Arctic Ocean, below, has been losing ice in the last decade:
The Arctic's in the news because of Global Warming; we'll now invoke the Texas Kiki bird- who says KiKirist, it's cold up here!
Sullivan Knoll is enlarged above for a determination whether it now rotates CW Clockwise upon cooling and shrinking. It formed after the 1 m.y. Ivin Knoll to the south, and by quartering would have erupted 250,000 years ago. Notice that there is a younger vent on the SW side- which should be of 62,500 years age.
Ayers Rock, Uluru, below is a reference near the center of the continent:
Files are voluminous, and I'll find the Uluru closeup yet.
I need the top view on Google Earth, not the one below:
Striations are NW-SE, 315 compass degrees, indicating a Transition to our Moon being locked in:
Speculation is that Coriolis Force was masked by the Faster Rotation of Earth before the Moon capture slowed both bodies, and the Equatorial bulge was Larger than now; age was 4,096 billion years. Search literature, for other speculations.Far side of our Moon has many Asteroid craters, compared to close side (with Eruptions caused by Tug of the Earth); before- it was "locked gravitationally" at speculated 4.096 billion years
Australia has few quakes (except at the edges), it has no arcuate features, and is ideal for a study of Coriolis Force influence, shown in the atmosphere below:
We will search for arcs, fractures, rotating features on Google Earth, and any indications that this oldest continent has pre-empted Coriolis influence, other than that producing Stability of the 4 billion+ years craton.
Searching my other "Sticks", I find more evaluations of the craton:
Above should be updated.
Interior of the outback shows playa basins- long since dried^.
Antarciica's Active Mt. Erebus is near 144 south of Canada's Craton (16,000 km along a meridian), and due to 2D presentation on Google Earth, it angles off with Distance.
Mt Erebus relative to the 16,000 km from Canada 60N latitude, above.
LaGrange equilateral triangle ET has 60 degree positions between green Asteeoids, controlled by Jupiter's gravitational attraction, and this speculated to influence Iceland's volcanodiscovery.com
Google Earth measurement of Bardurbunga 1500 km from last westward MAR ridge, above. Estimating 20 mm/year rate yields 75 million years traverse for this Mid Atlantic Ridge part.
Larger view of the Iceland forerunner of 1500 to 1600 km to Bardurbunga, above.
Ridges below the Iceland Bardurbunga eruption, in black, are lined in red, above.
Bardurbunga location in a Polygon, above.
Soiuth Africa is a semi-craton, halfway to Larger at Antarctica, above.
Moon over anomalous Sutter Buttes, above.
Moon- side facing Earth- blue area is that attracted since capture:
Continent unexplored has active Erebus and other Volcanoes under the ice:
Antarctica size, above.
Trial and Error from previous analyses must be updated:
Compare Canada's Craton with older Australia's, above, and the Later literature Sequence below:
Active Erebus, Antarctica is a Reference for this fairly stable Continent:
Antarctica is almost stable, except for a jut into the South Georgia-Shetlands archipeligo Reverse Tides to the East, below:
We must reference Location, Time, and characteristic, as shown for India's Deccan 40 m.y. basalts; it is similar in age to Chixculub- a supposed asteroid strike at Yucatan, Mexico:
Reverse Tides at 64 m.y. place Chixculub at the Deccan Traps, above, and these are a quartering Reference fron 16 m.y. Columbia Flood basalts and 256 Siberia traps, above.
Reef offshore Yucatan, Mexico- which may be a rebound from an asteroid Strike:
Reef is shown below enlarged:
Yucatan coordinates and large view. above.
No matter how old you are, family history is important. While you might not think so at the time, as you get older there will be things you and your grandchildren will want to know. Most of us don't realise it until the older generations are gone and you can't replace first hand comments. Don't just put in about the good times, add in the harder times and how you overcame those trials. Another thing to remember is what caused the deaths of those you loved. There are many things that have been found to continue into future generations that knowing it runs in the family can be helped with now or possible in the future. prevention starts with knowing where to start. I wish someone had taken the time to write these things down for mew to be able to go back to. My Grandmother and my mother told us many stories of what things happened in their lives and about the people in their lives. I now wish someone had written those things down since both have passed now. But I never thought at that busy point in my life that I would one day want to remember all those things. So much family history is lost when the older generations are gone. Please pass it on to your family while you can. You can even just do it digitally so it can be accessed by family later on.Family pictures are something to cherish also. Just be sure to write down who is pictured in them, where they are taken and when. I have found family pictures that no one now even knows who is in them.
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