1. How to say Basaltic in English? Pronunciation of Basaltic with 1 audio pronunciation, 1 synonym, 13 translations, 5 sentences and more for Basaltic.

2. Subaerial Basaltic flows and breccia and submarine Basaltic breccia, pillow lavas, lapilli and augite-rich tuff with interbeds of Basaltic sandstone, siltstone, and conglomerate

3. What does Basaltic mean? Information and translations of Basaltic in the most comprehensive …

4. Basaltic: 1 adj of or relating to or containing basalt “ Basaltic magma is fluid”

5. Basic or Basaltic or Shield lava

6. Basaltic Crustally-contaminated andesites could be produced by combined assimilation and fractional crystallization of Basaltic magmas

7. Definition of Basaltic in the Definitions.net dictionary

8. The Basaltic andesites are fresh as shown petrographically (Figs

9. There are diabase, basaltic, porphyritic, and other types of Amygdaloids

10. Basaltic liquids are characterized by low viscosities and relatively low volatile contents, such that Basaltic eruptions tend to be more effusive than explosions

11. The lower flanks consist of mostly basaltic and some andesitic lavas.

12. However, it seems that these lavas were originally basaltic andesites.

13. ‘Also of interest in the area is a Basaltic column by the sea near Owenga.’ ‘To the east was the thin crust of soil that covered the great Basaltic flows of the Great Basin.’ ‘It consists of a type of Basaltic rock favourable to the growth of almond trees.’

14. All these Basaltic channels are called cut rocks by the trappers.

15. Any planet with basaltic volcanism, any rocky planet, will probably have lava tubes.

16. Basaltic farms USDA certified organic garlic is suitable for eating and planting

17. Basaltic lavas are more fluid than andesites or dacites, which contain more silica

18. ‘Also of interest in the area is a Basaltic column by the sea near Owenga.’ ‘To the east was the thin crust of soil that covered the great Basaltic flows of the Great Basin.’ ‘It consists of a type of Basaltic rock favourable to the growth of almond trees.’

19. Includes some Basaltic andesite and, near the top of the sequence, some dacite

20. One major difference between Basaltic and granitic magma is their specific mineral contents

21. However, this doesn’t mean that Basaltic lavas always flow quietly from the Earth.

22. A study of strength and deformation measurements for Basaltic rocks, along with consideration of the influence of fracturing using a rock mass classification system, documents the range of brittle response for Basaltic rock masses

23. Sams Creek Metabasalt - Altered basaltic flows, some Amygdaloidal; green, schistose, containing hornblende, epidote, chlorite, and quartz

24. This leads to geyser-like eruptions of CO2 gas mixed with dark basaltic sand or dust.

25. Highest yields occur in basaltic rocks and are due to primary and secondary porosities.

26. Igneous rocks, especially glassy basaltic rocks are more susceptible to weathering and alteration forming halloysite.

27. The deposit is composed of Basaltic to andesitic vesiculated pyroclasts (scoria) lying near the eruptive vent

28. ‘A‘a types of blocky, cinder and breccia flows of thick, viscous Basaltic lava are common in Hawaii

29. Alkali basaltic rocks are enriched in LILE, LREE (Lan/Ybn = 10–19) and HFS elements.

30. From the Cambridge English Corpus The role of mantle plumes, particularly in the generation of flood Basaltic …

31. 13 Three small NEAs have spectra very similar to those of basaltic achondrites and of the asteroid Vesta.

32. Basaltic cinders are often red, coloured by oxidised iron from weathered iron-rich minerals such as pyroxene

33. The lava first very acidic became basaltic and spread over large fluid lava flows which covered the structure’ slopes.

34. 1st Stance: Basaltic Fist is the first stance of the Dance of Four Gods set of techniques

35. Augitite: In petrography , a non-feldspathic, basaltic rock consisting essentially of augite and magnetite with a generally scanty glass base

36. The late-Quaternary Icelandic-type basaltic Bely shield volcano in the northern Sredinny Range is topped by a small stratovolcano

37. Basaltic rocks at mid-ocean ridges, large igneous provinces and subduction zones have compositions at the silica-rich end of the range of composition, while silica-poor Basaltic rocks are largely confined to intraplate settings (ocean islands, isolated continental volcanic areas, and rift systems).

38. The late-Quaternary Icelandic-type basaltic Bely shield volcano in the northern Sredinny Range is topped by a small stratovolcano

39. Basaltic magmas contain around 50% silica; they are the most common extrusive rocks and comprise more than 90% of all volcanic rock

40. Basaltic andesites and andesites (SiO2 % = 50−59), erupted from Atitlán volcano located nearer to the trench, have the lowest degree of disequilibrium.

41. During the Cainozoic there was widespread basaltic igneous activity in eastern Austra- lia along and adjacent to the Eastern Highlands

42. Basaltic magmas that form the oceanic crust of Earth are generated in the asthenosphere at a depth of about 70 kilometres

43. Basaltic lavas are frequently spongy or pumiceous; the steam cavities become filled with secondary minerals such as calcite, chlorite, and zeolites

44. 20 A hornito is a small rootless spatter cone that forms on the surface of a basaltic lava flow (usually pahoehoe).

45. This paper reports the results of a detailed experimental investigation of fractionation of natural Basaltic compositions under conditions of high pressure and high temperature

46. One is represented by the 3.42 b.y. old aluminous basalt fragments, the other by the dominant component in the microbreccia fragments and basaltic glasses.

47. Rock types found in the mountainous volcanic districts include rhyolites, trachytes, dacites, andesites, basaltic lavas, widespread pyroclastic formations, and associated alluvial and lacustrine deposits.

48. The Miocene volcanic suite of Sierra de Gata (Betic Cordillera) is composed of dacites, rhyodacites and rhyolites, besides basaltic andesites and andesites.

49. Volcán Cay, located E of Macá volcano and NW of the town of Puerto Aisén, is a basaltic to dacitic stratovolcano

50. This strongly suggests that injections of melts with alkali basaltic affinity which had precipitated Group 11 rocks resulted in diffusion metasomatism on the Group I rocks.

51. The term “amygdaloid” refers to the texture of the effusive rock regardless of its mineral composition. There are diabase, basaltic, porphyritic, and other types of Amygdaloids

52. Basaltic rock that cools slowly in a large thick layer will often form a distinctive hexagonal prismatic columnar jointing that produces "columnar basalt"

53. Comparison with other types of mafic rocks shows that Pd/Ir ratios increase with decreasing alkalinity in basaltic rocks but plunge to alkali-basalt values in komatiites.

54. Northeasterly trending, tholeiitic, low-alkali basaltic dikes which cut the Archean rocks of northeastern Manitoba have yielded a paleomagnetic pole at 114°W, 28°N, α95 = 12°.

55. Basaltic rocks rise perpendicularly, so that it is impossible to get from the plain to the water, or from the river margin to the plain

56. Although basalts vary widely in composition and other physical factors, many of the properties of a Basaltic rock mass appear to vary within a factor of about …

57. Batholithic rocks formed from the mixing of basaltic and quartzo- feldspathic end-member magmas, and the removal of variable propor­ tions of plagioclase and mafic minerals, principally hornblende

58. Rock magnetism of ejected Basaltic boulders from Lonar crater, India: Implications for the existence of a short‐lived impact‐generated weak magnetic field Posted by Administrator 0

59. Basaltic lavas tend to be fluid and form thin flows that have a considerable amount of primary pore space at the tops and bottoms of the flows

60. Though typical of basaltic rocks, augite is also an important constituent of many other kinds of igneous rocks, and a rock composed almost wholly of augite is known as Augitite

61. All the Basaltic magma that is pushed out of the mantle to the crust due to convection currents is constantly pushed away from the fissures due to new magma flow.

62. Geologic unit mapped in Oregon: Lava flows and flow breccia of hypersthene and olivine andesite, Basaltic andesite containing plagioclase and pyroxene phenocrysts, and basalt; many flows contain phenocrysts of both hypersthene and augite

63. A single stage, piston-cylinder apparatus has been used in the pressure range up to 27 kb and at temperatures up to 1500° C to study the melting behaviour of several Basaltic compositions.

64. Volcanoes within the field have produced smaller amounts of basaltic andesite and andesite with silicon dioxide compositions up to 59 percent, though dacite is not very common among Indian Heaven eruptive products.

65. The mineral chemistry of several Pliocene alkali basaltic rocks from Burgenland and Styria (Eastern Austria) have been investigated in order to determine the evolution path of the basalt magmas prior to eruption.

66. Amygdaloid (countable and uncountable, plural Amygdaloids) A variety of trap or basaltic rock, containing small cavities, occupied, wholly or in part, by nodules or geodes of different minerals, especially agates, quartz, calcite, and the zeolites

67. Basaltic magma contains between 45 and 55 percent silicon dioxide and is high in magnesium, iron and calcium, while granitic magma contains between 65 and 75 percent silicon dioxide and only small amounts of those minerals.

68. Explain the differences between Basaltic, Rhyolitic and Andesitic volcanic eruptions with reference to processes, which lead to the eruptions, the type of volcano produced and the reasons for the differences between the material erupted by these volcanoes

69. Textural and mineralogical features of potash-rich basaltic rocks of the absarokite-shoshonite-Banakite series strongly suggest that most of the large crystals and aggregates in these rocks are xenocrysts and microxenoliths, not true phenocrysts as was previously thought.

70. The formation of alunite from natural leucite, nepheline, sodalite, potassium-feldspar, oligoclase and sericite as well as from basaltic-glass, trachyandesite, nephelinebasanite and nephelinite was experimentally investigated at different H2SO4-concentrations in the temperature range from 90° to 180° C.

71. In rock samples of a Middle Devonian spilitized basaltic sill near Langelsheim (Northwestern Harz Mountains) the following mineral assemblage: pumpellyite + prehnite + epidote + actinolite grown in a groundmass of albite, chlorite, calcite and quartz has been studied by use of a microprobe.

72. Batholithic residua likely to be amphibole rich, relatively feldspar poor, and to have modest amounts of garnet, are consistent with high pressure (>10 kbar) melting experiments of a basaltic source (e.g., Rapp et al., 1991; Wolf and Wyllie, 1993, 1994)

73. These lava tubes can be found at many of the lava flows that comprise the Indian Heaven volcanic field, which range from basaltic to andesitic in composition, and extend as far as 29 miles (46 km) from their source vents.

74. Furthermore, Basaltic and gabbroic rocks of the ocean basins represent magmas that have the least likelihood of being contaminated with continental crustal material, and thus should give us the best clues to the composition of and chemical evolution of the underlying mantle …

75. It is noteworthy that Sunda clinopyroxene shows strong analogies with that from basaltic rocks from the Ethiopian plateau and K-rich lavas from the Roman Province respectively, reflecting similarities between the composition and mineralogical assemblages of the host rocks, although they all came from different tectonic environments.

76. Basaltic breccia: 36: northwestern Africa: 21.2: 2.7: N: meteorite name: when found or purchased: lunar rock type 1: mass (grams) where found or purchased: total Fe as FeO (%) Th (ppm) click on number for chemical classification: largely unbrecciated mare basalts: 133: Northwest Africa 4898: 2007: mare basalt: 137: northwestern Africa:

77. As nouns the difference between Amygdaloid and amygdala is that Amygdaloid is a variety of trap or basaltic rock, containing small cavities, occupied, wholly or in part, by nodules or geodes of different minerals, especially agates, quartz, calcite, and the zeolites when the imbedded minerals are detached or removed by decomposition, it is porous, like

78. Ocean island Basaltic magmas are enriched in H 2 O relative to depleted MORB, giving rise to the possibility that the excess magmatism associated with mantle plumes is caused, at least in part, by the effect of higher H 2 O on mantle melting rather than solely being due to high mantle potential temperature (Schilling et al., 1980; Bonatti, 1990).

79. Basaltic Basalt Gabbro 45-55 SiO2 %, high in Fe, Mg, Ca, low in K, Na 1000 - 1200 oC Low Low Intermediate or Andesitic Andesite Diorite 55-65 SiO2 %, intermediate in Fe, Mg, Ca, Na, K 800 - 1000 oC Intermediate Intermediate Felsic or Rhyolitic Rhyolite Granite 65-75 SiO2 %, low in Fe, Mg, Ca, high in K, Na 650 - 800 oC High High Origin of Magma