CONCLUSION 0501-01:
That the average realspeed of the gravitons in the gravitoncore of a
blackhole is highest at the equator and lowest at the axis. CONCLUSION 0501-02:
That the average realspeed of the gravitons in the gravitonocean and gravitonosphere of a blackhole is highest above the gravitoncore's equator and
lowest over the gravitoncore's poles. CONCLUSION 0501-03:
That a sufficient increase in the energy measure of an
overstable blackhole results in the movement of gravitons toward the
equator and the raising of an equatorial disc. CONCLUSION 0501-04:
That a sufficient increase in the energy measure of an
overstable blackhole results in the forming of vortexes in the gravitonocean and gravitonosphere in which gravitons stream from the equator to the
poles at high level and from the poles to the equator at low level. CONCLUSION 0501-05:
That a sufficient increase in the energy measure of an
overstable blackhole will form a centrifugally structured stable
blackhole.
PART 0502 - AXIAL BLACKHOLES
CONCLUSION 0502-01:
That every blackhole gravitonosphere consists of gravitonstreams in
which the measure of dynamic mass varies from place to place. CONCLUSION 0502-02: That many blackholes are within the gravitonospheric gravitonstreams of larger objects. CONCLUSION 0502-03: That a centrifugal blackhole will attune itself to the dynamic mass of the gravitonstream it is within. CONCLUSION 0502-04:
That a sufficient dynamic mass imbalance between a blackhole and
a gravitonstream results in a centrifugal blackhole becoming an axial
blackhole.
PART 0503 - GRAVITONOSPHERES AS DARKMATTER
CONCLUSION 0503-01: That a blackhole's gravitoncore gravitypulls its gravitonosphere and its gravitonosphere gravitypulls its gravitoncore. CONCLUSION 0503-02:
That every object within the gravitonosphere of a blackhole is being
gravitypulled by the gravitonosphere, the effect of which is to strengthen
or weaken the gravitypull of the gravitoncore on the object.