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The other is also a low-population state whose stable manifold bounds the basin of attraction (shaded gray) of the control state and separates it from the basin (unshaded) of the failure state.
The other is a saddle whose stable manifold bounds the basin of attraction of the former: its location provides a measure of the tolerance of the control mechanism to perturbations in the resistant allele density.
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Two different successions of remnant landsurfaces have been identified along the faults bounding the basins to the east, in the hangingwall and the footwall, respectively.
As for the basin geometry, subsurface data show that two minor depressions formed in the Colfiorito Basin during the Quaternary, the oldest one close to the fault bounding the basin, while the youngest (and deepest) formed in the inner portion of the basin.
A normwise analysis provides lower bounds on the basin of attraction and a more revealing picture is provided by pseudo-eigenvalues.
Two SE-dipping normal faults are exposed along the eastern and the southern flank of Mt. Kinabalu, but the ~10-km-long, west-dipping Marakau Fault bounds the eastern margin of the Ranau basin (Fig. 2a).
Its generally level terrain, in the basin of the north-flowing, dissipative Wimmera River, is bounded by the Murray River on the north and the Eastern Highlands to the south and covers an area of about 9,200 square miles (23,800 square km).
The region is bounded on the north by the Moulouya Basin, to the north west by the basin of Oum-Rbia, to the west by the pool Draa, on the east by the watershed Guir and south by Algeria.
The upper basin is the basin of Venice.
Examples are the Rotorua-Taupo Basin in New Zealand and the basin of Lake Toba in Sumatra.
This dense water fills the basins of the Nordic seas (the oceanic region bounded by Iceland, Greenland, Scandinavia, and northern Russia) and the continental shelf of Antarctica.
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