Description
Both volcanism and impact cratering produce ejecta and associated deposits incorporating a molten rock component. While the heat sources are different (exogenous vs. endogenous), the end results are landforms with similar morphologies including ponds and flows of impact melt and lava around the central crater.
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Contributors
- Stopar, Julie D (Author)
- Robinson, Mark S. (Thesis advisor)
- Bell, James (Committee member)
- Christensen, Philip R. (Philip Russel) (Committee member)
- Clarke, Amanda (Committee member)
- Scowen, Paul (Committee member)
- Arizona State University (Publisher)
Date Created
The date the item was original created (prior to any relationship with the ASU Digital Repositories.)
2016
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Note
- Partial requirement for: Ph.D., Arizona State University, 2016Note typethesis
- Includes bibliographical references (pages 220-253)Note typebibliography
- Field of study: Geological sciences
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Statement of Responsibility
by Julie D. Stopar