Copyright © Philip M. Parker, INSEAD. Terms of Use.
| Domain | Definition |
Geological | A fracture zone along the ocean bottom where molten mantle material comes to the surface, thus creating new crust. This fracture can be seen beneath the ocean as a line of ridges that form as molten rock reaches the ocean bottom and solidifies. (references) |
Source: compiled by the editor from various references; see credits. | |
Hexadecimal (or equivalents, 770AD-1900s) (references)4F 43 45 41 4E 49 43 53 50 52 45 41 44 49 4E 47 52 49 44 47 45 |
| Leonardo da Vinci (1452-1519; backwards) (references)
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Binary Code (1918-1938, probably earlier) (references)01001111 01000011 01000101 01000001 01001110 01001001 01000011 00100000 01010011 01010000 01010010 01000101 01000001 01000100 01001001 01001110 01000111 00100000 01010010 01001001 01000100 01000111 01000101 |
HTML Code (1990) (references)O C E A N I C   S P R E A D I N G   R I D G E |
ISO 10646 (1991-1993) (references)004F 0043 0045 0041 004E 0049 0043 0053 0050 0052 0045 0041 0044 0049 004E 0047 0052 0049 0044 0047 0045 |
Encryption (beginner's substitution cypher): (references)49373935484337253505239353843484125243384139 |
| 1. Orthography 2. Bibliography |
Copyright © Philip M. Parker, INSEAD. Terms of Use.
