![]() It seems likely that difficulty in estimating transient depth arises due to the 2Ga history of erosion in the area as such the best option is probably to appeal to uniformitarianism, and assume that the Vredefort-forming impact obeyed the same diameter-depth relationship as has been modelled for the population of recent craters in works cited above. (2003) suggest that for an impactor of 10km diameter the maximum transient crater depth will be 24km. Browse 45 badlands guardian photos and images available, or start a new search to explore more photos and images. The high rock formations seem to dare and challenge you to. That area is a type of other-worldly experience, as if the land holds mysteries and myths hidden deep within the buttes. Wünneman & Ivanov (2003), which also discusses crater morphology meanwhile Turtle et al. Badlands National Park is not only one of the most amazing scenic spots in the world, but it is also one of the most eccentric. Viewed from the air, the feature has been said to. Numerical modelling of the impact diameter-crater depth relationship has been carried out: see e.g. 2.6K views 1 year ago The Badlands Guardian is a geomorphological feature located near Medicine Hat in the southeast corner of Alberta, Canada. (2008) also give no estimate of transient depth. does not take into account the extensive erosion that has occurred in this location. ![]() Dietz (1961) describes the impact crater as "40km across and 16km deep" - i.e. Turtle & Piarazzo (1998) suggest a smaller initial diameter but make no estimates of the depth they do, however, suggest an impactor of 10-14km diameter. (1993) suggest an initial diameter of 192-300km. ![]()
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