Some detailed information on the Web about the physical characteristics of the castle are at the following sites: Perhaps a snail-mail letter or telephone call to the museum at the castle might help. Their Web site is at http://www.aboutscotland.com/theroyalscots/museum.html. They may be reached at: I am doing my research paper on the Edinburgh Vaults and am having a lot of trouble finding accurate information.

BWEA Best Practice Guidelines were revised in 2005 to include offshore considerations. Amongst these is the recommendation that all offshore projects should be sited at least 5 km offshore, although some sites built already are closer to shore than this. All of the 'Round 2' projects are at least 8 km offshore, hard to see on anything but a very clear day.

Although it is possible to build structures in water deeper than 30 m (for example the oil platforms in the North Sea), it is very expensive and is not economically viable at present for offshore wind turbines. Wind speeds tend to increase as you move offshore. This means that turbines built further offshore should capture more wind energy.

Yes very... I would forget about the sea horses, as far as fish go in a reef you don't really have that many fish just a few for highlight and algae management ON the algae on the back glass there is multiplying some sort of parasite. It is smaller than the head of a pin and there are hundreds of them. They are white and move in a jerky fashion, plus I can see that they are producing larvae.

Yes, we can visit an area that is on the UNESCO World Heritage List , for example on a daytrip from Amsterdam.

By the year 2030, the global average sea level is likely to be between 3 and 17 cm higher than the 1990 level. By 2100, sea level is projected to rise by approximately 9 to 88 cm, compared with 1990. The rate and magnitude of sea-level change will vary from place to place in response to coastline features, changes in ocean currents, differences in tidal patterns and sea-water density, and vertical movements of the land itself. In some areas, sea level may actually fall.

If the Earth's atmosphere warms, the upper layers of the oceans will also warm. Like most substances, water expands when heated. Expansion will raise sea level. Land-based ice in temperate regions such as South America and North America will melt more rapidly. Glaciers may retreat. Melting also contributes to increased sea level. The net effect on sea level rise from ice changes in Greenland and Antarctica is likely to be small. Overall, Antarctica is not warming significantly.

A few people think that human-level intelligence can be achieved by writing large numbers of programs of the kind people are now writing and assembling vast knowledge bases of facts in the languages now used for expressing knowledge. However, most AI researchers believe that new fundamental ideas are required, and therefore it cannot be predicted when human-level intelligence will be achieved.

Sea level is the level of the surface of the sea especially at its mean position midway between mean high and low water. A sea level center measures these highs and lows and then analyzes the collected data.(MORE)

Averaged over all land and ocean surfaces, temperatures have warmed about 1.35°F (0.75ºC) over the last century. Much of this warming—about 0.72°F (0.4°C)—has occurred since 1979. Because oceans tend to warm and cool more slowly than land areas, continents have warmed the most (about 0.7ºC or 1.26°F since 1979), especially over the Northern Hemisphere. The year 2006 was the warmest year in U.S.

The short answer is no, Death Valley as we know it today has always been separated from the sea by mountains. On the other hand, long before Death Valley formed, the region was seabed for hundreds of millions of years as the abundant layers of limestone, dolomite and marble prove.

Global mean sea level has been rising at an average rate of 1 to 2 mm/year over the past 100 years, which is significantly larger than the rate averaged over the last several thousand years. Projected increase from 1990-2100 is anywhere from 0.09-0.88 meters, depending on which greenhouse gas scenario is used and many physical uncertainties in contributions to sea-level rise from a variety of frozen and unfrozen water sources.

Sea level data are used to confirm the generation of a tsunami and to predict the tsunami hazard for locations where the waves have yet to strike. They are critical to the Warning Centers' ability to provide timely and accurate tsunami watches, warnings and cancellations.

IPCC (Inter-governmental Panel for Climate Change) that consists of governmental persons and world prominent scientists, estimates in its latest report that the global average sea level rose between 0.1 and 0.2 meters during the 20th century. And the report says that the global mean sea level is projected to rise by 0.09 to 0.88 meters between 1990 and 2100.

In many parts of the world, the coastal land is very flat, so even modest sea level rise can lead to substantial changes in coastlines. The images below, courtesy of Jeremy Weiss and Jonathan Overpeck, show how sea level rise would affect coastlines in susceptible areas (see their website). In some areas, a sea level rise of only 3 feet (1 meter) would cause inward retreat of coastlines by tens of miles or more.

Most instruction manuals require the pool to be with in an inch of level. For overall appearance and integrity of the pool that is a very good rule of thumb. There are certain conditions that would make a pool that is off level by more than an inch still safe. If the pool is in the ground with dirt packed around it the level is not a safety factor. The more sand or dirt cove the pool has on the inside and the more soil packed around the outside the more variance a pool can tolerate.

Click the i key and a box will open to show you your level progression. Be sure the cursor is not blinking in the chat window first. Or type /whois yourname.

The manufacturing process uses up to two inches, leaving only eight inches (jaw length). Most of the children who receive hairpieces from Locks of Love are little girls, and most want long hair. When we need to provide a hairpiece to a boy, we use some of the shorter lengths that have been separated by hand from each donated ponytail. Yes, hair that is short, gray, or otherwise unusable will be sold to help offset manufacturing costs.

Roncesvalles to Santiago is about 800 km i.e. 4-5 weeks walking or 2 weeks by bike. Seville to Santiago, on the Via de la Plata, is 1000 km, walkable in about 6 weeks. Le Puy to Roncesvalles is about 5 weeks walking, Vézelay similar. Paris to Santiago is 2000 km. Arles to Puente la Reina is about 900 km. For descriptions of all the routes, click here.