Provide evidence for a same state past. Scientific
Well I'll be delighted to dad. Below I will describe through three independent methods how we know the past has been he same.
You see all the evidence is at least as much mine once we stop coloring and tainting it with your beliefs.
What I provide is physical evidence based on the laws of nature. What you have suggested is a made up fantasy world. You are the only one doing coloring and tainting.
1. Decay rates:
a. When a radionuclided decays it emits energy, therefore heat. For decay rates to have been higher in the past to yield the ages we get with rocks millions or billions of years of age in only 4,300 years (since the flood), the earth would have become completely molten. Thus absolutely no life could have existed before the flood.
b. In chain decays, for example the uranium series, goes through 18 separate decays before becoming stable as lead. Each of these separate decays forms a different isotope with a completely different decay rate. Thus, any rocks formed before said flood with said accelerated decay rate would show different ratios between each of those 18 isotopes than those formed after said flood. All rocks formed before and after said flood (said change of physics) would show different ratios in the decay chains. And uranium is not the only decay chain, there are others and there are no decay ratio changes.
2. Measured decay rates from supernova:
a. SN1987A is 168,000 light years distant, or if you prefer, 51.4 kiloparsecs distant. One parsec is 19 trillion miles. So we not only have time, but measured distance as well. Gamma rays emitted from SN198A for isotope decay for several radionuclides measured showed that those decay rates of those isotopes are the same which were generated 168,000 years ago are the same as we measure on earth today.
b. SN1987B - same scenario.
3. Ice core chronology:
a. Ice cores have been dated on the Greenland ice cap upwards to 100,000 years. Cores in Antarctica date to 800,000 years.
b. Ice core chronology dates annual layers, which are easily distinguishable from multiple seasonal snowfalls.
c. There are numerous different (independent) proxies that can be used to not only distinguish annual layers, but seasons within as well. Some of these are heavy stable isotope ratios, acidity, pollen, Sodium and Chloride ions, ammonium, Lead, Sulphates, Nitrates.
