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unfossiliferous

unfossiliferous Sentence Examples

  • They consist of a series of unfossiliferous crystalline slates.

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  • In the north the plateau is overlain by red and purple unfossiliferous sandstones, capped near its edge by a cherty limestone also unfossiliferous but possibly of Lower Cretaceous age.

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  • Greenland, but as they are unfossiliferous sandstone, rapidly disintegrating, this cannot be known.

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  • The former appears to be almost unfossiliferous, the latter has yielded a rich marine fauna, which belongs to the top of the Carboniferous or to the Permo-carboniferous.

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  • So far it has proved to be unfossiliferous.

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  • Primary deposits are doubtfully represented by the detached fragments of unfossiliferous strata of Traras, Blida and east of Orleansville.

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  • 1767) in Germany, who distinguished between the primary, or unfossiliferous, and secondary or fossiliferous, formations.

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  • From the edge of the coast belt to near the confluence of the Benue and Niger they are overlain by unfossiliferous sandstones, lying undisturbed and possibly of the age of the sandstones of the Congo basin.

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  • In the Kharga Oasis the upper portion consists of variously colored unfossiliferous clays with intercalated bands of sandstone containing fossil silicified woods (Nicolia Aegyptiaca and A raucarioxylon Aegypticum).

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  • There occur also below the Lias on some parts of the west coast unfossiliferous red sandstones, conglomerates and breccias, presenting lithological resemblance to the Rhaetic group of England.

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  • These ancient rocks, which form the foundation of the country, are overlaid unconformably by a series of conglomerates and sandstones, generally unfossiliferous and often red or purple in colour, very similar in character to the Nubian sandstone of Upper Egypt.

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  • Upon them rest the unfossiliferous strata known to Indian geologists as the Transition and Vindhyan series.

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  • The central plateau consists of ancient crystalline rocks with granites overlain by unfossiliferous sandstones and conglomerates considered to be of Palaeozoic age.

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  • The median zone is composed largely of crystalline rocks with granites and some Palaeozoic unfossiliferous rocks.

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  • The second is the zone of the snowy peaks and of the lower Himalaya, and is composed chiefly of crystalline and metamorphic rocks together with unfossiliferous sedimentary beds supposed to be of Palaeozoic age.

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  • In the region of Adigrat the metamorphic rocks are invariably overlain by white and brown sandstones, unfossiliferous, and attaining a maximum thickness of moo feet.

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  • They are interbedded with unfossiliferous sandstones and shales.

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  • It is unfossiliferous except for a few obscure sheils obtained near the base.

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  • Pondoland Cretaceous Series Uitenhage Series Stormberg Series Beaufort Series Ecca Series Dwyka Series Witteberg Series Bokkeveld Series Table Mountain Sandstone Series Includes several independent unfossiliferous formations of pre-Devonian age Cretaceous Carboniferous to Jurassic Devonian Archaean to Silurian(?) { Karroo System Cape System Pre-Cape Rocks Cretaceous System imperfect remains of plants (Spirophyton) are the only fossils, and these are not sufficient to determine if the beds belong to the Devonian or Carboniferous System.

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  • The formations older than the mesozoic are remarkably unfossiliferous, so that the determination of their age is frequently a matter of speculation, and in the following table the European equivalents of the pre-Karroo formations in many regions must be regarded as subject to considerable revision.

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  • They are unfossiliferous, and in the absence of undoubted Cambrian, Ordovician and Silurian strata in Africa they may be regarded as of older date than any of these formations.

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  • Some unfossiliferous conglomerates, sandstones and dolomites in South Africa and on the west coast are considered to belong to the Cambrian, Ordovician and Silurian formations, but merely from their occurrence beneath strata yielding Devonian fossils.

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  • The rocks are typically ' cleaner ' quartz sands and rather unfossiliferous apart from beds of microscopic sponge spicules.

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  • They consist of a series of unfossiliferous crystalline slates.

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  • In the north the plateau is overlain by red and purple unfossiliferous sandstones, capped near its edge by a cherty limestone also unfossiliferous but possibly of Lower Cretaceous age.

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  • Greenland, but as they are unfossiliferous sandstone, rapidly disintegrating, this cannot be known.

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  • The former appears to be almost unfossiliferous, the latter has yielded a rich marine fauna, which belongs to the top of the Carboniferous or to the Permo-carboniferous.

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  • So far it has proved to be unfossiliferous.

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  • Primary deposits are doubtfully represented by the detached fragments of unfossiliferous strata of Traras, Blida and east of Orleansville.

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    0
  • 1767) in Germany, who distinguished between the primary, or unfossiliferous, and secondary or fossiliferous, formations.

    0
    0
  • From the edge of the coast belt to near the confluence of the Benue and Niger they are overlain by unfossiliferous sandstones, lying undisturbed and possibly of the age of the sandstones of the Congo basin.

    0
    0
  • In the Kharga Oasis the upper portion consists of variously colored unfossiliferous clays with intercalated bands of sandstone containing fossil silicified woods (Nicolia Aegyptiaca and A raucarioxylon Aegypticum).

    0
    0
  • There occur also below the Lias on some parts of the west coast unfossiliferous red sandstones, conglomerates and breccias, presenting lithological resemblance to the Rhaetic group of England.

    0
    0
  • These ancient rocks, which form the foundation of the country, are overlaid unconformably by a series of conglomerates and sandstones, generally unfossiliferous and often red or purple in colour, very similar in character to the Nubian sandstone of Upper Egypt.

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    0
  • Upon them rest the unfossiliferous strata known to Indian geologists as the Transition and Vindhyan series.

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    0
  • The central plateau consists of ancient crystalline rocks with granites overlain by unfossiliferous sandstones and conglomerates considered to be of Palaeozoic age.

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    0
  • The median zone is composed largely of crystalline rocks with granites and some Palaeozoic unfossiliferous rocks.

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    0
  • The second is the zone of the snowy peaks and of the lower Himalaya, and is composed chiefly of crystalline and metamorphic rocks together with unfossiliferous sedimentary beds supposed to be of Palaeozoic age.

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    0
  • In the region of Adigrat the metamorphic rocks are invariably overlain by white and brown sandstones, unfossiliferous, and attaining a maximum thickness of moo feet.

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  • They are interbedded with unfossiliferous sandstones and shales.

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  • It is unfossiliferous except for a few obscure sheils obtained near the base.

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  • Pondoland Cretaceous Series Uitenhage Series Stormberg Series Beaufort Series Ecca Series Dwyka Series Witteberg Series Bokkeveld Series Table Mountain Sandstone Series Includes several independent unfossiliferous formations of pre-Devonian age Cretaceous Carboniferous to Jurassic Devonian Archaean to Silurian(?) { Karroo System Cape System Pre-Cape Rocks Cretaceous System imperfect remains of plants (Spirophyton) are the only fossils, and these are not sufficient to determine if the beds belong to the Devonian or Carboniferous System.

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  • The formations older than the mesozoic are remarkably unfossiliferous, so that the determination of their age is frequently a matter of speculation, and in the following table the European equivalents of the pre-Karroo formations in many regions must be regarded as subject to considerable revision.

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    0
  • They are unfossiliferous, and in the absence of undoubted Cambrian, Ordovician and Silurian strata in Africa they may be regarded as of older date than any of these formations.

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    0
  • Some unfossiliferous conglomerates, sandstones and dolomites in South Africa and on the west coast are considered to belong to the Cambrian, Ordovician and Silurian formations, but merely from their occurrence beneath strata yielding Devonian fossils.

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  • The rocks are typically ' cleaner ' quartz sands and rather unfossiliferous apart from beds of microscopic sponge spicules.

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    0
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