Compared to other well-studied hydrothermal systems in the Pacific, the ELSC is notable for unique ridge characteristics and gradients over short distances along the north-south ridge axis.
One schematic portrait of a man's skeleton points out that the skull is notable for a "thickened ridge where his shoulder and neck muscles connected to the back of his head," caused by heavy lifting.
A notable feature of the Daito Ridge crust is that a material with Vp ≤ 6.3 km/s and a thickness of 6 to 11 km is concentrated in the southern part, while a material with Vp ≥ 6.3 km/s ascends closer to the seafloor toward the Kita-Daito Basin in the north.
When a special election for a vacant seat in Scranton was held in June, Vice President Al Gore campaigned in the district; President Clinton recorded radio commercials; and Governor Ridge, along with other notable Republicans, made local appearances.
The ELSC is notable for north-to-south gradients in seafloor geology, ridge morphology and hydrothermal activity [6 9].
Other notable hills include Crown Hill, View Ridge/Wedgwood/Bryant, Maple Leaf, Phinney Ridge, Mt. Baker Ridge and Highlands/Carkeek/Bitterlake.
It follows the ridge of the southern Green Mountains, summitting such notable peaks as Stratton Mountain, Glastenbury Mountain, and Killington Peak.
A notable geologic feature is the fine series of eskers (long ridges of postglacial gravel), notably at Clonmacnoise, an ancient monastic site near the Shannon.
Despite the large heterogeneity among the Vp models for the DAr2, ODr9, DAr5, and DAr3 lines, a common characteristic of these velocity structures is another notable difference between the northern and southern parts of the ridge.
Notable landmarks include the Roman Catholic, Anglican, and Presbyterian churches, on the central ridge; Fort George, at the promontory's tip; and Government House, on a slope overlooking the town.
