1. Marlène Blin (1975-), French journalist with France 3

2. A thick porous chalk subsoil covered with marl, clay or sand.

3. Collusion Plus super wide leg seam front joggers in grey marl.

4. Cayman Marl Road is the authentic, raw and to the point news

5. Old alluviums mixed with flat and rounded stones, and with some chalk marl and clay.

6. Soil type consisting of marl and limestone common in Alsace dating back from the Upper Triassic period.

7. Marl clay A2: In this variant, the mineral additives are very fine and homogeneously distributed through the paste.

8. The projecting porch with its embattled parapet is rendered with local marl and is a late sixteenth-century addition.

9. The limestone/marl alternation of the Zlambach Beds can be subdivided into an autochthonous background sedimentation and an allochthonous carbonate sedimentation.

10. Possible related people for Marlene Caporiccio include Anthony A Caporiccio, Marl Caporiccio, Robert P Caporiccio, Robert Pino Caporiccio, Michelle E Curet.

11. Soil type consisting of various compositions of sandstone, marl, dolomite, and shingle common in Alsace dating back from the Middle Triassic period.

12. Up to 10% cash back  · arthrolite, Arthrolith [ A cylindrical concretion intersected by transverse cracks and found in shales, marls and clays] Arthrolith m

13. For example, Argillaceous limestones are limestones consisting predominantly of calcium carbonate, but including 10-40% of clay minerals: such limestones, when soft, are often called marls.

14. For example, Argillaceous limestones are limestones consisting predominantly of calcium carbonate, but including 10-40% of clay minerals: such limestones, when soft, are often called marls.

15. The race starts at Marl Pitts and is well known for being the muddiest and Boggiest course and this year did not disappoint

16. It is situated in a sequence of soft sandstone, siltstone and marl with the layers inclined at an angle of about 20°.

17. The soils on the hills are derived from lime, marl or clay substrates and those on the plains from loose, alluvial substrates.

18. The subsoil consists of clay and marl or silty sand topped by a layer of silt several metres thick formed from vegetable and animal substances.

19. The new ammonoid speciesDesmoceras (Pseudouhligella) intrapunctatum (DesmoceratoideaZittel, 1895) is described and figured from the dark glauconitic marls of the Lower Albian of Ambatolafia (Mahajanga Basin of northwestern Madagascar).

20. The Crenulate lead-plant is a perennial, deciduous shrub that inhabits marl prairies and wet pine rocklands in a small area of Miami-Dade County

21. The paleographic pattern of the Upper (“White”) Jurassic of the Suebian Alb mountain area is characterized by intersecting of algal-sponge-reef and micritic limestone-marl facies.

22. Upper Cretaceous cyclic sequences in Germany and marl–opal-rich Tortonian-Messinian strata in the Sorbas basin related to multiple sea drawdown have been correlated with Milankovitch orbital forcing.

23. - ON PLAINS AND/OR PLATEAUX ON AN AUTOCHTHONOUS SUBSTRATUM OF CALCAREOUS ROCK , MARL OR SAND OR COLLUVIAL OF MORAINIC , GLACIAL OR VOLCANIC ORIGIN , OR ALLUVIAL ORIGIN BUT COARSE IN COMPOSITION ,

24. Chalcedony can be found as vein fillings or crusts in volcanic rocks, as the main constituent in silica-rich marine sedimentary rocks, as layers in limestone and marls, as cement in sandstones, and as a fossilizing material

25. 6 The Saliyak melange consists of dark-gray to black muddy and silty microclastic rock with intercalation of grayish purple and grayish green calcareous and muddy shale, marl and tuff.

26. Constitutively, these deposits are accumulations of gravel and sand covered by a layer of Quaternary clayish loess sediments, which lies on top of marine sediments (marl, clay, sand) of the Pliocene era.

27. The post-Cambrian marine sedimentation is made up of alternate layers of limestone, dolomites, schists and clays, with the successive series of Pliocene sedimentations represented by basal conglomerates, marls, clays and finally loose sandstones and sand

28. The post-Cambrian marine sedimentation is made up of alternate layers of limestone, dolomites, schists and clays, with the successive series of Pliocene sedimentations represented by basal conglomerates, marls, clays and finally loose sandstones and sand.

29. - ON PLAINS AND/OR PLATEAUX ON AN AUTOCHTHONOUS SUBSTRATUM OF CALCAREOUS ROCK , MARL OR SAND OR COLLUVIAL OF MORAINIC , GLACIAL OR VOLCANIC ORIGIN , OR OF ALLUVIAL ORIGIN BUT COARSE IN COMPOSITION ,

30. They consist of alternate layers of clay or marl and discontinuous layers of sand, sandstone or limestone, with the occurrence of calcareous banks that are increasingly frequent and increasingly thick to the west.

31. Newly collected material from Mississippi’s Matthews Landing Marl Member of the Porters Creek Formation (Late Paleocene: Selandian) with well preserved anastrophic protoconchs provides evidence that this species belongs to the Heterostropha/Heterobranchia.

32. Building materials (non-metallic), alabaster, artificial stone, bricks, building stone, cement, clay, concrete building elements, concrete, construction materials (not of metal), fire clay, gypsum, marl, plaster, stone, terracotta, building materials formed from recycled or recovered materials

33. Cement generally refers to a very fine powdery substance chiefly made up of limestone (calcium), sand or clay (silicon), bauxite (aluminum) and iron ore, and may include shells, chalk, marl, shale, clay, blast furnace slag, slate.

34. 5). A diagram of the E-W section along the Southern Franconian Alb and the Swabian Alb exhibits the transition from the Franconian platform into the Swabian marl basin and the Swabian reef area (Fig.

35. Calcareous rocks are formed from a variety of chemical and detrital sediments such as limestone, dolostone, or marl and are largely composed of calcium oxide (CaO), magnesium oxide (MgO), and carbon dioxide (CO 2), with varying amounts of aluminum, silicon, iron, and water

36. 2¿/g), whereby up to half of this proportion can be substituted by aluminosilcates such as fly ash, alumina, marl or the like. The slag cement also comprises 0.1 to 2 wt. % clinker, sulfate provided in quantities of less than 5 wt. %, calculated as SO¿3?, and 0.3 to 1 wt. % of a superliquifier such as naphthalene sulfonate.