UNESCO World Heritage Centre - World Heritage List. Extension of the . It was transferred to the Xunta de Galicia by Royal Decree in 1. The Spanish Constitution reserves certain rights in relation to the heritage to the central government. However, these are delegated to the competent agencies in the Autonomous Communities, in this case the Xunta de Galicia. For the Lugo walls the Xunta is in the position of both owner and competent agency. Under the Galician Heritage Law the Xunta is required to cooperate with the municipal authorities in ensuring the protection and conservation of listed monuments, and certain functions are delegated down to them. The Xunta operates through its General Directorate of Cultural Heritage (Direcci. This was followed in 1. Special Plan for the Protection and Internal Reform of the Fortified Enceinte of the Town of Lugo, which is concerned principally with the urban environment of the historic town. However, it has a direct impact on the protection afforded to the walls, in terms of traffic planning, the creation of open spaces, and regulation of building heights. Another planning instrument which affects the walls is the Special Plan for the Protection of the Mi. Nor is there a technical unit specifically responsible for the conservation and restoration of the walls. It is against this background that serious consideration is being given to the creation of an independent foundation, under royal patronage and with representatives from government, academic, voluntary, and business institutions, to work with the General Directorate of Cultural Heritage of Galicia. The work plan of this body would include the development and implementation of integrated conservation, restoration, and maintenance programmes. Le « Mur d'Hadrien », pr. Sacramento River: Buenaventura, San Roque, Rio de los Sacramentos: Sacramento River from the old pumping station in Sacramento, California. Nickname: Sac River, Nile. Dealer in maps and atlases from the 16th to 19th Centuries. Also offers reference books about maps, the history of cartography, and geography. Organisation de l’ ISTITUTO ORDINE DI SANT ANDREA DI CAFFA ORDRE SAINT ANDRE DE CAFFA. 1890; 1900; 1910; 1920; 1930; 1940; 1950; 1960; 1970; 1980; 1990; 2000. Patrimonio de la Humanidad: la lista del Patrimonio Mundial de la UNESCO actualizada en Agosto 2011, con enlaces a fotograf La structure du parc est simple : une scenic road de huit miles qui s’enfonce dans les dunes. The WH area is managed directly by the Divisional Forest Officer from the Forest Dept. A national steering Committee co- ordinates institutions for Sinharaja as a National Wilderness Area, Biosphere Reserve (1. Welcome Fortune City Customers. Fortune City is now Dotster. With this change, you now have 24x7 support. Don't hesitate to call our Support team toll free at 800-401. Route 50 (El Dorado Freeway), Ruta Estatal 99, Ruta. Barnum & Bailey's Greatest Show on Earth, 1901 Route Barnum & Bailey, Ltd., proprietor. WH site. There are two management plans, prepared in 1. In 1. 97. 9, the Committee decided to inscribe the Ohrid Lake on the World Heritage List under natural criteria (iii). In 1. 98. 0, this property was extended to include the cultural and historical area, and cultural criteria (i)(iii)(iv) were added. The “Hadrian’s Wall” which was previously inscribed on the World Heritage List, is part of the transnational property “Frontiers of the Roman Empire”. Extension of . See Decision 3. Sacramento River - Wikipedia. Sacramento River. Buenaventura,San Roque,Rio de los Sacramentos. Nickname: Sac River, Nile of the West. The river drains about 2. California counties, mostly within the fertile agricultural region bounded by the Coast Ranges and Sierra Nevada known as the Sacramento Valley, but also extending as far as the volcanic plateaus of Northeastern California. Historically, its watershed has reached farther, as far north as south- central Oregon where the now, primarily, endorheic (closed) Goose Lake rarely experiences southerly outflow into the Pit River, the most northerly tributary of the Sacramento. The Sacramento and its wide natural floodplain were once abundant in fish and other aquatic creatures, notably one of the southernmost large runs of chinook salmon in North America. For about 1. 2,0. Native American populations in California. The river has provided a route for trade and travel since ancient times. Hundreds of tribes sharing regional customs and traditions inhabited the Sacramento Valley, first coming into contact with European explorers in the late 1. The Spanish explorer Gabriel Moraga named the river Rio de los Sacramentos in 1. Sacramento. In the 1. Sacramento River, starting the California Gold Rush and an enormous population influx to the state. Overland trails such as the California Trail and Siskiyou Trail guided hundreds of thousands of people to the gold fields. By the late part of the century mining had ceased to be a major part of the economy, and many immigrants turned to farming and ranching. Many populous communities were established along the Sacramento River, including the state capital of Sacramento. Intensive agriculture and mining contributed to pollution in the Sacramento River, and significant changes to the river's hydrology and environment. Since the 1. 95. 0s the watershed has been intensely developed for water supply and the generation of hydroelectric power. Today, large dams impound the river and almost all of its major tributaries. The Sacramento is used heavily for irrigation and serves much of Central and Southern California through the canals of giant state and federal water projects. While now providing water to over half of California's population and supporting one of the most productive agricultural areas in the nation, these changes have left the Sacramento greatly modified from its natural state and have caused the decline of its once- abundant fisheries. The Sacramento River originates in the mountains and plateaus of far northern California as three major waterways that flow into Shasta Lake: the Upper Sacramento River, Mc. Cloud River and Pit River. The Upper Sacramento begins near Mount Shasta, at the confluence of North, Middle and South Forks in the Trinity Mountains of Siskiyou County. It flows east into a small reservoir, Lake Siskiyou, before turning south. The river flows through a canyon for about 6. Dunsmuir and Castella, before emptying into Shasta Lake near Lakehead in Shasta County. The Mc. Cloud River rises on the east slope of Mount Shasta and flows south for 7. Cascade Range, roughly parallel to the Upper Sacramento, eventually to reach the Mc. Cloud Arm of Shasta Lake. Draining a vast and remote volcanic highlands area, it flows southwest for nearly 3. Shasta Lake near Montgomery Creek. Goose Lake, straddling the Oregon. The Goose Lake watershed is the only part of the Sacramento River basin extending into another state. Before the construction of Shasta Dam the Mc. Cloud River emptied into the Pit River, which joined the Sacramento near the former mining town of Kennett, submerged when Shasta Lake was filled. The Pit River Bridge, which carries Interstate 5 and the Union Pacific Railroad over the reservoir, is the highest double- decked bridge in the United States. The Upper Sacramento River canyon also provides the route for I- 5 and the railroad between Lakehead and Mount Shasta. It flows through Keswick Dam, where it receives about 1,2. Trinity River. It then swings east through Redding, the largest city of the Shasta Cascade region, and turns southeast, entering Tehama County. East of Cottonwood it receives Cottonwood Creek . Below Battle Creek it carves its last gorge, Iron Canyon, emerging from the hills at Red Bluff, where the Red Bluff Diversion Dam removes water for irrigation. Beyond Red Bluff the river reaches the low floodplain of the Sacramento Valley, receiving Mill Creek from the east and Thomes Creek from the west near Los Molinos, then Deer Creek from the east near Vina. A few miles downstream it forms the border of Butte County and Glenn County to the west. Stony Creek joins from the west in Glenn County, near Hamilton City and about 1. Chico. The river then forms the Glenn. It passes by the Sutter Buttes, a group of volcanic hills that rise abruptly from the middle of the Sacramento Valley, where it receives Butte Creek from the east at Colusa. Below Colusa the river flows south- southeast, forming the border of Colusa County and Sutter County to the east. During floods, water overtops the weir and flows east into the Sutter Bypass, the first of two major bypass channels that temporarily store and move floodwaters downstream to reduce pressure on the main channel of the Sacramento. The Sacramento River and the Sutter Bypass flow parallel for over 4. Sutter County and Yolo County near Knights Landing. The Feather River, the largest tributary of the Sacramento, joins from the east at Verona directly below the Sutter Bypass. A second flood control structure, the Fremont Weir, diverts flood waters from both the Sacramento and Feather Rivers into the Yolo Bypass, which parallels the Sacramento River down the west side of the valley. Cache Creek and Putah Creek, two major tributaries which formerly joined the Sacramento River from the west, are now intercepted by the Yolo Bypass via man made channels. Sacramento International Airport is located on the east bank of the river near Fremont. The river then enters the Sacramento metro area, where it receives the American River from the east, then passes under the historic Tower Bridge and Interstate 8. The California State Capitol sits less than half a mile (0. Tower Bridge crosses it. Shortly downstream, the Port of Sacramento is located on the west side of the Sacramento, connected to the river by a lock. The Sacramento River Deep Water Ship Channel provides access to the port from the Pacific, bypassing about 4. Sacramento. The channel runs parallel to the Sacramento several miles to the west, and also forms the eastern boundary of the Yolo Bypass. The Sacramento is by far the largest contributor of fresh water to the Delta; in an average year it accounts for more than 8. At Walnut Grove, the manmade Delta Cross Channel connects the Sacramento to the Mokelumne River channel, allowing a portion of the water to be pumped south toward Clifton Court Forebay, the receiving reservoir for the main CVP and State Water Project aqueducts which irrigate millions of acres and supply water to over 2. San Joaquin Valley, the San Francisco Bay Area and Greater Los Angeles. Although river levels are tidally influenced here and occasionally as far north as Verona. Saltwater intrusion from the Pacific Ocean was one of the main reasons for the construction of the federal Central Valley Project (CVP), whose dams maintain a minimum flow in the Sacramento to keep seawater at bay. Maintained as part of the Deep Water Ship Channel, it is navigable by large oceangoing vessels and averages three- quarters of a mile (1. North of Antioch and Pittsburg, the Sacramento and San Joaquin Rivers join at the head of Suisun Bay, marking the official end of both rivers. The combined waters flow west through Suisun Bay and the Carquinez Strait into San Francisco Bay, joining the Pacific at the Golden Gate. The natural runoff of the river is 2. Before dams were built on its tributaries, the river flooded up to 6. Mississippi River. Late summers of particularly dry years could see flows drop below 1,0. Annual depletions (water not returned to the river after use) are about 4. An additional 7. 6. Delta to combat salinity. Geological Survey (USGS) has stream gauges on 2. Sacramento River, although not all of them are currently operational. The Freeport gauge, which sits just downstream of Sacramento, provides a relatively good metric of the annual outflow from the Sacramento River Basin. The average flow between 1. The maximum recorded flow was 1. February 1. 9, 1. October 1. 5, 1. 97. A separate gauge on the bypass recorded an average throughput of 4,8. December. The highest recorded flow was 3. February 2. 0, 1. During the dry season of July through September, the bypass carries low to zero flow. At the USGS Montgomery Creek gauge, the average flow of the Pit River was 4,7. Almost the entire basin lies between the Sierra Nevada and Cascade Range on the east and the Coast Ranges and Klamath Mountains in the west. The other two are the Klamath River and Columbia River. The Colorado River, which reaches the Gulf of California just south of the US- Mexico border near the southeast part of the state, is far larger than the Sacramento by both length and drainage area but has a slightly smaller flow. The Sacramento, when combined with the Pit, is also one of the longest rivers in the United States entirely within one state. The Russian River also lies to the west and the endorheic (closed) Honey Lake and Eagle Lake basins to the north. On the east side are many endorheic watersheds of the Great Basin including the Truckee River and Carson River. Parts of the Sacramento watershed come very close to, but do not extend past, the border of California and Nevada. Mount Shasta, the highest mountain in the Sacramento drainage, is seen in the distance. The basin's diverse geography ranges from the glacier- carved, snowcapped peaks of the Sierra Nevada to the sea- level (and often lower) marshes and agricultural lands of the Sacramento- San Joaquin Delta.
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