Dundas and co-authors say that banding and color variations apparent in some of the scarps
suggest layers "possibly deposited with changes in the proportion of ice and dust under varying climate conditions.
The elliptical scarps
and low depth-to-diameter ratio for both the North and Bloody Creek structures suggest a low-angled impact (Elbeshausen et al.
Prior to preparing the SCARP
samples used in this study for MIIUPLSR analyses, the influence of duration of grinding in the Retsch MM400 grinding mill on the variability of acquired MIR spectra and PLSR prediction results was quantified.
By contrast with the smaller streams to north and south, the River Torrens had the volume to maintain its flow to the west, although immediately below its gorge mouth its course was diverted to the north by the alluvial fans building out from the Burnside-Eden Fault Scarp
, which caused it to undercut and steepen the northern slope of the valley (GREAR et al.
are complicated financial products which provide income to customers but also expose them to the risk that they lose all or part of their initial capital.
Differentiated heights of the Sudetic mountain front correlate to some extent with the lithology of the footwall; the highest sectors of the scarp
correspond to geological units that are built mainly of gneisses (Sowie Mts.
The Sudetic Marginal Fault (SMF) is one of the most clearly marked tectonic zones of Europe, more than 300-km-long, the 200 km of which is represented by a well-pronounced morphotectonic scarp
Thus we have the Manitoulin Scarp
bordering Georgian Bay in the Bruce; the Scarp
of Valleys which extend deeply inland further east along Georgian Bay; the Earthen Scarp
stretching south toward the town of Belfountain where moraines and glacial debris bury the underlying structures; and the relatively well known Southern Scarp
which is largely dominated by steep cliffs stretching to Niagara Falls and into New York State.
Without a dynamically positioned ship and tow-fish system, near-bottom surveys over rough topography or along scarp
faces are virtually impossible to achieve.
Linear programming models of representative farms in SCARP
1 area of Punjab Province were developed to explore the efficiency and equity implications of various transition options.
The Crump Geyser and main hot springs occur on the NGP geothermal leases over a four mile interval at the base of a prominent range front faults scarp
along the western edge of Warner Valley and out into the valley a distance of about 3000 feet.
from 132-KV Scarp
Colony grid station, 240 Mor, Ali Pur, Dana Abad and Bachiana feeders originating from 132-KV Jaranwala grid station, Jaranwala Road feeder emanating from 132-KV Khurarianwala grid station, Usman Abad feeder originating from 132-KV Chiniot grid station, Imam Bargah Road feeder emanating from 132-KV Factory Area grid station, Akbar Abad feeder originating from 132-KV University grid station, Gulistan Colony feeder emanating from 132-KV OTP grid station, Wallah and Lalian City feeders originating from 132-KV Lalian grid station,