I'm sure a science buff can help me out with some theories on this one. Aplologies if this seems like a stupid question, but was it always just.....there?

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4 billion years ago, the Earth could be described as a very large, hot rock without a trace of water on its surface. Water on the young Earth came from two sources, outgassing from within the Earth and bombardment by comets. Outgassing is the process whereby gases are released from molten rock in the mantle of the planet by volcanic activity. This was probably the primary source of gases for the early atmosphere. Comets and meterorites also bring with them gases which contributed to the Earth's atmosphere.
Some of the gases in the new atmosphere were methane (CH3), ammonia (NH3), water vapor (H2O), and carbon dioxide (CO2). The water on Earth stayed in gaseous form until the planet's surface cooled below 100 degrees Celsius. At this time, 3.8 billion years ago, water condensed into rain and poured onto the land. Water collected in low lying areas which gradually became the primitive oceans.
As water entered the oceans from the atmosphere, it brought with it dissolved gasses released from the mantle by volcanoes and geysers. Water also flowed as runoff from the land, bringing in dissolved minerals from the rocks on the surface. These minerals include the salts which make seawater taste salty.
watched a doco on foxtel on how the earth was created and from memory the theory was......
the earth was originally molten rock (or something like that) and as it cooled over billions of years it produced gases the gases rose but couldn't escape the earths atmohere (due to gravity??), as these gases built up chemical reaction created hydogen and oxygen (then formed water particles it then began to rain and did so for for millions of years ie as it rained it cooled the moten quicker which produced steam which is term created more rain. as mentioned this cycle continued for millions of years until the earths crust was cooled, and the water settled where erosion and tatonic (sp?) plates had shifted creating oceans and from the oceans single cells microisms formed and from there life was created.
that was a very laymans description and im not sure if i even got it right
Accurate enough.
The asteroid theory seems right.
Assuming the oxygen formed in the rocks, not in the atmosphere...?
http://www.ux1.eiu.edu/~cfjps/1400/atmos_origin.htmlAddition of O2 to the Atmosphere
Today, the atmosphere is ~21% free oxygen. How did oxygen reach these levels in the atmosphere? Revisit the oxygen cycle:
Throughout the Archean there was little to no free oxygen in the atmosphere (<1% of presence levels). What little was produced by cyanobacteria, was probably consumed by the weathering process. Once rocks at the surface were sufficiently oxidized, more oxygen could remain free in the atmosphere. During the Proterozoic the amount of free O2 in the atmosphere rose from 1 - 10 %. Most of this was released by cyanobacteria, which increase in abundance in the fossil record 2.3 Ga. Present levels of O2 were probably not achieved until ~400 Ma.
- Oxygen Production
- Photochemical dissociation - breakup of water molecules by ultraviolet
- Produced O2 levels approx. 1-2% current levels
- At these levels O3 (Ozone) can form to shield Earth surface from UV
- Photosynthesis - CO2 + H2O + sunlight = organic compounds + O2 - produced by cyanobacteria, and eventually higher plants - supplied the rest of O2 to atmosphere. Thus plant populations
- Oxygen Consumers
- Chemical Weathering - through oxidation of surface materials (early consumer)
- Animal Respiration (much later)
- Burning of Fossil Fuels (much, much later)
The asteroid theory seems right.
But quite far in the future, the ocean will start boiling and then it will evaporate completely.
Asteroids could have only contributed a very small amount of water after formation of the earth as could comets, however technically a large proportion of the accreted matter which formed the earth could be considered to be asteroids so it just depends on you view point.About the time the earth was formed, the sun became large enough that the fusion reactions in the sun ignited. This didn't happen smoothly, but likely in sputtering way for a while. Each flaring up of the sun sent streams of particles sweeping out. If the earth had an atmosphere at this time, it would have been blown off leaving the earth as a rock with neither air or water on its surface. In fact, after the sun stabilized, the earth went through a process of releasing gases from its interior in a process called degassing. Over a relatively short time, something like a 100 million years, enough material had been released to form the oceans and to give the earth an atmosphere. There was no free oxygen in the atmosphere at this time, but it was a collection of gases, largely ammonia, methane and carbon dioxide, held to the earth by gravitational attraction. Fortunately, early in its history, the temperature of the earth dropped below 212 degrees Fahrenheit, and the water condensed into the oceans we know today. In fact, the mass of water present in the oceans, now about 10(24) grams, is about the same as the mass of water that was contained in the crust when the degassing process started.
Strangely enough Oxygen (O2) only appeared in any quantity after Water (H2O).
Until the explosion of plant life.