Copyright © Philip M. Parker, INSEAD. Terms of Use.
| Domain | Definition |
Geological | "Hawaiian" eruptions may occur along fissures or fractures that serve as linear vents, such as during the eruption of Mauna Loa Volcano in Hawaii in 1950, or they may occur at a central vent such as during the 1959 eruption in Kilauea Iki Crater of Kilauea Volcano, Hawaii. In fissure-type eruptions, molten, incandescent lava spurts from a fissure on the volcano's rift zone and feeds lava streams that flow downslope. In central-vent eruptions, a fountain of fiery lava spurts to a height of several hundred feet or more. Such lava may collect in old pit craters to form lava lakes, or form cones, or feed radiating flows. (Tilling, 1985). (references) |
Source: compiled by the editor from various references; see credits. | |
Hexadecimal (or equivalents, 770AD-1900s) (references)48 41 57 41 49 49 41 4E 45 52 55 50 54 49 4F 4E |
| Leonardo da Vinci (1452-1519; backwards) (references)
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Binary Code (1918-1938, probably earlier) (references)01001000 01000001 01010111 01000001 01001001 01001001 01000001 01001110 00100000 01000101 01010010 01010101 01010000 01010100 01001001 01001111 01001110 |
HTML Code (1990) (references)H A W A I I A N   E R U P T I O N |
ISO 10646 (1991-1993) (references)0048 0041 0057 0041 0049 0049 0041 004E 0045 0052 0055 0050 0054 0049 004F 004E |
Encryption (beginner's substitution cypher): (references)423557354343354823952555054434948 |
| 1. Orthography 2. Bibliography |
Copyright © Philip M. Parker, INSEAD. Terms of Use.
