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Is the Teluk Tomini - the gulf on the Equator surrounded by the
graceful arc of Sulawesi (the Celebes) - possibly an impact crater? (I am not referring to volcanic craters.) |
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![]() "Axel Harvey" wrote in message om... Is the Teluk Tomini - the gulf on the Equator surrounded by the graceful arc of Sulawesi (the Celebes) - possibly an impact crater? (I am not referring to volcanic craters). A.H.: There is no evidence for that. Shocked quartz, high-pressure quartz polymorphs,diaplectic glass in any plagioclase, impact breccias, shatter cones ,signatures of telltale extraterrestrial elemental concentrations and the distinctive bulge of basement rocks in a crater--all of which are indicative of impact sites-- are lacking in the Tomini area. Furthermore, Indonesia has the largest population of volcanos on the globe and the movement of the sea floor under Northern Sulawesi contributes to the ring of fire having overseen the many eruptions of volcanos and explosions of volcanic islands in the Gulf of Tomini which have been recorded throughout this and the last century. Another factor militating against your mentioned possibility is that the pyroclastic deposits in the area are all explicably volcanic in origin. I hope that helps. Regards, Edward Hennessey |
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(Axel Harvey) wrote in message . com...
(don findlay) wrote: (Axel Harvey) had written: Is the Teluk Tomini - the gulf on the Equator surrounded by the graceful arc of Sulawesi (the Celebes) - possibly an impact crater? (I am not referring to volcanic craters.) "The radial-concentric structure is an intriguing one, and invites consideration of the impact option. " http://users.indigo.net.au/don/re/looking.html The problem with it being an impact structure is the protracted growth of all the related elements - unless we can think of the aftermath of really big impacts happening in 'slow motion'. If it is an impact structure, the most likely candidate was the Moon, when the Earth was much smaller: impact ignites some sort of nuclear fire in the core. Maybe? Could you expand on your answer? I am not an Earth scientist, and the Moon is still up there... I'll reply later. I just want to say (whilst I see Edward's post) that the two styles of impacts (and their results) are not comparable. Compare say, a grain of sand blown against the windscreen of your car (and the tiny nick that might arise from that) against, say, a meteorite crater e.g:- http://ottawa.rasc.ca/astronomy/earth_craters/barringer/ Further along the scale we have the possibility of Moon - Earth collision. The prospect really defies imagination, but though it's conceptually easier to keep the moon at a distance, one must still admit the possibility, although the results are difficult to imagine. Like two blobs of jelly I would think (brittle shock tectures? surely not; much volcanism? Surely yes.) hat (difference in scale) is what makes me think the effect could well be different/ much more protracted in time too - no sharp shock, but a prolonged period of deformation and "phase change" (water production) - however that might be understood from a dense plasma-like core "...that most simulates iron". (Sorry Edward - no comparison) (The Moon still up there? Yes, but look at it! Talk about battle scarred and bleeding!!) (well, ..past tense) |
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