We explore the Magellanic Stream (MS) using a Gaussian decomposition of the
HI velocity profiles in the Leiden-Argentine-Bonn (LAB) all-sky HI survey. This
decomposition exposes the MS to be composed of two filaments distinct both
spatially (as first pointed out by Putman et al.) and in velocity. Using the
velocity coherence of the filaments, one can be traced back to its origin in
what we identify as the SouthEast HI Overdensity (SEHO) of the Large Magellanic
Cloud (LMC), which includes 30 Doradus. Parts of the Leading Arm (LA) can also
be traced back to the SEHO in velocity and position. Therefore, at least
one-half of the trailing Stream and most of the LA originates in the LMC,
contrary to previous assertions that both the MS and the LA originate in the
Small Magellanic Cloud (SMC) and/or in the Magellanic Bridge. The two MS
filaments show strong periodic, undulating spatial and velocity patterns that
we speculate are an imprint of the LMC rotation curve. If true, then the drift
rate of the Stream gas away from the Magellanic Clouds is ~49 km/s and the age
of the MS is ~1.74 Gyr. The Staveley-Smith et al. high-resolution HI data of
the LMC show gas outflows from supergiant shells in the SEHO that seem to be
creating the LA and LMC filament of the MS. Blowout of LMC gas is an effect not
previously accounted for but one that probably plays an important role in
creating the MS and LA.Comment: 31 pages, 26 figures, Accepted for publication in Ap