Saxum conglomeratum

Saxum conglomeratum^[1] est saxum sedimentarium, tribus componentibus constans, quorum prima est glarea, secunda harena vel aleurites inter glareas cavitates explens, tertium ferrumen aliquod minerale, primam secundamque concrescens. Ferrumina saxorum conglomeratorum sunt carbonata vel marga vel ferri oxida. Saxum vulgo breccia dictum a conglomerato distinguendum est; pro glareis rotundiformibus multa fragmenta angulata et acria includit. Saxa conglomerata secundum compositionem dividuntur in multimixta, quorum composita varia sunt, et unimixta, eisdem elementis composita.

↑ Pauli Kitaibel^(hu) Hydrographica Hungariae, pars II, Pestini 1829, p. 223; Adolfi Overweg^(de) De compositione et origine trium collium..., Bonnae 1847, pp. 17, 21, 2, 26, 31; Nova acta Regiae Societatis Scientiarum Upsaliensis, ser. III, vol. I, Upsaliae 1855, pp. 294, 307, etc.

[1] Pauli Kitaibel^(hu) Hydrographica Hungariae, pars II, Pestini 1829, p. 223; Adolfi Overweg^(de) De compositione et origine trium collium..., Bonnae 1847, pp. 17, 21, 2, 26, 31; Nova acta Regiae Societatis Scientiarum Upsaliensis, ser. III, vol. I, Upsaliae 1855, pp. 294, 307, etc.

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Saxum conglomeratum

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