Cintos Research is an independent organization of individuals dedicated to interdisciplinary scientific research into the intersection of our solar system and the earth's geological history.

We wish to pursue the truth, no matter where it leads. But to find the truth, we need imagination and skepticism, both. We will not be afraid to speculate, but we will be careful to distinguish speculation from fact. – Carl Sagan, Cosmos Introduction.

Our current goal is to spark interest in the Carolina bays among members of various professions. Our data is provided freely, and are open to direct collaboration, or to support your independent research.

What is a “Carolina Bay”, and why should one care”? The following quote is from the abstract of a 1998 PhD dissertation by Timothy D. Nifong:

Carolina bay depressions, once thought to number in the hundreds of thousands, are substantially rarer than previously believed. I estimate that fewer than 900 bay depressions with relatively unaltered site hydrologies remain within the study area. Those that do remain continue to disappear at an alarming rate. North and South Carolina bay depressions are important refuge for wildlife and for plant populations, including more than 65 "special status" plant species. Field observations and pertinent literature indicate that bay vegetation at relatively intact sites is highly dynamic, and that depression vegetation responds dramatically to differences in site disturbance regimes. Development of surrounding upland areas has resulted in increased isolation of Carolina bay depressions from the once pervasive role of fire as a landscape disturbance factor, and in the lowering of regional water tables. Consequently, bay vegetation has undergone an apparent "homogenization", with concomitant decreases in species richness and community diversity. If Carolina bay biodiversity is to be conserved and protected, increased and immediate attention must be given to prioritization, acquisition, and restoration of bay systems.

My personal energies have been directed at socializing the bays - for the pressing ecological reasons, but also to encourage scientists in general to consider research into how they were created.

Gradualistic processes are considered by modern science to be responsible for the creation and evolution of the Carolina bay phenomenon. Given our LiDAR views of 45,000 bays perfectly formed and aligned landforms, that approach seems silly. For a full explanation of our speculation as to the origin of the Carolina Bays, please see the Saginaw Manifold pages on, where we explore a cosmic impact into the Saginaw Bay area of Michigan at the time of the Mid-Pleistocene Transition, ~800,000 years ago.

A talk entitled “A Tale Of Two Craters: Coriolis-Aware Trajectory Analysis Correlates Two Pleistocene Impact Strewn Fields And Gives Michigan A Thumb” was presented at the GSA’s North-Central Section 2015 Meeting in Madison, WI. The abstract is linked above, and a PDF version of the talk is available from the GSA via the link HERE.

Pleistocene Epoch cosmic impacts have been implicated in the geomorphology of two enigmatic events. Remarkably, in both cases spirited debates remain unsettled after nearly 100 years of extensive research. Consensus opinion holds that the Australasian (AA) tektites are of terrestrial origin despite the failure to locate the putative crater, while a cosmic link to the Carolina bays is considered soundly falsified by the very same lack of a crater.

A challenging aspect of the hypothesis involves the lack of an identifiable impact structure. The conjecture suggests an extremely oblique - nearly tangential-impact, and that terrestrial material ejected from such an event would be distributed in a stylized manner. Our analysis correlates numerous proposed ejecta material emplacements - including the Carolina bays and the Goldsboro Ridge - to a cosmic impact event that struck the Laurentide ice shield at ~43°N, ~87°W. The proposed cratering impact, when combined with the scouring action of 7 full glacial ages, is seen producing the current-day Saginaw Bay Basin. We have followed the chronological constraints to a proposed date of ~780 ± 10  thousand years ago.

If you are a Google Earth user, you can click the GE logo here to download a starter kmz.

At present, the survey project is unfunded. Please contact us if should you chose to assist.

Michael Davias
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