From: owner-ammf-digest@smoe.org (alt.music.moxy-fruvous digest) To: ammf-digest@smoe.org Subject: alt.music.moxy-fruvous digest V14 #14396 Reply-To: ammf@fruvous.com Sender: owner-ammf-digest@smoe.org Errors-To: owner-ammf-digest@smoe.org Precedence: bulk alt.music.moxy-fruvous digest Tuesday, August 6 2024 Volume 14 : Number 14396 Today's Subjects: ----------------- Say Goodbye to Monthly Bills with ClearWave HD TV Antenna ["TV Antenna" <] ---------------------------------------------------------------------- Date: Tue, 6 Aug 2024 12:11:04 +0200 From: "TV Antenna" Subject: Say Goodbye to Monthly Bills with ClearWave HD TV Antenna Say Goodbye to Monthly Bills with ClearWave HD TV Antenna http://brandrotation.cfd/yvMM8cvN6kKjthF3ItXEuADiXX5JzHHtAniyM3hExCRZdE65lQ http://brandrotation.cfd/5Vab01DXK7h6ZX51E1E1_-GlHUx_Nzvx2uhBgNoJxE8ZCQR5 ortheast monsoon, but during the dry season surface water becomes an important factor. The bodies of surface water appear in the forms of streams, tanks, waterholes, rock pools, and lagoons. Waterholes occur in low lying places while rock pools of varying size are capable of containing water year-round, and are hence an important source of water for elephants. For many water birds and water buffaloes natural waterholes are ideal habitats. Such reservoirs are largely concentrated to the Block I followed by Block II. Several tanks are there including, Maha Seelawa, Buthawa, Uraniya, and Pilinnawa tanks. Many rivers and streams flow in a southeasterly direction, originating in the highlands of adjacent Uva and central hills. Kumbukkan Oya in the east and Menik River and its tributaries in the west flow across the park, and provide an important water source in the dry season to wild animals of the park. Normally the streams of the park are dry during the drought season. These rivers and streams exhibit a degree of runoff fluctuations between wet and dry seasons. Kumbukkan Oya discharges seven times as much water in the rainy season than in the dry season. A number of lagoons are situated along the coast line of the park. There are several routes to get to Yala from Colombo, while the route via Ratnapura and Tissamaharama is the shortest with 270 kilometres (170 mi). Impact of the 2004 tsunami Yala lay in the direct path of the 2004 Indian Ocean tsunami, which impacted Sri Lanka 90 minutes after its generation. The tsunami caused severe but localized damage on the park, with around 250 people being killed. The tsunami wave was reported to be 20 feet (6.1 m) high. The tsunami waves reached inland only through the river-mouth gaps in the coastal dunes. Inundation distances from ranged up to 392 to 1,490 metres (429 to 1,629 yd). The main habitats affected are scrub forest and grasslands. About 5,000 hectares (19 sq mi) of grassland, forest, and wetland were directly affected by the tsunami. The satellite images revealed that mean normalized difference vegetation index (NDVI) range from 0.245 to 0.772 in the Block I and II. After the disaster the NDVI value fell dramatically to 0.2111. Around 60% of the area along the coastline has changed. The damage was worse closer to the sea. The movement patterns of two radio collared elep ------------------------------ End of alt.music.moxy-fruvous digest V14 #14396 ***********************************************