farmerman wrote:AVERAGE tectonic motion is usually computed based upon how fast and far ophiolitic magma erupts at seafloor spreading centers and then its routinely timed by the distance travelled normal to the ocean vent before each magnetic reversal imprints its "Bar Code" on the suboceanic lava. Seeing the process begin does, in no way mean that the scientists are stating that such initial opening events will persist. When a plate begins to spread at a center, theres no resistance and the plate masses are small. Soon (geologically) the speed will reduce to about 2 to 4 cm /yr. India has been a rapidly moving continental mass with some episodes of spreading at about 10 cm per year or thereabouts.
The process is wonderful and gives us a planetary "speedometer". If you look at teh Atlantic and Pacific spreading centers to their trailing or subducting ends, we see that there are no sediment or magmatic layers older than Jurassic , which is a pretty good way to do a Time, rate, and distance problem.
Popular science mags would lose readers if theyd print all the qualifiers and boring data . Anyway, if you look at a map of the horn of Africa this is one of a few rare zones on earth that are called "triple junctions" Three plate margins come together here at the junction of the red sea, gulf of Aden, as well as the East Africa Rift valley. There was a "plume" beneath this area , a plume of volcanics thats active since about 30 my ago. After the initial vulcanism Aden and the Red sea began to open and the unusual thing is that the Red sea is actually crust being "strtched" rather than new oceanic ophiolitic crust being formed. The East Africa rift valley has always been called an "aulocogen" sort of a failed rift since no new ocean basin had been opening within it for the 30 my. Now that it seems to be beginning I inclined to remind the authors that triple point stresses need to be resolved over the entire life of the tectonic feature, not because some "popular Science" dude wants to jazz up a story with a speedy sea floor spread.
Its about goddam time sez I. I was sick of Africa with this damn quiet plume. Plumes, which are a slightly different tectonic model base, are always quick to open , and then slow down, and in that fashion theyre slightly different from mid ocean ridges. Plumes are what we call " mantle source hotspots", like under Hawaii, or the Deccan plateau or the Parana basin , or the Snake River Plain. At a hotspot we often have the hotspot and the overlying plate moving separately. Torsvik and Van der Voo (2002) used geomag data to plot the differential movement of the Hawaian Island hotspot at about 3 cm a year moving SW and the overlying ocean crust moving NW at a speed of 4 cm a year. They solve the motion using vector analyses and inelastic collision physics (at very low velocities obviously).
I hope youre not implying by your "interesting " statement that this , in anyway concurs with someones young earth beliefs, cuz it doesnt.
Farmerman, are you a member here? You have to be a member to get the full text.
http://bulletin.geoscienceworld.org/cgi/content/abstract/115/9/1053
Early continental breakup boundary and migration of the Afar triple junction, Ethiopia
Samson Tesfaye,1, David J. Harding,2 and Timothy M. Kusky,3
1 Department of Earth and Atmospheric Sciences, St. Louis University, St. Louis, Missouri 63103, USA
2 NASA (National Aeronautics and Space Administration), Goddard Space Flight Center, Geodynamics Branch, Greenbelt, Maryland 20771, USA
3 Department of Earth and Atmospheric Sciences, St. Louis University, St. Louis, Missouri 63103, USA
Megascale accommodation zones mark the early continental breakup boundary of the Afro-Arabian plateau in Ethiopia. Motion along these megascale accommodation zones enabled the different arms of the Afar RRR (rift-rift-rift) triple junction to join together. An arcuate accommodation zone 45 km wide and 60 km long marks the transition from the N25°W-striking Southern Red Sea Rift trend in the western Afar margin to the N25°E-striking Main Ethiopian Rift. Another accommodation zone 80 km long marks the transition between the northeast- to north-northeast-trending Main Ethiopian Rift and the nearly east-trending Gulf of Aden. The positions of accommodation zones where rift orientations change by 50° suggest that they served as soft linking points between the kinematically "misaligned" arms of the triple junction during the initial breakup of the Afro-Arabian dome.
We use structural features to infer the present location of the triple junction in the Lake Abhe area. On the basis of the location of the paleo-triple junction, deduced from the position of accommodation zones and geomorphic considerations, it is estimated that the Afar triple junction has migrated 1.5° (160 km) in a north- northeast direction with respect to the African (Nubian) plate. The estimated amount of migration of the Afar triple junction is less than the 200 km migration expected from plate-kinematic analysis. This discrepancy suggests either a slower rate of spreading than the current 1.6 cm/yr (Africa-Arabia) during the early phase of rifting or a later early Miocene rather than Oligocene-Miocene age for the initiation of tectonic activity in the triple junction.