SEDIMENTNE KAMNINE / SEDIMENTARY ROCKS

Kremenov brečasti konglomerat je klastična sedimentna kamnina, v kateri so zrna kremena večja od 2 mm in so deloma zaobljena (značilna za konglomerate) in deloma še ostroroba (značilna za breče).

Quartz breccia conglomerate is a clastic sedimentary rock with quartz grains that are larger than 2 mm in size and are partly rounded (as in conglomerates) and partly sharp-edged (as in breccias).

Trbiška konglomeratna breča je klastična sedimentna kamnina iz geološke dobe spodnjega perma, ki jo sestavljajo zaobljena do ostroroba zrna apnencev in kremena z rdečkastim vezivom in je še posebno značilna za Karavanke. Na stiku med klasti je opazno delno raztapljanje karbonatnih fragmentov.

Tarvisio conglomerate breccia is a Lower Permian clastic sedimentary rock that consists of rounded to sharp-edged limestone and quartz grains with a reddish binder and is particularly characteristic of Karavanke. The contact between the clasts shows partial dissolution of carbonate fragments.

Apnenec s polami roženca je kemična sedimentna kamnina, ki jo pretežno sestavljajo drobna zrna kalcita, vmes pa so pole iz drobnozrnatega kremena roženca, ki je v kamnini zrasel na račun fosilnih kremeničnih mikroorganizmov.

Limestone with chert is a chemical sedimentary rock composed primarily of fine calcite grains interspersed with chert, which grew in the rock at the expense of fossil quartz microorganisms.

Dolomit je sedimentna kamnina, ki jo pretežno sestavlja mineral z enakim imenom dolomit in je lahko nastal kot kemična sedimentna kamnina ali pa je bil prvotni apnenec kasneje v fazi strjevanja nadomeščen z dolomitom.

Dolomite is a sedimentary rock composed primarily of the mineral of the same name, dolomite. It may have formed as a chemical sedimentary rock, or the original limestone was replaced by dolomite during the solidification phase.