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entablatures

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Figure 10. Average column-bounding fracture spacing within flow A ( Fig. 3A...
Published: 01 March 2004
Figure 10. Average column-bounding fracture spacing within flow A ( Fig. 3A ). Spacing is least at the top surface of the flow and increases from both the upper and lower boundaries toward the central entablature. Entablatures prevent trailing column-bounding fractures of the upper and lower
Image
(a) Exceptionally well-developed chisel marks on joint columns forming the ...
Published: 16 May 2022
Fig. 1. (a) Exceptionally well-developed chisel marks on joint columns forming the colonnade of the Garni intracanyon lava flow, Armenia, a basaltic trachyandesite of mid-Pleistocene age (Neill et al. 2015 ). Geologist is Davit Manucharyan. (b) Colonnade and overlying entablature in a dipping
Image
Features of a very thick sheet lobe exposed on the National Highway 8B near...
Published: 16 May 2022
Fig. 9. Features of a very thick sheet lobe exposed on the National Highway 8B near Bamanbor. (a) Road-cut through a thick entablature (12 m exposed, person for scale). Around this location the entablature is traversed by master joints with a roughly equal spacing of ∼6 m, one of which is seen
Journal Article
Journal: GSA Bulletin
Published: 01 September 1986
GSA Bulletin (1986) 97 (9): 1144–1155.
...PHILIP E. LONG; BERNARD J. WOOD Abstract Flood basalt flows of the Columbia River Basalt Group commonly exhibit well-developed colonnade and entablature structures formed during cooling of individual flows. The colonnade refers to the well-defined columnar structure of many flows, which appears...
Journal Article
Published: 16 May 2022
Geological Magazine (2022) 159 (8): 1415–1436.
...Fig. 1. (a) Exceptionally well-developed chisel marks on joint columns forming the colonnade of the Garni intracanyon lava flow, Armenia, a basaltic trachyandesite of mid-Pleistocene age (Neill et al. 2015 ). Geologist is Davit Manucharyan. (b) Colonnade and overlying entablature in a dipping...
FIGURES | View All (14)
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Figure 3. Cross-section fracture maps of four Box Canyon flows having diffe...
Published: 01 March 2004
Figure 3. Cross-section fracture maps of four Box Canyon flows having different aspect ratios (AR = width/height). Approximate aspect ratios for flows A–D are respectively 5, 4, 3, and 1. AR affects entablature shape (gray regions), inflation-fracture locations (crosses), and the flow-scale pattern
Journal Article
Journal: GSA Bulletin
Published: 01 March 2004
GSA Bulletin (2004) 116 (3-4): 322–336.
...Figure 10. Average column-bounding fracture spacing within flow A ( Fig. 3A ). Spacing is least at the top surface of the flow and increases from both the upper and lower boundaries toward the central entablature. Entablatures prevent trailing column-bounding fractures of the upper and lower...
FIGURES | View All (11)
Journal Article
Journal: Geology
Published: 01 February 2009
Geology (2009) 37 (2): 171–174.
... in the best observations. The foreshortening may also be worse than ideal. Columns and possibly multiple tiers of columns and/or entablature are visible. Many of the craters exposing columnar jointing formed in regions with histories of extensive volcanic activity. For example, Elysium Planitia...
FIGURES | View All (4)
Journal Article
Published: 01 July 2000
Journal of the Geological Society (2000) 157 (4): 715–722.
...-columnar parts of the lava (the entablature) shows textural signs of quenching, compared with the lower more regular columnar zone (the colonnade). These common field and petrographic features confirm the model of multi-tiered flow formation by modification of the cooling regime in the upper part...
FIGURES | View All (19)
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Features of sheet lobes exposed 3 km southwest of Talaja on the road to Mah...
Published: 16 May 2022
Fig. 4. Features of sheet lobes exposed 3 km southwest of Talaja on the road to Mahuva. Location of the outcrop is 21° 19′ 59.9″ N, 72° 00′ 49.4″ E, elevation 36 m. Persons provide a scale in all photographs. (a) Broad view of a sheet lobe SS15 with entablature and colonnade tiers. The lobe dips
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Figure 6. <span class="search-highlight">Entablature</span>-fracture evolution. (A) Column-bounding fractures (da...
Published: 01 March 2004
Figure 6. Entablature-fracture evolution. (A) Column-bounding fractures (dashed lines) are the first fractures to propagate through an entablature. (B–E) Successive generations of fractures (thick black lines) then dissect the blocks of basalt delineated by preceding generations (gray lines). (F
Image
Photographs of intracanyon dam remnants showing cooling structures. (A) Col...
Published: 01 October 2015
Figure 20. Photographs of intracanyon dam remnants showing cooling structures. (A) Columns in the entablature of a remnant at river mile (RM) 184R are orthogonal to a master fracture due to convective flow of water in the fracture. (B) Most remnants (like this one from RM 194R) have a much
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Figure 2. Internal morphology of a typical pahoehoe basalt flow. An upper c...
Published: 01 March 2004
Figure 2. Internal morphology of a typical pahoehoe basalt flow. An upper colonnade and a lower colonnade are separated by a more intensely fractured entablature. Upper colonnades contain column-bounding and column-normal fractures, whereas lower colonnades are almost exclusively composed of column
Journal Article
Published: 01 September 2001
The Journal of Geology (2001) 109 (5): 585–601.
... layer located at the contact of the colonnade with the overlying entablature; and type 3, very thick (up to 96 m) lens-shaped accumulations within thickened portions of the flow. No single mechanism is capable of generating all three types. Our evidence indicates that most type 1 segregations were...
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Figure 11. Relative-fracture-density plots for the four fracture maps in th...
Published: 01 March 2004
flows having a higher aspect ratio. Flow tops and inflation-fracture locations also show high fracture densities. Entablature locations are shown in white with black borders. Entablature-fracture densities are not included in this analysis.
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Thin-section photomicrographs showing representative views of the colonnade...
Published: 16 May 2022
Fig. 12. Thin-section photomicrographs showing representative views of the colonnade and entablature of the Bamanbor sheet lobe under the petrological microscope. Plagioclase (Pl) grains (both phenocrysts and in the groundmass) are lath-shaped, and the clinopyroxene (Cpx) grains are equant
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(a–e) A series of cartoons schematically illustrating the concepts of the f...
Published: 16 May 2022
Fig. 14. (a–e) A series of cartoons schematically illustrating the concepts of the formation of lava morphotypes slabby pāhoehoe and rubbly pāhoehoe, and of entablature and colonnade tiers in sheet lobes (here of rubbly pāhoehoe). (a) A small pāhoehoe lobe being emplaced develops an upper crust
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The colonnade (a) and <span class="search-highlight">entablature</span> (b) joint tiers, Fingal’s Cave, Staffa.
Published: 01 July 2000
Fig. 2. The colonnade (a) and entablature (b) joint tiers, Fingal’s Cave, Staffa.
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Photograph of <span class="search-highlight">entablature</span> with fanning and radiating patterns in a lava flo...
Published: 01 February 2009
Figure 4. Photograph of entablature with fanning and radiating patterns in a lava flow that dammed Little Colorado River in northern Arizona.
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Polygonal <span class="search-highlight">entablature</span> blocks 2–3 m across which have broken along master jo...
Published: 01 July 2000
Fig. 9. Polygonal entablature blocks 2–3 m across which have broken along master joints in the lava flow.