Woody wrote:It [The Urantia Book] indicates that Earth is right at 1 billion years old.
Not to pick on you Woody, really, but that is not factually correct. The Urantia Book, in describing the origin of our solar system, states the following:
Urantia Book wrote:4,500,000,000 years ago the enormous Angona system began its approach to the neighborhood of this solitary sun. The center of this great system was a dark giant of space, solid, highly charged, and possessing tremendous gravity pull. (655.9)
Scientists have long since determined the age of the earth based on studying our solar system, for the age of our solar system and the earth are the same. So, per the internal dating of the papers (1934/35) of the Urantia Book the earth is said to be 4.5 billion years old. Of course, the Urantia Book was published in 1955, so this would be the conservative date to use for when it made this claim that the earth is 4.5 billion years old.
Alfred Noyes wrote:These rocks, these bones, these fossil ferns, and shells, shall yet be touched with beauty and reveal the secrets of the book of earth to humans.
-- Alfred Noyes, 1925
All of this story is graphically told within the fossil pages of the vast "stone book" of world record. And the pages of this gigantic biogeologic record unfailingly tell the truth if you but acquire skill in their interpretation. Many of these ancient sea beds are now elevated high upon land, and their deposits of age upon age tell the story of the life struggles of those early days. It is literally true, as your poet has said, "The dust we tread upon was once alive."
-- The Urantia Book p., 671.5
The dating of the earth is intimately tied to the dating of our solar system, for our earth was created at the same time and from the same mass as our solar system. The history of how science determined the age of the earth makes for an interesting story. Based on different methods scientists have proposed ages for the earth ranging from a few m.y. old to 8,000 m.y. old. For example, in 1921 H. N. Russell proposed an upper and lower age for the earth of between 2,000 - 8,000 m.y. old based on the decay of U to Pb in the crust. In 1927 in his book <i>The Age of the Earth: An Introduction to Geological Ideas</i>, Homes revised Russell's calculation and came up with an age of just over 3,000 m.y. for the earth. Around the period of the 1930s, we can see, the question of the age of the earth was a work in progress so to say.
Much that we know about the origin and evolution of our solar system and the age of the earth was learned by studying the rock samples brought back from the moon or meteorites. The reason these source are important is because they are not subject to the same tectonic forces that have churned the surface of the earth to the point that the oldest rocks going back to the origin have long since been lost. Since the moon and meteorites are not subject to these forces, they are more accurate measures of the origin of our solar system, and hence the age of the earth too. Scientists from all over the world have studied these rocks; it was the dating of these rocks that largely confirmed the 4.5 Ga (billion) age of the earth that the Urantia Book gives for the age of the earth.
It is my assessment that the age of the earth would be considered known information as of the 1953 date below, despite the fact that scientists were still debating the issue and working out the exact methods that would give them the most reliable approximation for the age of the earth during the 1930s and 1940s. The scientist/historian Steven G. Brush shows in Transmuted Past when the number of 4.5 m.y. was formally established as the most reliable estimate and made public.
While reading Transmuted Past, by Stephen G. Brush (1996), I came across the following on page 82:
Brush wrote:
Although some scientists pointed out that the available data did not exclude a value for the age of the Earth as high as 5000 m.y. the Holmes-Houtermans value of 3000 to 3400 m.y. was generally accepted until 1953. In that year a group of scientists at the University of Chicago and the California Institute of Technology reported that the abundances of the radiogenic lead isotopes in some meteoritic material were significantly lower than the figures previously considered "primeval" in estimating the age of the Earth. The ratio for the four isotopes was found to be 1 : 9.4 : 10.3 : 29.2. Moreover, the ratio of uranium to lead in these meteorites was extremely low, so little if any of the present abundance of 206Pb and 207Pb could be attributed to decay or uranium since the formation of the meteorite. It seemed reasonable to suppose that this material was much less affected by chemical differentiation processes than minerals found in the Earth's crust, so that these values were the most appropriate ones to use for the abundances at the time of formation of the Earth.
Results based on these data were announced in September 1953 by C. C. Patterson (1953): The minimum age of the Earth is "about 4.5 billion years and is probably somewhat older." Friedrich Houtermans (1953) published a similar result based on the same data soon after:
Age of the Earth = 4500 +- 300 m.y.
By 1956 Patterson thought enough data were available to clinch the argument for the 4500 m.y. age. (Brush 1996, vol 2: 82-3)
In footnote 33 on page 82, Brush states:
Patterson's original publication appeared in a volume that was not widely available and hence is either not cited at all or cited in a rather confusing way by later workers. The abstract of a paper presented by Patterson, Tilton, and Inghram at the GSA meeting in Toronto, November 9-11, 1953, mentions ages "greater than 4 billion years" (Patterson et al. 1953b); the headline of a report in Chemical and Engineering News (1953) boldly asserts: "Earth's age: 4.6 Billion Years."
Dalrymple wrote:
[T]he oldest well-studied rocks on Earth are metamorphosed supracrustal rocks that are intruded and enveloped by only slightly younger granitoids. The oldest of these are found at Isua in western Greenland, where two sedimentary units and a mafic intrusive body have been dated ... at 3.7—3.8 Ga….
It is known from other evidence to be discussed that the Earth's age is most probably between 4.5 and 4.6 Ga, yet the oldest rocks found on Earth are only about 3.8—3.9 Ga. What happened to the rocks that represent the first two-thirds to three-fourths of a billion years of Earth's history? The answer to this question is not really known—there are only speculations and possibilities. One possibility is that during that period of Earth’s history not only was the first continental crust forming, it was also being vigorously recycled and regenerated. Thus, the earliest crustal rocks may have been consumed by recycling into the primitive mantle almost as fast as they were generated. A second possibility arises from the observation that the Moon and, by inference, the Earth were subjected to intense bombardment by large meteorites from the time of their initial formation to about 3.8 Ga. This bombardment occurred because the planets were still sweeping up huge masses of material from their orbital paths. Perhaps the bombardment was sufficiently intense to obliterate the first crustal rocks. A third possibility is that the record of the Earth’s early history exists somewhere but has not been found. The discovery of zircon grains 4.0—4.3 Ga old in sedimentary rocks from Earth’s earliest history may yet be discovered. The correct reason for the absence of the most ancient rocks may well be some combination of the above.
The absence of known rocks that represent the first two-thirds to three- fourths of a billion years of Earth’s history is probably due to destruction owing to vigorous crustal recycling, intense meteoritic bombardment, lack of discovery, or some combination thereof. But whatever the reason for the missing record on Earth may be, we can learn much about the history and age of the Earth by examining the evidence from more primitive bodies in the Solar System, in particular the Moon and meteorites. (Dalrymple 1991: 190-192)
Definite volcanic action dates from these times. The internal heat of the earth continued to be augmented by the deeper and deeper burial of the radioactive or heavier elements brought in from space by the meteors. The study of these radioactive elements will reveal that Urantia is more than one billion years old on its surface. The radium clock is your most reliable timepiece for making scientific estimates of the age of the planet, but all such estimates are too short because the radioactive materials open to your scrutiny are all derived from the earth's surface and hence represent Urantia's comparatively recent acquirements of these elements. (Urantia Book 659: 2)
This entire age was characterized by frequent and violent storms. The early crust of the earth was in a state of continual flux. Surface cooling alternated with immense lava flows. Nowhere can there be found on the surface of the world anything of this original planetary crust. It has all been mixed up too many times with extruding lavas of deep origins and admixed with subsequent deposits of the early world-wide ocean. (Urantia Book 661: 5)
The trips to the Moon by the Apollo astronauts were surely the greatest feats of engineering and exploration in the history of humankind. In addition to their technical and spiritual benefits, the manned lunar missions had significant scientific worth, for they gave scientists, for the first time, an exciting opportunity to study rock samples collected from another planet. (Dalrymple 1991: 193)
One of the most significant scientific benefits of the Apollo program was the return of samples of rock and soil for study by Earth-bound scientists. Nine missions, six from the United States and three from the USSR, returned a total of nearly 382 kg of samples. This priceless material consists of crystalline rocks, breccias, and soil, the later in the form of both scooped samples and cores, from a variety of geological environments. (Dalrymple 1991: 212)
Moon rocks are not exactly like Earth rocks and much has been made of the differences. Although these differences are important, the overall similarity of Earth and Moon rocks is equally worthy of note. Contrary to the impression conveyed by many pre-Apollo films and television series, there are no totally new or weird types of rocks in the lunar sample collection. The lunar rocks include both crystalline igneous rocks and impact breccias. Virtually all of the lunar rock types have their terrestrial analogs, albeit not necessarily in the same abundances. (Dalrymple 1991: 213)
The radiometric data, including both rock and model ages, show clearly that the moon is at least 4.5 Ga in age. (Dalrymple 1991: 256)
Actually, friends, I am no expert. I am just a student who enjoys learning along the Paradise journey. McCullock, I am not ignoring your fair and thoughtful questions. They deserve a thoughtful answer, and today is my daughter's birthday, and I am afraid that takes precedence over your questions, so please be patient with me. The only reason I was able to answer this question was because the material was readily available from a two year study I just completed on the history of the idea of continental drirft proposed by Alfred Wegener in 1924.
Also, I cannot communicate with any of the pms and have questions before I start posting regularly which I need answered. And, I don't even know which thead to answer you in, for I want to abide by the rules of this forum, and that is not the topic of this thread, which is the "Age of the Earth." At this time the threads dealing with these questions look more like "discussion" threads rather than topical-debates (in the best and most honorable sense of the word).
Peace,
Rob
Some excellent sources for this study regarding the question of the age of the earth and how it was determined, see:
Dalymple, Brent G. (1994) The Age of the Earth. Stanford University Press.
Brush, Stephen G. (1996) A History of Modern Planetary Physics. Vol. 1-3. Transmuted Past: The Age of the Earth and the Evolution of the Elements from Lyell to Patterson. Vol. 2. Cambridge: Cambridge University Press.
Lewis, Cherry (2000) The Dating Game: One Man's Search for the Age of the Earth. Cambridge University Press.
Burchfield, Joe D. (1990) Lord Kelvin and the Age of the Earth. University of Chicago Press.