I would like to exam your evidence from science (if you have any) that proves the uniformitarian assumption that millions of varves represent millions of years. Do you have such evidence?
No assumptions there. Initially, it was thought that they were some kind of weird rhythmites or other kind of laminae. Only after considerable investigation did it become clear that they were seasonal laminae that showed two alternating layers per year.
During fieldwork in 1878, De Geer noticed that the appearance of laminated sediments deposited in glacial lakes at the margin of the retreating Scandinavian ice sheet at the end of the last ice age, closely resembled tree-rings. In his best known work Geochronologia Sueccia, published in 1940, De Geer wrote "From the obvious similarity with the regular, annual rings of the trees I got at once the impression that both ought to be annual deposits" (1940, p.13).
While this observation was not new, De Geer was the first geologist to exploit its potential application. De Geer called these annual sedimentary layers varves and throughout the 1880s further developed his theory, publishing a brief outline of his discovery in 1882, which he followed with a presentation to the Swedish Geological Society in 1884. It was not until 1910, at the International Geological Congress, that De Geer's pioneering work reached the wider international scientific community.
Wikipedia
While varves were not useful for worldwide climate correlations as De Geer had hoped, they are useful in that they can provide tens of thousands of years of data, which can be accurately dated by counting varves.
Glenn Morton, citing Richard Flint's work:
A rhythmite deposited in a lake near Interlaken in Switzerland consists of thin couplets each containing a light-colored layer rich in calcium carbonate and a dark layer rich in organic matter. Proof that the couplets are annual, and therefore varves, is established on organic evidence, first recognized by varves, is established on organic evidence, first recognized by Heer(1865). The sediment contains pollen grains, whose number per unit volume of sediment varies cyclically being greatest in the upper parts of the dark layers. The pollen grains of various the upper parts of the dark layers. The pollen grains of various genera are stratified systematically according to the season of blooming. Finally, diatoms are twice as abundant in the light-colored layers as in the dark. From this evidence it is concluded that the light layers represent summer seasons and the dark ones fall, winter and spring. Counts of the layers indicate a record that is valid through at least the last 7,000 years B. P. Richard Foster Flint,
Glacial and Quaternary Geology, New York: John Wiley and Sons, Inc., 1971, p. 400.
Another careful analysis of varves extends the data much farther:
Lake Suigetsu is located near the coast of the Sea of Japan (35°35'N, 135°53'E). The lake is 10 km around the perimeter and covers 4.3 km2. It is a typical kettle-type lake, nearly flat at the center, Ca. 34 m deep. A 75-m-long continuous core (Lab code = SG) and four short piston cores (Lab codes = 501, -2, -3 and -4) were taken from the center of the lake before 1993 (Kitagawa et al. 1995).
The sediments are characterized by dark-colored clay with white layers due to spring season diatom growth. The seasonal changes in the depositions are preserved in the clay as thin, sub-millimeter scale laminations or "varves". Based on observation of varve thickness change, we expect that the annually laminated sediment records the paleoenvironmental changes during the past 100 ka. This sequence of annually laminated sediments not only forms a unique continuous paleoenvironmental record after the last interglacial but also permits us to reconstruct a complete 14C calibration extending back to at least 40 ka BP, and probably even more by means of combined isotope enrichment and AMS 14C dating (Kitagawa and van der Plicht 1997). We have performed AMS 14C measurements on >250 terrestrial macrofossil samples of the annual laminated sediments from Lake Suigetsu. Here, we report varve and 14C chronologies of these sediments. The combined varve and 14C chronologies back to 40,000 BP are used to reconstruct a 14C calibration curve for the total range of the 14C dating method.
HIROYUKI KITAGAWAI and JOHANNES VAN DER PLICHT2
Proceedings of the 16th International 14C Conference, edited by W. G. Mook and J. van der Plicht
RADIOCARBON, Vol. 40, No. 1, 1998, P. 505-515