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Physical Sciences and Mathematics Commons™
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Full-Text Articles in Physical Sciences and Mathematics
Craters And Cracks Caused By Accelerated Nuclear Decay Heat Throughout The Solar Systemaccelerated Radioactive Decay Heat In The Solar System And Its Implications For Earth, Don Stenberg Jr.
Proceedings of the International Conference on Creationism
When we look throughout the solar system, we see evidence for accelerated radioactive decay such as fission tracks and isotope ratios. We also see the major effects of that decay heat, including the thermal expansion of planets and moons, massive lava flows, volcanic activity associated with craters, and more. These findings challenge that conventional impact theory of crater formation, and instead suggest that the creation scientists of the 1600s to 1800s were correct that the majority of craters were probably formed by immense explosions. We can now infer the energy source to be accelerated nuclear decay. If this decay heat …
Find The Distance To The Moon, Dean Smith
Find The Distance To The Moon, Dean Smith
AI Assignment Library
This assignment leads students through a series of measurements that lead the student to calculate the distance to the Moon. Students who complete this assignment will see how knowledge that they would normally look up is gathered through experiment and observation.
What Is A Polygonal Impact Crater? A Proposed Framework Toward Quantifying Crater Shapes, Stuart J. Robbins, Jamie D. Riggs
What Is A Polygonal Impact Crater? A Proposed Framework Toward Quantifying Crater Shapes, Stuart J. Robbins, Jamie D. Riggs
College of Population Health Faculty Papers
Impact craters are used for a wide array of investigations of planetary surfaces. A crater form that is somewhat rare, forming only ∼10% of impact craters, is the polygonal impact crater (or PIC). These craters have been visually, manually identified as having at least two rim segments that are best represented as straight lines. Such straight lines or edges are most often used to infer details about the subsurface crust where faults control the structure of the crater cavity as it formed. The PIC literature is scant, but almost exclusively these craters are identified manually, and the potentially straight edges …