Topography Clause Samples

Topography. Altering the existing topography of the Property by digging, plowing, disking, or otherwise disturbing the surface is prohibited, unless Grantee determines such requested action will be carried out consistent with the Restoration Plan and will be carried out in a manner that protects the conservation values. Grantor shall obtain ▇▇▇▇▇▇▇’s written permission in advance of commencing such action.

Topography. The Long Beach Peninsula exhibits long and low parallel north-south dune ridges🕈 interspersed with shallow ▇▇▇▇▇. The following dune forms are found in this landscape: foredune, deflation plain, sand hummock🕈, blowout🕈, dune ridge, and swale🕈. (▇▇▇▇▇▇▇▇▇, 1984) From west to east, first there is a broad and gradually sloping ocean beach. The foredune is a ridge of sand parallel to the ocean beach and located just above the limit of ordinary wave action. Behind the foredune is a low-lying deflation plain where interdunal wetlands form at surface elevations of 14 feet National Geodetic Vertical Datum of 1929🕈 (NGVD29🕈) or lower. To the east of the deflation plain is the historic foredune, a dune ridge. The foredune, deflation plain, and dune ridge comprise the city’s dune area, or dune complex, averaging about 2,000 feet in width. The ocean floor from the shore outward to approximately seven (7) miles is considered the inner (nearshore-shallow) continental shelf🕈 with a relatively flat slope and depths up to 131 feet. West of the inner shelf is the midshelf, an irregular band varying in width from seven (7) to 17 miles, also of a relatively flat slope and with depths of 131 to 656 feet. Beyond the midshelf is a the relatively narrow mesobenthal🕈 upper continental slope with depths of 656 to 2,297 feet, and finally is the bathybenthal🕈 lower to toe of the continental slope with depths of 2,297 to 11,500 feet. The substrate of the inner shelf is sand; the substrate of the midshelf and the mesobenthal is sand and mud with some rock outcropping; and the substrate of the bathybental is mud. (Washington Marine Spatial Planning, 2014)

Topography. Contractor has visually surveyed the general surface conditions of the Project Site topography and represents that, subject to Unforeseen Subsurface Conditions, the same are sufficient for Contractor to construct the Project and perform the Work. Contractor will be responsible for clearance of the Project Site, including the removal of obstructions. Contractor will be responsible for access road construction as described in the Scope of Work. Contractor shall provide for the procurement of or disposal of, as necessary, all soil, gravel and similar materials required for the performance of or otherwise in connection with the Work. Contractor will provide adequate treatment of and protection against water runoff resulting from Contractor’s and its Subcontractor’s work. Contractor will provide for the collection, treatment and disposal of groundwater resulting from Contractor’s and its Subcontractors’ work.

Topography. There shall be no ditching; draining; diking; filling; excavating; removal of topsoil, sand, gravel, rock, or other materials; or any change in the topography of the land in any manner, unless in accordance with the farm conservation plan for agricultural use on the Protected Property referenced in Paragraph C above.

Topography. The surface topography of the Kriel area is typical of the Mpumalanga Highveld consisting in the main of a gently undulating plateau. The flood plains of the local streams are at an average elevation of ± 1540 meters above mean sea level and drainage generally is a northerly direction. The existing and potential sources of air pollution in Kriel area are the following:  ▇▇▇▇▇ Power Station stack emissions  ▇▇▇▇▇ Power Station dry dust (fly ash) handling plant  Dust blow from the Eskom coal stock yard  Dust blow from the roads in the area  Seasonal dust blow caused by ploughing of farmlands, and dust blow off denuded fields  Dust blow from dried out exposed surfaces of the wet ash dam. However, Eskom utilises the majority of the top surface of the ash dam as an evaporation pan for polluted water, which means that the exposed surface is constantly wet. The sides of the ash dam have largely been rehabilitated, with the result that dust blow from the ash dam.

Topography. The surface topography of the Kriel area is typical of the Mpumalanga Highveld consisting in the main of a gently undulating plateau. The flood plains of the local streams are at an average elevation of ± 1540 meters above mean sea level and drainage generally is a northerly direction.

Topography. 4.4 Drainage

Topography. The landform lies relatively flat along the most northerly section, and then slopes gently downwards in a south easterly direction towards Eglwys Brewis Road. The land falls from 44m AOD to 34m AOD over a distance of approximately 310m. At Boverton Brook, the site rises to 36m AOD southwards and at Llanmaes Brook, the site rises again to approximately 39m AOD eastwards.

Topography. There shall be no change in the topography of the Property except as expressly provided in the PRMP or MBI. There shall be no surface mining, filling, excavating, grading, dredging, mining or drilling upon the Property, and there shall be no removing of topsoil, peat, sand, gravel, rock, minerals or other materials from the Property except to restore natural topography or drainage patterns.