The drift is a remarkable stratum of clay, sand, gravel, and far-from-source boulders seemingly flung by some careless hand over the northern portions of Europe and North America. Some of this debris has been moulded into distinctive ridges (moraines), rounded hills (drumlins), and long sinuous ridges (eskers). Any theory of drift formation must account for these singular accumulations as well as an immense family of scratches, lake basins, and sundry gougings.
“Just as in the case of all other countries, the earliest pages in the Geological Record of South Africa are most fragmentary and utterly confusing; much remains to be done before even the outlines can be reconstructed. It must suffice to remark that at some extremely remote date, possibly more than 1000 million years ago, basic lavas—seemingly the earliest known of the rocks—were being poured out over several large sections of this country, in many places sub-aqueously—probably upon the ocean floor—that they were accompanied and followed by tuffs, slates, limestones, and the remarkable group of the banded ironstones, jaspilites, and cherts, and by quartzites, grits, and conglomerates.”
The first obstruction to knowledge is often not the world itself, but the human instrument by which the world is received.
A people who saw the sea arrive where no sea belonged would not leave behind a peer-reviewed monograph. They would leave a story. And the descendants of that story would eventually be mocked by men who mistake their own notation for reality.
If the Earth has rapidly reoriented in the past, the resulting inertial mismatch between the solid Earth and its fluid envelopes would drive high-velocity surface transport. The atmosphere, hydrosphere, and unconsolidated materials would be mobilised along coherent trajectories dictated by the rotation geometry, producing large-scale, directionally organised flow fields. These flows would imprint persistent anisotropic signatures into the geological and geomorphological record, expressed through aligned erosional features, sediment transport pathways, and coherent structural overprints.
