The sand ridges are identified as accumulations of material that have been brought down by rivers from Sumatra.
Linear ridges are identified as dark brown tone linear structures.
A chicken transcriptome map is described previously, and regions with clusters of the most highly expressed genes, covering about 10% of the chicken genome, so called "RIDGEs", are identified [11].
Most work on change-points is directed towards curve discontinuities but in the facial setting the boundary ridges are identified by discontinuities, or sharp changes, in the first derivative of the curve z (s ) which corresponds to the depth component z of the principal curve as it moves up the facial surface.
A sandstone pinch out, inferred to be part of the Turonian Coniacian sandstone ridge, was identified at depths of ~25 m, towards the eastern end of the profile.
The normal oceanic crust was identified beneath the Zenisu Ridge by a velocity structure study using OBS (Nakanishi et al. 2002), and the magnetization highs associated with the ridge topography were identified by a magnetic inversion study (Kido and Fujiwara 2004).
In summary, contact angle hysteresis, roughness, and evaporation from ridge partitioned microlayer were identified as the three mechanisms associated with nanoscale and microscale G/GO coated surfaces.
RIDGEs and anti-RIDGEs were identified using the same approach as for the chicken data.
The optimum synthetic conditions, which were identified using Ridge max analysis, were as follows: immobilized lipase AWCO mass ratio 0.02 1, fatty acid:methanol molar ratio 1 1.10, hexane AWCO ratio 1.33:1 (mL/g), and temperature 40 °C.
Until January 2008, the United States Board on Geographic Names (USBGN) did not recognize Metacomet Ridge, Traprock Ridge or any other name, although several sub-ranges were identified.
