Dendrochronology and Young Earth
Posted: Tue Jul 10, 2012 1:32 am
Young Earthers, could you please explain to me why you do not believe in Dendrochronology?
Are there any of these methods of dating that you do believe work?
(from wiki: http://en.wikipedia.org/wiki/Dating_met ... rchaeology )
Absolute methods
Absolute dating methods rely on using some physical property of an object or sample to calculate its age. Examples are:
Radiocarbon dating - for dating organic materials
Dendrochronology - for dating trees, and objects made from wood, but also very important for calibrating radiocarbon dates
Thermoluminescence dating - for dating inorganic material including ceramics
Optically stimulated luminescence or optical dating for archaeological applications
Potassium-argon dating - for dating fossilized hominid remains
Numismatics - many coins have the date of their production written on them or their use is specified in the historical record
Archaeomagnetic dating - Clay lined fire hearths take on a magnetic moment pointing to the North Pole each time they are fired and then cool. The position of the North Pole for the last time the fire hearth was used can be determined and compared to charts of known locations and dates [1]
Magnetic Properties of Lead used to establish dates. Chemistry Professor Shimon Reich, a specialist in superconductivity, has demonstrated a method for dating artifacts based on the magnetic properties of lead, a material widely used in Israel and elsewhere in antiquity. Reich and coworkers found that at cryogenic temperatures, lead becomes a superconductor, but the corrosion products formed from centuries of exposure to air and water (lead oxide and lead carbonate) do not superconduct. On the basis of magnetic measurements and comparison with artifacts that were known (using other techniques) to be up to 2500 years old, the group showed that the mass of lead corrosion products is directly proportional to an object's age (New Journal of Physics, 2003, 5, 99)
Amino acid dating[2][3][4][5]
Obsidian hydration dating - a geochemical method of determining age in either absolute or relative terms of an artifact made of obsidian
Rehydroxylation dating- for dating ceramic materials[6]
Relative methods
Relative or indirect methods tend to use associations built from the archaeological body of knowledge. An example is seriation. Ultimately, relative dating relies on tying into absolute dating with reference to the present. One example of this is dendrochronology which uses a process of tying floating chronologies of tree rings together by cross referencing a body of work.
In practice several different dating techniques must be applied in some circumstances, thus dating evidence for much of an archaeological sequence recorded during excavation requires matching information from known absolute or some associated steps, with a careful study of stratigraphic relationships.
Age Equivalent Stratigraphic Markers
Paleomagnetism: the polarity of the Earth changes at a knowable rate. This polarity is stored within rocks; through this the rock can be dated.
Tephrochronology: volcanic ash has its own signature for each eruption. In a sedimentary sequence the associated material within the ash layer can be dated, giving a date for the eruption. If this ash is found anywhere else in the world, a date will already be known (bearing in mind transportation time).
Oxygen isotope chronostratigraphy: this is based on the climatic stages displayed in SPECMAP relating to different cold and warm stages experienced in deep time; for example, point 5.5 in the SPECMAP chronology describes the peak of the last interglacial 125,000 years ago.
Are there any of these methods of dating that you do believe work?
(from wiki: http://en.wikipedia.org/wiki/Dating_met ... rchaeology )
Absolute methods
Absolute dating methods rely on using some physical property of an object or sample to calculate its age. Examples are:
Radiocarbon dating - for dating organic materials
Dendrochronology - for dating trees, and objects made from wood, but also very important for calibrating radiocarbon dates
Thermoluminescence dating - for dating inorganic material including ceramics
Optically stimulated luminescence or optical dating for archaeological applications
Potassium-argon dating - for dating fossilized hominid remains
Numismatics - many coins have the date of their production written on them or their use is specified in the historical record
Archaeomagnetic dating - Clay lined fire hearths take on a magnetic moment pointing to the North Pole each time they are fired and then cool. The position of the North Pole for the last time the fire hearth was used can be determined and compared to charts of known locations and dates [1]
Magnetic Properties of Lead used to establish dates. Chemistry Professor Shimon Reich, a specialist in superconductivity, has demonstrated a method for dating artifacts based on the magnetic properties of lead, a material widely used in Israel and elsewhere in antiquity. Reich and coworkers found that at cryogenic temperatures, lead becomes a superconductor, but the corrosion products formed from centuries of exposure to air and water (lead oxide and lead carbonate) do not superconduct. On the basis of magnetic measurements and comparison with artifacts that were known (using other techniques) to be up to 2500 years old, the group showed that the mass of lead corrosion products is directly proportional to an object's age (New Journal of Physics, 2003, 5, 99)
Amino acid dating[2][3][4][5]
Obsidian hydration dating - a geochemical method of determining age in either absolute or relative terms of an artifact made of obsidian
Rehydroxylation dating- for dating ceramic materials[6]
Relative methods
Relative or indirect methods tend to use associations built from the archaeological body of knowledge. An example is seriation. Ultimately, relative dating relies on tying into absolute dating with reference to the present. One example of this is dendrochronology which uses a process of tying floating chronologies of tree rings together by cross referencing a body of work.
In practice several different dating techniques must be applied in some circumstances, thus dating evidence for much of an archaeological sequence recorded during excavation requires matching information from known absolute or some associated steps, with a careful study of stratigraphic relationships.
Age Equivalent Stratigraphic Markers
Paleomagnetism: the polarity of the Earth changes at a knowable rate. This polarity is stored within rocks; through this the rock can be dated.
Tephrochronology: volcanic ash has its own signature for each eruption. In a sedimentary sequence the associated material within the ash layer can be dated, giving a date for the eruption. If this ash is found anywhere else in the world, a date will already be known (bearing in mind transportation time).
Oxygen isotope chronostratigraphy: this is based on the climatic stages displayed in SPECMAP relating to different cold and warm stages experienced in deep time; for example, point 5.5 in the SPECMAP chronology describes the peak of the last interglacial 125,000 years ago.