Abstract
A shield volcano has been identified on Io, based on photoclinometrically determined slope values and planimetric presentation. The slope values (typically 10°) and 2.5 km height of the volcano imply that it is composed of a material with the mechanical properties of basaltic rock. The height of the volcano may also indicate a minimum value of ∼40 km for the thickness of the local lithosphere.
| Original language | English (US) |
|---|---|
| Pages (from-to) | 181-183 |
| Number of pages | 3 |
| Journal | Icarus |
| Volume | 67 |
| Issue number | 1 |
| DOIs | |
| State | Published - Jul 1986 |
| Externally published | Yes |
ASJC Scopus subject areas
- Astronomy and Astrophysics
- Space and Planetary Science