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SENNI

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Beispiele für die Verwendung von SENNI in einem Satz

  • The upper slopes of the hill are composed of Devonian age sandstones assigned to the Senni Formation (formerly known as the "Senni Beds").
  • For example, Koyraboro Senni, spoken in Gao, is unintelligible to speakers of Zarma in Niger, according to Ethnologue.
  • The village is linked by minor roads with Heol Senni to the north and the A4059 north of Penderyn, and with Pontneddfechan, which lies in the community, at the head of the Vale of Neath to the south.
  • East of Timbuktu, Koyra Chiini gives way relatively abruptly to another Songhay language, Koyraboro Senni.
  • A year later, he again worked with Branch, alongside Lauri Honko and Senni Timonen, to produce a large work of poetry from across the Finno-Ugric peoples and languages: this comprised over 30 poets, 450 poems, and 13 languages, including Veps, Mordvin, Udmurt, and Livonian.
  • It is the sandstones and mudstones of the Lower Devonian Brownstones and Senni Formations, sometimes capped by the hard wearing sandstones of the Plateau Beds which form such striking peaks as Pen y Fan and Sugar Loaf and the dramatic scarps of the Black Mountains and Black Mountain.
  • Thin beds of calcrete, a thin limestone of terrestrial origin, occur on the hill; its very summit consists of sandstone from the Senni Formation (formerly referred to as the 'Senni Beds').
  • Craionog: Hanes plwyf Defynog : yn cynnwys y rhanbarthau cynlynol; Crai, Glyntawy, Senni, Glyntarell, a Maescar.
  • Cefn Cul is formed from sandstones and mudstones of the Senni Beds and Brownstones Formations of the Old Red Sandstone laid down during the Devonian period.
  • It continues northwestwards to near the junction of the minor road to Heol Senni with the A4067 before crossing the latter and curving westwards and northwards towards Crai.
  • Traditionally divided into three parts, the lowermost Red Marl Group, the middle Red Sandstone Group and uppermost Quartz Conglomerate Group, modern classification of the sequence recognises the St Maughans Formation (which directly overlies the Raglan Mudstone Formation), the Senni Formation and the Brownstones Formation (these three comprising the Lower Devonian) together with the Plateau Beds Formation and Quartz Conglomerate Group of the Upper Devonian.
  • The base and indeed greater part of the hill is formed from mudstones of the St Maughans Formation whilst the upper part is formed from the sandstones and mudstones of the Senni Formation (formerly known as the 'Senni Beds'), both of which are assigned to the Old Red Sandstone laid down during the Devonian period.
  • Its deposition continued in the early Devonian and is present as the St Maughans, Senni and Brownstones formations.



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