Fold mountains taa la eebo yi guoluŋ a naŋ guoli a menne a saazuŋ a teŋɛ zuŋ. Yi a maalo saŋa a plate tectonics ane a internal architecture ko thrust belts da taa la teɛseɛbo, a yelnyɔgeraa ŋa da la da manne wuli a mountain belts kyɛ da ba la taa toma zaa.
Fold mountains maalo zie la thrust tectonics, teseŋ tectonic plates ayi naŋ tuori taa a convergent plate turibogi. A plates ane a continents vɛŋɛɛ ka a meele taa bee naŋ gaa subduction (naŋ e – naŋ zo do gaŋ a o tɔ zuŋ), a kubo naŋ meele taa naŋ guoli made taa teseŋ tablecloth naŋ daa gaa gaŋ aŋa table, gbɛɛ gyamaa a naŋ wuli ka mechanically weak layer teseŋ nyɛnnoo. Wagre naŋ a less dense continental crust "floats" a denser mantle rocks beneath, a tegroŋ naŋ na be a crustal material fere maalɛɛ tanlii, plateaus bee mountains naŋ taa la sentaaloŋ neŋ buoyancy feroo ka a lantaa maale mantle. Kyɛ ka a continental crust maŋ waa la vakpara a be a puli a mountains, teseŋ neŋ lower-lying ziiri. [1]Kubo naŋ baŋ guolee symmetrically bee asymmetrically. A upfolds la anticlines ane a downfolds la synclines. Gbɛɛ ggyamaa guoluu ane ŋmaroo kubo e la ka ba boɔlɔ ka nappes. A asymmetric guoluu a na baŋ wuli ka a recumbent ane overturned folds naŋ bebe la. A mountains maaloo maŋ baŋ waa la wogi yi o wogiruŋ naŋ seŋ ka a da e a yɛloŋ.[2]
A Jura mountains – A series of sub-parallel mountainous ridges naŋ taa maaloo yi folding neŋ a Triassic evaporite decollement yi thrust movements naŋ be a foreland a Alps
A 'Simply Folded Belt' naŋ be Zagros Mountains – A boma ko elongated anticlinal domes, gbɛɛ yaga a detachment folds neŋ underlying thrusts naŋ be a foreland a Zagros collisional belt, generally above a basal decollement naŋ maale evaporite neŋ a Neoproterozoic ko Early Cambrian Hormuz Formation
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