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The backbone range of the Ōu Mountains forms the major climatic boundary of the region.
To the south, the Backbone Range descends abruptly in a steep escarpment to the Kibi Plateau.
The Chūgoku Range consists of three landforms the Backbone Range, the Kibi Plateau, and the Iwami Plateau.
The Backbone Range constitutes a sharp divide between the Sea of Japan and the Inland Sea, broken only by the gorge of the Gōno River in the west.
The Iwami Plateau, lying to the north of the Backbone Range, is narrower and more dissected than the Kibi Plateau, except in the Akiyoshi Plateau area in the west, where karst topography occurs in some places.
Ou Backbone Range.
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In previous gaming generations, these mid-range games formed the functional backbone of gaming.
Calculated half-lives for the isomerization of cis-azobenzene linkages buried in the polymer backbone ranged from 1 day near room temperature to about 1 h at the 60°C isotherm.
At greater crustal depths, the backbone ranges are associated with 2-D conductors elongated in the NNE-SSW direction.
Gray dashed lines encircle strain concentration zones of the Ou-backbone Range (OBR) and the northeastern part of the Niigata-Kobe Tectonic Zone (NKTZ).
After examining interseismic strain anomalies and the coseismic deformation of the 2011 earthquake in NE Japan, Ohzono et al. (2012b) proposed a weak zone below the tens of kilometers wide Ou-backbone range, in the vicinity of the arc.
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