The fact that trends in O isotopic values vs. elevation and distance inland are consistent, supports this method of determining paleoelevations from surface temperatures that much more. I also support this because of climate change. Climate change introduces many variables that can drastically change current, future elevations or paleoelvations. This method is able to correlate to a climate model and for this reason makes the evidence or accuracy of the method even more pronounced. In future studies, this method can be used in correlation with other methods such as leaf physiognomy or the less accurate cosmogenic radio nuclide dating techniques. A possible study site for this can be the Wind River Range in Wyoming because there are many geologic variables in this region such as wind, erosion and huge climate variations throughout the year. Also, there are a lot of alpine lakes where carbonate clumped- isotopes can be used to study the sedimentary deposits and paleoelevations from past surface temperatures. Further studies can establish the accuracy of this method to a higher degree and lead to new discoveries in the geologic and science realm. Through the support of all the methods discussed, whether accurate or not, I have determined that the Rockies and the Colorado Plateau began to rise about 65 million years