The fate of the Earth?
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From: oriel36 on 6 Oct 2009 17:16 On Oct 6, 9:04 pm, Sam Wormley <sworml...(a)mchsi.com> wrote: > oriel36 wrote: > > > At an elevation of 1 km,roughly .6 km below Denver's elevation ,an > > observer with an unrestricted view can see across a distance of 112 km > > to the horizon allowing for any minor variations such as refraction > > ect .This 112 km value represents the equivalent of 1 degree latitude > > so that the total distance the observer can see across a North/South > > longitude meridian is 2 degrees of Latitude. > > Don't want to tax your brain too hard, Gerald, but a geosynchronous > satellite can "see" Denver and a location on the equator simultaneously > and the two locations have NO relative motion. Beneath the fractured crust is a vast ocean constructed of a rotating viscous composition and when it appears through the fissures and volcanoes on the surface,it is spectacular - http://www.youtube.com/watch?v=jXDyUi6PKjs&NR=1 Far from the taffy-like substance that scientists organise the interior of the Earth around to support 'convection cells',I see the geodynamics of differential rotation bands as the viscous composition rotates unevenly from the maximum equatorial speed diminishing to nothing at the geographical poles. A mechanism worthy of the great Oceanic ridges and the fracture zones must be supplied by planetary rotational dynamics and if people cannot interpret that magnificent spectacle of the true nature of the interior pouring out from beneath the crust,then they are missing out on something really exciting if somewhat tragic from people who live in Earthquakes zones as the cause of those events are signatures of the rotation of the molten/viscous composition.
From: Sam Wormley on 6 Oct 2009 17:54 oriel36 wrote: > On Oct 6, 9:04 pm, Sam Wormley <sworml...(a)mchsi.com> wrote: >> oriel36 wrote: >> >>> At an elevation of 1 km,roughly .6 km below Denver's elevation ,an >>> observer with an unrestricted view can see across a distance of 112 km >>> to the horizon allowing for any minor variations such as refraction >>> ect .This 112 km value represents the equivalent of 1 degree latitude >>> so that the total distance the observer can see across a North/South >>> longitude meridian is 2 degrees of Latitude. >> >> Don't want to tax your brain too hard, Gerald, but a geosynchronous >> satellite can "see" Denver and a location on the equator simultaneously >> and the two locations have NO relative motion. > > Beneath the fractured crust is a vast ocean constructed of a rotating > viscous composition and when it appears through the fissures and > volcanoes on the surface,it is spectacular - > > http://www.youtube.com/watch?v=jXDyUi6PKjs&NR=1 > > Far from the taffy-like substance that scientists organise the > interior of the Earth around to support 'convection cells',I see the > geodynamics of differential rotation bands as the viscous composition > rotates unevenly from the maximum equatorial speed diminishing to > nothing at the geographical poles. A mechanism worthy of the great > Oceanic ridges and the fracture zones must be supplied by planetary > rotational dynamics and if people cannot interpret that magnificent > spectacle of the true nature of the interior pouring out from beneath > the crust,then they are missing out on something really exciting if > somewhat tragic from people who live in Earthquakes zones as the cause > of those events are signatures of the rotation of the molten/viscous > composition. > Nice change of subject, Gerald! I still worry that you don't have a coherent thought process.
From: oriel36 on 7 Oct 2009 02:09 On Oct 6, 10:54 pm, Sam Wormley <sworml...(a)mchsi.com> wrote: > oriel36 wrote: > > On Oct 6, 9:04 pm, Sam Wormley <sworml...(a)mchsi.com> wrote: > >> oriel36 wrote: > > >>> At an elevation of 1 km,roughly .6 km below Denver's elevation ,an > >>> observer with an unrestricted view can see across a distance of 112 km > >>> to the horizon allowing for any minor variations such as refraction > >>> ect .This 112 km value represents the equivalent of 1 degree latitude > >>> so that the total distance the observer can see across a North/South > >>> longitude meridian is 2 degrees of Latitude. > > >> Don't want to tax your brain too hard, Gerald, but a geosynchronous > >> satellite can "see" Denver and a location on the equator simultaneously > >> and the two locations have NO relative motion. > > > Beneath the fractured crust is a vast ocean constructed of a rotating > > viscous composition and when it appears through the fissures and > > volcanoes on the surface,it is spectacular - > > >http://www.youtube.com/watch?v=jXDyUi6PKjs&NR=1 > > > Far from the taffy-like substance that scientists organise the > > interior of the Earth around to support 'convection cells',I see the > > geodynamics of differential rotation bands as the viscous composition > > rotates unevenly from the maximum equatorial speed diminishing to > > nothing at the geographical poles. A mechanism worthy of the great > > Oceanic ridges and the fracture zones must be supplied by planetary > > rotational dynamics and if people cannot interpret that magnificent > > spectacle of the true nature of the interior pouring out from beneath > > the crust,then they are missing out on something really exciting if > > somewhat tragic from people who live in Earthquakes zones as the cause > > of those events are signatures of the rotation of the molten/viscous > > composition. > > Nice change of subject, Gerald! I still worry that you don't have > a coherent thought process. No change of subject,the Earth's rotational characteristics show up in geological features and central to the internal mechanism based on differential rotation of the viscous composition are different latitudinal speeds.On the surface fractured crust the speeds diminish from a maximum at the equator down to nothing at the geographical poles whereas a rotating viscous composition rotates in shear bands or unevenly from equator to poles.Of course,the maximum equatorial speed is 1669.8 km per hour making an entire revolution of the equatorial circumference (40,075 km) in 24 hours and sadly,an entire community refuses to acknowledge this basic planetary fact organised around the daily rotational characteristics of the Earth. For centuries they have known that the Earth's spherical deviation has a rotational component and adding differential rotation,something observed in all rotating celestial objects with exposed viscous compositions, as the major factor behind the 40 km spherical deviation meshes beautifully with the mechanism behind crustal evolution/motion and short term events such as Earthquakes or volcanic eruptions. Ever wonder why planetary rotational dynamics is absent from geodynamics and geology in general ? or in respect to the fuss of 'climate change' there are no inputs based on planetary dynamics,not even for the seasonal temperature fluctuations.My thought processes are fine however,and I never ask anyone to do it,I have to deal with 4 separate areas - the antecedent geocentric timekeeping systems of equable day/calendar system,the methods and insights behind planetary dynamics which dramatically altered the relationship between astronomical cause and terrestrial effect,the late 17th century distortions and errors which you adhere to and finally,the power of modern imaging and data which restores certain productive elements and opens up new areas for discussion such as geological signatures of planetary rotational dynamics.
From: Sam Wormley on 7 Oct 2009 03:12 oriel36 wrote: > On Oct 6, 10:54 pm, Sam Wormley <sworml...(a)mchsi.com> wrote: >> oriel36 wrote: >>> On Oct 6, 9:04 pm, Sam Wormley <sworml...(a)mchsi.com> wrote: >>>> oriel36 wrote: >>>>> At an elevation of 1 km,roughly .6 km below Denver's elevation ,an >>>>> observer with an unrestricted view can see across a distance of 112 km >>>>> to the horizon allowing for any minor variations such as refraction >>>>> ect .This 112 km value represents the equivalent of 1 degree latitude >>>>> so that the total distance the observer can see across a North/South >>>>> longitude meridian is 2 degrees of Latitude. >>>> Don't want to tax your brain too hard, Gerald, but a geosynchronous >>>> satellite can "see" Denver and a location on the equator simultaneously >>>> and the two locations have NO relative motion. >>> Beneath the fractured crust is a vast ocean constructed of a rotating >>> viscous composition and when it appears through the fissures and >>> volcanoes on the surface,it is spectacular - >>> http://www.youtube.com/watch?v=jXDyUi6PKjs&NR=1 >>> Far from the taffy-like substance that scientists organise the >>> interior of the Earth around to support 'convection cells',I see the >>> geodynamics of differential rotation bands as the viscous composition >>> rotates unevenly from the maximum equatorial speed diminishing to >>> nothing at the geographical poles. A mechanism worthy of the great >>> Oceanic ridges and the fracture zones must be supplied by planetary >>> rotational dynamics and if people cannot interpret that magnificent >>> spectacle of the true nature of the interior pouring out from beneath >>> the crust,then they are missing out on something really exciting if >>> somewhat tragic from people who live in Earthquakes zones as the cause >>> of those events are signatures of the rotation of the molten/viscous >>> composition. >> Nice change of subject, Gerald! I still worry that you don't have >> a coherent thought process. > > No change of subject,the Earth's rotational characteristics show up in > geological features and central to the internal mechanism based on > differential rotation of the viscous composition are different > latitudinal speeds.On the surface fractured crust the speeds diminish > from a maximum at the equator down to nothing at the geographical > poles whereas a rotating viscous composition rotates in shear bands or > unevenly from equator to poles.Of course,the maximum equatorial speed > is 1669.8 km per hour making an entire revolution of the equatorial > circumference (40,075 km) in 24 hours and sadly,an entire community > refuses to acknowledge this basic planetary fact organised around the > daily rotational characteristics of the Earth. > > For centuries they have known that the Earth's spherical deviation has > a rotational component and adding differential rotation,something > observed in all rotating celestial objects with exposed viscous > compositions, as the major factor behind the 40 km spherical deviation > meshes beautifully with the mechanism behind crustal evolution/motion > and short term events such as Earthquakes or volcanic eruptions. > > Ever wonder why planetary rotational dynamics is absent from > geodynamics and geology in general ? or in respect to the fuss of > 'climate change' there are no inputs based on planetary dynamics,not > even for the seasonal temperature fluctuations.My thought processes > are fine however,and I never ask anyone to do it,I have to deal with 4 > separate areas - the antecedent geocentric timekeeping systems of > equable day/calendar system,the methods and insights behind planetary > dynamics which dramatically altered the relationship between > astronomical cause and terrestrial effect,the late 17th century > distortions and errors which you adhere to and finally,the power of > modern imaging and data which restores certain productive elements and > opens up new areas for discussion such as geological signatures of > planetary rotational dynamics. Gerald, do you understand the Coriolis force?
From: oriel36 on 7 Oct 2009 09:45
On Oct 7, 8:12 am, Sam Wormley <sworml...(a)mchsi.com> wrote: > oriel36 wrote: > > On Oct 6, 10:54 pm, Sam Wormley <sworml...(a)mchsi.com> wrote: > >> oriel36 wrote: > >>> On Oct 6, 9:04 pm, Sam Wormley <sworml...(a)mchsi.com> wrote: > >>>> oriel36 wrote: > >>>>> At an elevation of 1 km,roughly .6 km below Denver's elevation ,an > >>>>> observer with an unrestricted view can see across a distance of 112 km > >>>>> to the horizon allowing for any minor variations such as refraction > >>>>> ect .This 112 km value represents the equivalent of 1 degree latitude > >>>>> so that the total distance the observer can see across a North/South > >>>>> longitude meridian is 2 degrees of Latitude. > >>>> Don't want to tax your brain too hard, Gerald, but a geosynchronous > >>>> satellite can "see" Denver and a location on the equator simultaneously > >>>> and the two locations have NO relative motion. > >>> Beneath the fractured crust is a vast ocean constructed of a rotating > >>> viscous composition and when it appears through the fissures and > >>> volcanoes on the surface,it is spectacular - > >>>http://www.youtube.com/watch?v=jXDyUi6PKjs&NR=1 > >>> Far from the taffy-like substance that scientists organise the > >>> interior of the Earth around to support 'convection cells',I see the > >>> geodynamics of differential rotation bands as the viscous composition > >>> rotates unevenly from the maximum equatorial speed diminishing to > >>> nothing at the geographical poles. A mechanism worthy of the great > >>> Oceanic ridges and the fracture zones must be supplied by planetary > >>> rotational dynamics and if people cannot interpret that magnificent > >>> spectacle of the true nature of the interior pouring out from beneath > >>> the crust,then they are missing out on something really exciting if > >>> somewhat tragic from people who live in Earthquakes zones as the cause > >>> of those events are signatures of the rotation of the molten/viscous > >>> composition. > >> Nice change of subject, Gerald! I still worry that you don't have > >> a coherent thought process. > > > No change of subject,the Earth's rotational characteristics show up in > > geological features and central to the internal mechanism based on > > differential rotation of the viscous composition are different > > latitudinal speeds.On the surface fractured crust the speeds diminish > > from a maximum at the equator down to nothing at the geographical > > poles whereas a rotating viscous composition rotates in shear bands or > > unevenly from equator to poles.Of course,the maximum equatorial speed > > is 1669.8 km per hour making an entire revolution of the equatorial > > circumference (40,075 km) in 24 hours and sadly,an entire community > > refuses to acknowledge this basic planetary fact organised around the > > daily rotational characteristics of the Earth. > > > For centuries they have known that the Earth's spherical deviation has > > a rotational component and adding differential rotation,something > > observed in all rotating celestial objects with exposed viscous > > compositions, as the major factor behind the 40 km spherical deviation > > meshes beautifully with the mechanism behind crustal evolution/motion > > and short term events such as Earthquakes or volcanic eruptions. > > > Ever wonder why planetary rotational dynamics is absent from > > geodynamics and geology in general ? or in respect to the fuss of > > 'climate change' there are no inputs based on planetary dynamics,not > > even for the seasonal temperature fluctuations.My thought processes > > are fine however,and I never ask anyone to do it,I have to deal with 4 > > separate areas - the antecedent geocentric timekeeping systems of > > equable day/calendar system,the methods and insights behind planetary > > dynamics which dramatically altered the relationship between > > astronomical cause and terrestrial effect,the late 17th century > > distortions and errors which you adhere to and finally,the power of > > modern imaging and data which restores certain productive elements and > > opens up new areas for discussion such as geological signatures of > > planetary rotational dynamics. > > Gerald, do you understand the Coriolis force? Ah,once I hear 'coriolis force' mentioned in respect to uni- directional differential rotation I know I am wasting my time with individuals who are just not up to the job of linking planetary dynamics with geological signatures,either in terms of features or short term events.If you can't figure out that the equatorial Earth rotates through 1669.8 km per hour ,and this none of you can do,then I am not going to throw good information after bad.I prefer to wait for individuals who can easily adapt to rotational dynamics of the interior and the common rotational mechanism which links spherical deviation with crustal evolution/motion. |