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| | siddoway.html |
 | | The Ford Ranges of western Marie Byrd Land (MBL) form a block-faulted topography marked by isolated summit plateaus and scattered outcrops of late Cenozoic volcanic rocks. |
 | | Present mountain topography in western MBL may be a result of Cenozoic extension in the eastern Ross Sea rift (Behrendt et al. |
 | | Luyendyk, B.P.; Smith, C.H.; and van der Wateren, F.M., 1994, Glaciation, block faulting, and volcanism in western Marie Byrd Land, Terra Antartica, v. |
| igloo.gsfc.nasa.gov /wais/pastmeetings/abstracts97/siddoway.html (491 words) |
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