The derived mathematical function therefore offered some solutions which however were ‘rough approximations’ that allowed for large margins of errors. But at least now they had a stable point of departure. By inputting time as a parameter along with the coordinates of the geographic longitude and latitude as a second parameter, as required, the equation could estimate reasonably well the slope of the crystal in relation to the earth’s radius, with a margin of error ranging from a few decimals to one decimal of a radian for the current spatiotemporal continuum, while the position of the spatiotemporal continuum to which they would like to ‘transfer’ or ‘experience’ had a margin of error of one decimal of a radian, a deviation which created a few hours’ or days’ or even months’ difference, t
