Dit artikel is gesjreve (of begós) in 't Remunjs.
Laes hie wie v'r mit de versjillende saorte Limburgs ómgaon.
'nen Eilandjbaog is 'n rie aan gooddeils vólkanische eilenj, die gevörmp is gewaore dore wirking vanne plaattektoniek.
Eilandjbäög waere gevörmp op plaatse wo de ein oceanische plaat ónger de anger subduceertj. Baove de subductiezone zal 'n lang topografische depressie óntsjtaon, 'nen oceanischen traog. De subducerende kórs zal sjuuns de aerdmantjel in bewaege. Ómdet de subducerende kórs nag väöl zogeneumde vlöchtige besjtandjsdeiler (lichte sjtoffe wie water of gaas) bevat, zal deze gedeiltelik sjmulte. De sjmult kump ómhoog es vleujbaar magma, wodoor op de euverriejende plaat vólkanisme plaatsvindj. Hiedoor óntsjtaon 'n langgerèkde kitting van eilenj langs d'n oceanischen traog.
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