starbiter wrote:Hello Mungo: It sounds like the sea sloshed over the island at the end of the process. If WiC is correct, the top layers of Malta should be comet dust, volcanic ash, and Earth dust, interspersed with the debris left behind after the Mediterranean sloshed over the island. Probably repeatedly. Sea level would have been reduced during the process, and possibly higher also.
The Sun was reported to reverse it's course during the first encounter with Mars. So sloshing was an option 700 years after Athena. The creatures in the caves you speak of could be associated with these later events.
Hope to see you in the desert, michael


Update: Village Blazes Again
Jeremy Charles for The Mirror
March 18, 2004
A village hit by a series of mystery fires was in flames again yesterday, leaving experts more baffled than ever. The phenomenon began two months ago as fridges, washing machines and cookers all burst into flames for no reason.
Locals were evacuated amid calls for an exorcism but experts put the fires down to electrostatic interference from power pylons.
But just a month later, as villagers were moving back to Canneto di Caronia, near Messina, Sicily, fires have started again. Disconnected fuse boxes have burst into flames, car central locking systems blocked up and mobile phones have caught fire.
Yesterday mayor Pedro Spinnato said: "Yes, it's started all over again. Now we are back to where we started."
Last night experts, surveyors and engineers were probing the mystery.
Electric polarization induced by mechanical loading of Solnhofen limestone
http://www.informaworld.com/smpp/conten ... order=page
Abstract
Electromagnetic radiation was detected while loading a sample of Solnhofen limestone, which is not a piezoelectric material. The sample was subjected to mixed tensile and shear loading. The signals observed are associated with a fall-off in electric polarization induced by the loading, and represent the second time derivative of the polarization. The polarization is ascribed to the complicated type of loading, leading to the existence of a chosen direction, which makes polarization possible.
So the ingredients in the upper layers of Malta are available in comet dust. How convenient.
MrAmsterdam wrote:Hello all,
While searching for piezoelectric properties of limestone I came across the following website;
http://www.humanresonance.org/messina.html
If any of these stories can be confirmed youll have a couple of other clues that seem to point to electric phenomena.Update: Village Blazes Again
Jeremy Charles for The Mirror
March 18, 2004
A village hit by a series of mystery fires was in flames again yesterday, leaving experts more baffled than ever. The phenomenon began two months ago as fridges, washing machines and cookers all burst into flames for no reason.
Locals were evacuated amid calls for an exorcism but experts put the fires down to electrostatic interference from power pylons.
But just a month later, as villagers were moving back to Canneto di Caronia, near Messina, Sicily, fires have started again. Disconnected fuse boxes have burst into flames, car central locking systems blocked up and mobile phones have caught fire.
Yesterday mayor Pedro Spinnato said: "Yes, it's started all over again. Now we are back to where we started."
Last night experts, surveyors and engineers were probing the mystery.
Matt, maybe you can ask arround if any person saw simular stuff like this. Maybe they have mysterious fires too...
---
And now something completely different;Electric polarization induced by mechanical loading of Solnhofen limestone
http://www.informaworld.com/smpp/conten ... order=page
Abstract
Electromagnetic radiation was detected while loading a sample of Solnhofen limestone, which is not a piezoelectric material. The sample was subjected to mixed tensile and shear loading. The signals observed are associated with a fall-off in electric polarization induced by the loading, and represent the second time derivative of the polarization. The polarization is ascribed to the complicated type of loading, leading to the existence of a chosen direction, which makes polarization possible.
Starbiter was mentioning the following ;So the ingredients in the upper layers of Malta are available in comet dust. How convenient.
....the lines found on pembrokes rolling hill appear to have large crystals in them (The end of the lines for Geology?). i have only seen inside 1 of them because they are rock hard and look as fresh as if they were newly made or being renewed.
Chemical Precipitates:
This is the general term for rocks originating from the precipitation of the substances under saturated solutions. Of these, the most abundant by far are the limestones, which are rocks constituted almost wholly by calcite.
Some limestones can form by direct precipitation of calcium carbonate from marine or fresh water. Limestones formed this way are chemical sedimentary rocks. They are thought to be less abundant than biological limestones.
Chert is a microcrystalline or cryptocrystalline sedimentary rock material composed of silicon dioxide (SiO2). It occurs as nodules, concretionary masses and as layered deposits
How Does Chert Form?
Diatoms are microscopic, single-celled algae that live in marine or fresh water. They produce hard parts made of silicon dioxide. NASA Image.
Most chert forms when microcrystals of silicon dioxide grow within soft sediments that will become limestone or chalk. In these sediments, enormous numbers of silicon dioxide microcrystals grow into irregularly-shaped nodules or concretions as dissolved silica is transported to the formation site by the movement of ground water. If the nodules or concretions are numerous they can enlarge and merge with one another to form a nearly continuous layer of chert within the sediment mass. Chert formed in this manner is a chemical sedimentary rock.
Chert (pronounced /ˈtʃɜrt/) is a fine-grained silica-rich microcrystalline, cryptocrystalline or microfibrous sedimentary rock that may contain small fossils. It varies greatly in color (from white to black), but most often manifests as gray, brown, grayish brown and light green to rusty red; its color is an expression of trace elements present in the rock, and both red and green are most often related to traces of iron (in its oxidized and reduced forms respectively).
Chert occurs mainly in three forms: bedded sequences, nodular, and massive. Bedded chert (called ribbon chert if beds show pinch-and-swell structure) consists of rhythmically interlayered beds of chert and shale; chert and carbonates; or in some pre-Phanerozoic formations, alternations of chert and siderite or hematite. Bedded sequences can be hundreds of feet thick stratigraphically and cover areas of hundreds of square miles. Individual beds are commonly (1–20 cm) thick. Chert nodules and lenses occur primarily in chalk, limstone, and dolomite.
The chemical process for chert formation sounds quite similar to what I have observed in eastern Washington in the formation of opal lenses in diatomaceous earth beds sandwiched between basalt lava flows.
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