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NUMBER 19 FIGURE 2.—Side view of Harleton meteorite, showing flow lines on fusion crust; maximum length of specimen, 21 cm. 63
64 SMITHSONIAN CONTRIBUTIONS TO THE EARTH SCIENCES and the slower-moving vortex pushing the molten material from the rear face to the edge. Where these forces met, a ridge formed around the rear face of a falling orientated body. FIGURE 3.—Side view of Harleton meteorite, showing cuboidal form; maximum length of specimen, 19 cm. 4. The square face (Figure 1) is to some degree ablated but less so than the other faces, and it has totally different flight markings. 5. Since this side has a square outline it repre-
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SMITHSONIAN CONTRIBUTIONS TO THE EA
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Contents MINERALOGY COMPOSITION OF
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Constituent SiO TiO Al 0 fl 2 3 Cr
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PER CENT CBLCIUM FIGURE 3.—The ca
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Constituent TiO,, 2 2 3 FeO* MnO Mg
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20 Cfl 40 .60 SMITHSONIAN CONTRIBUT
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35'50' I L 6.. 3.. 2.. r FOKT DEFIA
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Page 17 and 18: 14 20 SMITHSONIAN CONTRIBUTIONS TO
Page 19 and 20: 16 Constituent Si0 2 TiO2 A12O3 Cr
Page 21 and 22: 18 20 40 £0 SMITHSONIAN CONTRIBUTI
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Page 25 and 26: Abyssal Basaltic Glasses as Indicat
Page 27 and 28: 24 Electron-M icroprobe Analysis An
Page 33 and 34: 30 Hill in the NE Atlantic, and fro
Page 35 and 36: 32 cores the arrangement is stratig
Page 39 and 40: 36 ATLANTIC OCEAN LAT. LONG. DEPTH
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Page 75 and 76: TABLE 1.—Chemical composition in
Page 85 and 86: 82 Literature Cited Bostrom, K., an
Page 87 and 88: Geochemical Differences among Compo
Page 99 and 100: The St. Mary's County, Maryland, Ch
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Page 107 and 108: Mineralogical and Chemical Composit
Page 111 and 112: 108 Sampling Inclusion 1 was taken
Page 115 and 116: 112 15 10 32 3.6 40 44 48 •fl-r O
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114 SMITHSONIAN CONTRIBUTIONS TO TH
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2.0- 1.5- 1.0 0.8 : 0.6: 0.4- 0.2-
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