Once the sediments of the Carpathian geosyncline deposited - in the Superior Cretaceous - and the mountain peaks rising above the water, the erosion forces began their action, so that the orogenesis of the Carpathian must be understood as an alternation between folding, rising and erosion of the existent forms of relief.
(the sediments of the Carpathian geosyncline; deposited; ) (the mountain peaks; rising; L:above the water) (the erosion forces; began; their action; T:Once the sediments of the Carpathian geosyncline deposited; T:in the Superior Cretaceous - and the mountain peaks) (the orogenesis of the Carpathian; must be understood; as an alternation between folding) (an alternation between folding; rising; )
the sediments of the Carpathian geosyncline the mountain peaks the erosion forces the orogenesis of the Carpathian an alternation between folding
deposited rising began must be understood rising
L:above the water
their action T:Once the sediments of the Carpathian geosyncline deposited T:in the Superior Cretaceous - and the mountain peaks
as an alternation between folding