Codru sörteszt, Iperium Strong

Fotbal Club Codru Lozova - Lozova-MDA

София Ротару - Кодры

Moldova is famous not only for delicious food and good winemaking but also for being a green land with amazing landscapes and peaceful nature. That is why, when visiting Moldova try to get lost in Codru forests also called Codrii, located on the central Moldavian hills and covering a huge part of them. Due to the deforestation for getting more vineyards, orchards and sunflower lands, Codrii is nowadays protected as a reserve, where people take care of its flora and fauna. Otherwise - the forests would just disappear.

KODI STATIONWed, September 8, 2021 9:50pmURL:Embed:

Kaufland deschide al cincilea magazin din Chișinău, în suburbia Codru, pe strada Haiducilor nr. 31.

Capriana is considered one of the most ancient monasteries in Moldova. Just try to imagine. It was settled up six centuries ago in 1429 in the heart of majestic Codru Wood. It should not surprise you, but nearly every citizen of Moldova knows this monastery as a religious place to visit when it comes to inward peace, freethinking and recuperation. It is surrounded by the most beautiful forest massifs, which makes the atmosphere around very special and peaceful. This monastery might be considered the most important one, as it was the residence of the metropolitan of Moldova for a long time. Capriana Monastery has an essential value for Moldavian history, which can also be proved by its image on the banknote of “One Lei”. The fact that the biggest monastic library was saved in Capriana Monastery makes this place really outstanding. It is very often said that here is the cradle of Moldavian culture, i.e. the language, architecture and music.

Abstract Permian felsic volcanic rocks were encountered in petroleum exploration boreholes in SE Hungary (eastern Pannonian Basin, Tisza Mega-unit, Békés–Codru Unit) during the second half of the 20th century. They were considered to be predominantly lavas (the so-called “Battonya quartz-porphyry”) and were genetically connected to the underlying “Battonya granite.” New petrographic observations, however, showed that the presumed lavas are crystal-poor (8–20 vol%) rhyolitic ignimbrites near Battonya and resedimented pyroclastic or volcanogenic sedimentary rocks in the Tótkomlós and the Biharugra areas, respectively. The studied ignimbrites are usually massive, matrix-supported, fiamme-bearing lapilli tuffs with eutaxitic texture as a result of welding processes. Some samples lack vitroclastic matrix and show low crystal breakage, but consist of oriented, devitrified fiammes as well. Textural features suggest that the latter are high-grade rheomorphic ignimbrites. Felsic volcanic rocks in SE Hungary belong to the Permian volcanic system of the Tisza Mega-unit; however, they show remarkable petrographic differences as compared to the other Permian felsic volcanic rocks of the mega-unit. In contrast to the crystal-poor rhyolitic ignimbrites of SE Hungary with rare biotite, the predominantly rhyodacitic–dacitic pyroclastic rocks of the Tisza Mega-unit are crystal-rich (40–45 vol%) and often contain biotite, pyroxene, and garnet. Additionally, some geochemical and geochronological differences between them were also observed by previous studies. Therefore, the Permian felsic volcanic rocks in SE Hungary might represent the most evolved, crystal-poor rhyolitic melt of a large-volume felsic (rhyodacitic–dacitic) volcanic system. The Permian volcanic rocks of the studied area do not show any evident correlations with either the Permian felsic ignimbrites in the Finiş Nappe (Apuseni Mts, Romania), as was supposed so far, or the similar rocks in any nappe of the Codru Nappe System. Moreover, no relevant plutonic–volcanic connection was found between the studied samples and the underlying “Battonya granite.”