Talk:Emperor of China (volcano)
From Wikipedia, the free encyclopedia
 |
Emperor of China (volcano) is part of WikiProject Indonesia, which aims to improve Wikipedia's coverage of Indonesia and Indonesia-related topics. If you would like to participate, visit the project page. Please do not substitute this template.
|
| Start | This article has been rated as start-Class on the quality scale. |
| Low | This article has been rated as low-importance on the importance scale. |
|
|
|
 |
This article is part of WikiProject Volcanoes, a project to systematically present information on volcanoes, volcanology, igneous petrology, and related subjects. If you would like to participate, you can choose to edit the article attached to this page (see Wikipedia:Contributing FAQ for more information), or join by visiting the project page. |
|
| Start | This article has been rated as Start-Class on the quality scale. | |
| Mid | This article has been rated as Mid-importance to WikiProject Volcanoes on the project's importance scale. | |
| If you have rated this article please consider adding assessment comments. | ||
 |
An entry from Emperor of China (volcano) appeared on Wikipedia's Main Page in the Did you know? column on 10 March 2007. |
 |
[edit] Translation?
- "The 1–2 km thick of Pliocene–Quarternary sedimentary Damar Basin is relatively flat bottoms.[2]"
I'm not sure how this should be rephrased. 'The Damar Basin is relatively flat bottomed, with 1–2 km of Pliocene–Quarternary sediments.'?
—wwoods 15:39, 16 September 2007 (UTC)
