@Patty phil,
Xris, it is all a wondrous, sublime, fascinating thing.
But as Khetil says, the amount of time, energy, and mass of substrate is impossible for us to conceptualize.
If you're familiar with organic chemistry, this will be routine stuff, but just think about how easy it is to get organic molecules from elemental materials. Organic molecules are defined by carbon and hydrogen, but commonly include phosphorus, oxygen, nitrogen, and sulfur.
The early earth had H2O, water, at some point, which was the major source of both hydrogen and oxygen (an electrons to donate to covalent bonds). CO2 (carbon dioxide), PO4 (phosphate), SO4 (sulfate), NH4 (ammonia), NO2 (nitrate), H2 (elemental hydrogen), O2 (elemental oxygen), etc, were all probably abundant since the formation of the planet.
It would not take much energy to catalyze the production of very simple organic molecules like CH4 (methane), H3COH (methanol), H2C=O (formaldehyde), H3C-CH3 (ethane), etc.
What do you get if you put together a string of methanes, CH3-CH2-CH2-CH2OH, for instance -- that's a fatty acid.
The longer your chain of fatty acids, the more hydrophobic it gets. These form micelles, or globules of fat. A phospholipid is three fatty acid chains attached to a glycerol backbone (a simple 3-carbon sugar), and phospholipids form
bilayers -- a hydrophobic layer that is hydrophillic on both the outside and inside, so it can contain water inside. That is the basic structure of a cell.
The simplest amino acid, alanine, is 3HN-CH2-COOH. It's a simple two carbon molecule. There are hundreds of naturally occurring amino acids, it just happens that 20 of them can be genetically encoded.
Nucleic acids are not much more complicated.
These things are not hard to imagine arising even in routine experimental conditions. The development of things like a self-replicating genome, catalytic proteins (enzymes), regulatory mechanisms, etc, is something much more complicated, but hey, there was a lot of time and the building blocks were already there.