. The thickness of the crust ranges between about 20 and km. Crust on the far side of the Moon averages about 12 km thicker than that on the near side. Estimates of average thickness fall in the range from about 50 to 60 km. Most of this plagioclase-rich crust formed shortly after formation of the moon, between about 4.

The best-characterized and most voluminous of these later additions are the mare basalts formed between about 3.

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Pearl, considered by some[who? 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.

Minor volcanism continued after 3. There is no evidence of plate tectonics. 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. 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? Molecular polymerization, resulting from high pressures and temperatures produced by overlying sediment, transforms the resin first into copal.

Sustained heat and pressure drives off terpenes and results in the formation of amber.

Many trees produce resin, but in the majority of cases this deposit is broken down by physical and biological processes. Exposure to sunlight, rain, microorganisms such as bacteria and fungiand extreme temperatures tends to disintegrate resin.

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