1.Efflux of Helium-4 into the atmosphere1,750 - 175,000 years12.Influx of meteoritic dust from spacetoo small to calculate13.Influx of radiocarbon to the earth system5,000 - 10,000 years14.Development of total human populationless than 4,000 years15.Influx of uranium to the ocean via rivers10,000 - 100,000 years16.Influx of sodium to the ocean via rivers260,000,000 years17.Influx of nickel to the ocean via rivers9,000 years18.Influx of magnesium to the ocean via rivers45,000,000 years19.Influx of silicon to the ocean via rivers8,000 years110.Influx of potassium to the ocean via rivers11,000,000 years111.Influx of copper to the ocean via rivers50,000 years 112.Influx of gold to the ocean via rivers560,000 years113.Influx of silver to the ocean via rivers2,100,000 years114.Influx of mercury to the ocean via rivers42,000 years115.Influx of lead to the ocean via rivers2,000 years116.Influx of tin to the ocean via rivers100,000 years117.Influx of aluminum to the ocean via rivers100 years118.Influx of carbonate to the ocean via rivers100,000 years219.Influx of sulphate to the ocean via rivers10,000,000 years 220.Influx of chlorine to the ocean via rivers164,000,000 years221.Influx of calcium to the ocean via rivers1,000,000 years222.Leaching of sodium from continents32,000,000 years223.Leaching of chlorine from continents1,000,000 years 224.Leaching of calcium from continents12,000,000 years225.Influx of sediment to the ocean via rivers30,000,000 years326.Erosion of sediment from continents14,000,000 years327.Decay of earth's magnetic field10,000 years428.Efflux of oil from traps by fluid pressure10,000 - 100,000 years529.Formation of radiogenic lead by neutron capturetoo small to measure530.Formation of radiogenic strontium by neutron capturetoo small to measure531.Decay of natural remanent paleomagnetism100,000 years532.Decay of C- 14 in pre-Cambrian wood4,000 years533.Decay of uranium with initial leadtoo small to measure634.Decay of potassium with entrapped argontoo small to measure635.Influx of juvenile water to oceans340,000,000 years736.Influx of magma from mantle to form crust500,000,000 years737.Growth of active coral reefs10,000 years738.Growth of oldest living part of biosphere5,000 years739.Origin of human civilizations5,000 years740.Formation of river deltas5,000 years841.Submarine oil seepage into oceans50,000,000 years942.Decay of natural plutonium80,000,000 years1043.Decay of lines of galaxies10,000,000 years1144.Expanding interstellar gas60,000,000 years1245.Formation of Carbon 14 on meteorites100,000 years1346.Decay of short-period comets10,000 years1447.Decay of long-period comets1,000,000 years1548.Influx of small particles to the sun83,000 years1549.Maximum life of meteor showers5,000,000 years1550.Accumulation of dust on the moon200,000 years1551.Deceleration of earth by tidal friction500,000,000 years1652.Cooling of earth by heat efflux24,000,000 years1653.Accumulation of calcareous ooze on sea floor5,000,000 years1754.Influx of lithium into ocean via rivers20,000,000 years1855.Influx of titanium into ocean via rivers160 years1856.Influx of chromium into ocean via rivers350 years1857.Influx of manganese into ocean via rivers1,400 years1858.Influx of iron into ocean via rivers140 years1859.Influx of cobalt into ocean via rivers18,000 years1860.Influx of zinc into ocean via rivers180,000 years1861.Influx of rubidium into ocean via rivers270,000 years1862.Influx of strontium into ocean via rivers19,000,000 years1863.Influx of bismuth into ocean via rivers45,000 years1864.Influx of thorium into ocean via rivers350 years1865.Influx of antimony into ocean via rivers350,000 years1866.Influx of tungsten into ocean via rivers1,000 years1867.Influx of barium into ocean via rivers84,000 years1868.Influx of molybdenum into ocean via rivers500,000 years1869.Influx of bicarbonate into ocean via rivers700,000 years1970.Escape of high-velocity stars from globular clusters40,000 years2071.Rotation of spiral galaxies200,000,000 years2072.Accumulation of peat in peat bogs8,000 years2173.Accumulation of sediments for sedimentary rocks20,000 years2174.Lithification of sediments to form sedimentary rocks20,000 years2175.Instability of rings of Saturn1,000,000 years1576.Escape of methane from Titan20,000,000 years15
Here are some more possible indications for a young earth it is all I had a chance to do today. When you consider this is only one list of many, even if 50% could be ruled out then the volume of what's left would at the very least justify an open mind to the possability. Try present-truth.org/3truth.org/3-Nature/Evolution for some of the explanations you asked about. I hope that address works. I still can't post links but hopefully that will get you close.
Talk at you later,