One side of the stage leads straight to a rising slope of tiered seating, with a proximity the Joyce usually lacks.
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Dubbed, Rancho San Leandro, the estate sits on a "gently rising slope, with glorious views that extend from the Santa Ynez mountains across the Montecito Valley to the shimmering Pacific," according to a previous listing.
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Founded in 1100, the scattered village is located on a gently rising slope of the valley at the foot of the 2718 m high Serles. Inhabited from the early Middle Ages, the centre has houses decorated with baroque frescoes.
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Piedra Negra Airport (), is an airstrip just southwest of Curanipe, a Pacific coastal town southwest of Pelluhue, in the Maule Region of Chile. The airstrip is in a wooded section less than inland from the shore. The runway has a rising slope to the northeast.
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The house nestles in the Chiltern Hills. Behind the main house, there is a walled garden in an Italianate style on a rising slope, providing good views. Around the house is a park with a herd of fallow deer. Around the park are Almshill Wood, Balham's Wood and Kildridge Wood.
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158 A wide entrance that narrowed down on a gently rising slope would also slow their progress when pursued by hounds and places where people could hide,Fletcher, p.157 possibly with hounds until required would be advantageous.Fletcher, p.156 The beaters would also separate the stags from the hinds if required.
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The attic acts as a hayloft and is accessed via a ramp or a footbridge from the rising slope behind the house. The often dormer-shaped entrance is known in Alemannic as a "Ifahrhüsli". The hay can easily be thrown down into the stalls below from the hayloft through a so-called hay hatch (Heuloch, literally "hay hole").
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Convective precipitation occurs when air rises vertically through the (temporarily) self-sustaining mechanism of convection. Stratiform precipitation occurs when large air masses rise diagonally as larger-scale atmospheric dynamics force them to move over each other. Orographic precipitation is similar, except the upwards motion is forced when a moving air mass encounters the rising slope of a landform such as a mountain ridge.
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The soak is controlled primarily by the conveyor speed. The peak of the RTS profile is the endpoint of the linear ramp to the peak segment of the profile. The same considerations about defects in an RSS profile also apply to an RTS profile. When the PCB enters the cooling segment, the negative slope generally is steeper than the rising slope.
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Pier 6, ground zero of the explosion, is on the extreme right. The Hydrostone District was built to replace buildings devastated by the Halifax Explosion. Richmond was devastated on December 6, 1917 when the Halifax Explosion levelled much of its structures and waterfront. The rising slope of Fort Needham protected some areas from the immediate effects of the shock wave.
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It then continued across a narrow ravine and crashed against the side of a steeply rising slope approximately half a mile beyond the first tree strike. The main wreckage area was at about above sea level. The landing gear was down and locked at the time of impact. There was no evidence of mechanical or structural failure prior to the impact.
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This effect is known as the optical spring effect (light-induced spring constant). However, the model is incomplete as it neglects retardation effects due to the finite cavity photon decay rate \kappa. The force follows the motion of the mirror only with some time delay, which leads to effects like friction. For example, assume the equilibrium position sits somewhere on the rising slope of the resonance.
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The ratha is a simple structure, resembling a small palace or pavilion. It is carved over an elongated stone rock formation, a protrusion above the sand near the coast (which has a gradually rising slope from the north end to the southern end) of a moulded plinth, with a square plan similar to the Dharmaraja Ratha. It faces west and measures and is in height. It is on the same upapitha (secondary platform) as the Draupadi Ratha next to it.
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Ancient Elateia was situated about the middle of the great fertile basin that extends nearly 20 miles, from the narrows of the Cephissus River below Amphicleia, to the entrance into Boeotia. Hence it was admirably placed for commanding the passes into southern Greece from Mount Oeta, and became a post of great military importance.Strabo, Geographica, ix. 3 Pausanias describes it as situated over against Amphicleia, at the distance of 180 stadia from the latter town, on a gently rising slope in the plain of the Cephissus.
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Convective Instability, denoted in the red highlighted region ("positive area"), on a Skew-T log-P diagram. In meteorology, convective instability or stability of an air mass refers to its ability to resist vertical motion. A stable atmosphere makes vertical movement difficult, and small vertical disturbances dampen out and disappear. In an unstable atmosphere, vertical air movements (such as in orographic lifting, where an air mass is displaced upwards as it is blown by wind up the rising slope of a mountain range) tend to become larger, resulting in turbulent airflow and convective activity.
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The village is centered on the former site of the mill on the east bank of the Quinebaug River, near where modern Route 205 crosses the river. The village extends eastward from the river up a gently rising slope towards Route 12 located at the crest of a ridge. The mill workers' houses are located along Walnut and Chestnut streets just east of the mill site, while the supervisor's houses and the company store are located further east (and further up in elevation). The mill owners' houses and the church are even further up and east.
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The Hub was opened on Monday 5 September 2011 and has since become a focal point of the locality. Due to its height, rising to three storeys, and position on the gently rising slope of Rodway Road, the Hub building can be seen rising above the surrounding buildings, particularly when approaching the area from the north side, over the railway bridge. Patchway has had a long connection with the Scout Movement, with the Headquarters being located in buildings of Worthing Road – behind the Town Council offices. In June 2011 the Scout Movement are celebrating their 70th Anniversary and will be holding special events to commemorate this.
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In addition to sharing the Carboniferous Lowlands, the southern portion of the peninsula is dominated by the Atlantic Interior (Sissiboo Lowlands, South Mountain, various slate ridges), followed by the comparatively small Triassic Lowlands (the Annapolis Valley), and the Fundy Coast (including Economy Mountain and North Mountain) and Atlantic Coast regions. The Atlantic Interior is dominated by a glacial landscape of exposed granitic rock, thick forest, drumlins and numerous lakes. The Sissiboo Lowlands comprise many river valleys and lowland inland areas in the southwest and central portion of the peninsula. The South Mountain is a steadily rising slope that descends sharply at the Annapolis Valley but more gradually toward the Atlantic, resulting in a plateau across much of the southwest interior of the peninsula with average elevations of 150 m and maximum elevations of 275 m.
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Azarethes's deployment was similar; his left flank was composed of Lakhmid cavalry under al-Mundhir and corresponded to the Ghassanid section of his opposing force, while his own cavalry was in the center. The two armies met outside Callinicum on 19 April 531 CE. Both armies formed up differently, Belisarius again choosing an "odd" formation that confused his opposing general. In this case he anchored his left flank on the bank of the river with heavy Byzantine infantry, to their right the army's centre, all of the Byzantine cavalry, many of which were cataphracts under the command of Ascan. Linking the centre to the Byzantine right was a detachment of Lycaonian and/or Isaurian infantry (under Stephanacius and Longinus), positioned such that their right was anchored on a rising slope occupied by the army's right wing, which consisted of the 5,000 Ghassanid allies.
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The neighborhood is located along the eastern (left bank) of the Lehigh River on the opposite bank from the Jim Thorpe business district. Situated on a gently rising slope of Bear Mountain, and its street grid is arrayed along either side of PA 903 which proceeds almost due northeast roughly parallel to the south-facing escarpment of Bear Mountain to connect with Albrightsville, PA and originates across the bridge joining the neighborhood with Jim Thorpe's business district and Tees into US 209. By the 1790s the area above the Lehigh Gap was being regularly penetrated by pioneers, and logging companies, in the face of the developing energy crisis, began small scale operations. Sitting to south of the dominant height of Broad Mountain across the Lehigh from where the Nesquehoning Creek crashes into the Lehigh in direct opposition, their confluence skews off at right angles to both in a wide mile long 'slack water pool' that sits between railyards on both banks and was the historic divide between the Mauch Chunk sides.
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