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Toze: To pull violently; to touse.

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Toze soils

The Toze soils are on moderately sloping to moderately steep hillside slopes and alluvial fans, usually in pockets. They formed in alluvium from limestone, shale and dolomite. These soils occur at elevations of 7,500 to 9,000 feet in a moist subhumid climate. Mean annual air temperature ranges from 35 to 45 degrees F. Mean summer air temperature is 53 to 57 degrees F. Average annual precipita-tion ranges from 25 to 30 inches. Frost-free period is 80 to 90 days.
 

Limestone is a sedimentary rock composed largely of the mineral calcite (calcium carbonate: CaCO3). Limestone often contains variable amounts of silica in the form of chert or flint, as well as varying amounts of clay, silt and sand as disseminations, nodules, or layers within the rock. The primary source of the calcite in limestone is most commonly marine organisms. These organisms secrete shells that settle out of the water column and are deposited on ocean floors as pelagic ooze or alternatively is conglomerated in a coral reef (see lysocline for information on calcite dissolution). Secondary calcite may also be deposited by supersaturated meteoric waters (groundwater that precipitates the material in caves). This produces speleothems such as stalagmites and stalactites. Another form taken by calcite is that of oolites (oolitic limestone) which can be recognized by its granular appearance. Limestone makes up about 10% of the total volume of all sedimentary rocks .

Calcite can be either dissolved by groundwater or precipitated by groundwater, depending on several factors including the water temperature, pH, and dissolved ion concentrations. Calcite exhibits an unusual characteristic called retrograde solubility in which it becomes less soluble in water as the temperature increases.

When conditions are right for precipitation, calcite forms mineral coatings that cement the existing rock grains together or it can fill fractures.

Karst topography and caves develop in carbonate rocks due to their solubility in dilute acidic groundwater. Cooling groundwater or mixing of different groundwaters will also create conditions suitable for cave formation.

Coastal limestones are often eroded by organisms which bore into the rock by various means. This process is known as bioerosion. It is most common in the tropics, and it is known throughout the fossil record (see Taylor and Wilson, 2003).

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Iron impregnations in limestone
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A stratigraphic section of Ordovician limestone exposed in central Kentucky, USA. The less-resistant and thinner beds are composed of shale
Pure limestone is almost white. Because of impurities, such as clay, sand, organic remains, iron oxide and other materials, many limestones exhibit different colors, especially on weathered surfaces. Limestone may be crystalline, clastic, granular, or massive, depending on the method of formation. Crystals of calcite, quartz, dolomite or barite may line small cavities in the rock. Folk and Dunham classifications are used to describe limestones more precisely.

Travertine is a banded, compact variety of limestone formed along streams, particularly where there are waterfalls and around hot or cold springs. Calcium carbonate is deposited where evaporation of the water leaves a solution that is supersaturated with chemical constituents of calcite. Tufa, a porous or cellular variety of travertine, is found near waterfalls. Coquina is a poorly consolidated limestone composed of pieces of coral or shells.

During regional metamorphism that occurs during the mountain building process (orogeny) limestone recrystallizes into marble.

Limestone is a parent material of Mollisol soil group.
Limestone landscape

Main article: Karst topography

Limestone is partially soluble, especially in acid, and therefore forms many erosional landforms. These include limestone pavements, pot holes, cenotes, caves and gorges. Such erosion landscapes are known as karsts. Limestone is less resistant than most igneous rocks, but more resistant than most other sedimentary rocks. Limestone is therefore usually associated with hills and downland and occurs in regions with other sedimentary rocks, typically clays.

Bands of limestone emerge from the Earth's surface in often spectacular rocky outcrops and islands. Examples include the Burren in Co. Clare, Ireland; the Verdon Gorge in France; Malham Cove in North Yorkshire and the Isle of Wight[1], England; on Fårö near the Swedish island of Gotland, the Niagara Escarpment in Canada/USA, Notch Peak in Utah, and the Ha Long Bay National Park in Vietnam.

Unique habitats are found on alvars, extremely level expanses of limestone with thin soil mantles. The largest such expanse in Europe is the Stora Alvaret on the island of Oland, Sweden.

Huge quarries in northwestern Europe, such as those of Mount Saint Peter (Belgium/Netherlands), extend for more than a hundred kilometers.
Uses of limestone
Courthouse built of limestone in Manhattan, Kansas
Limestone is especially popular in architecture, and many landmarks around the world, especially in North America and Europe, are made primarily of the material. So many buildings in Kingston, Ontario, Canada were constructed from it that it is nicknamed the 'Limestone City'. Limestone is readily available and relatively easy to cut into blocks or more elaborate carving. It is also long-lasting and stands up well to exposure. However, it is a very heavy material, making it impractical for tall buildings. It is also quite expensive.

Limestone was most popular in the early 20th and late 19th centuries. Train stations, banks and other structures from that era are normally made of limestone. Limestone is used as a facade on some skyscrapers, but only in thin plates for covering rather than solid blocks. In the United States, Indiana, most notably the Bloomington area, has long been a source of high quality quarried limestone, called Indiana limestone. Many famous buildings in London are built from Portland limestone.

Limestone was also a very popular building block in the Middle Ages in the areas where it occurred since it is hard, durable, and commonly occurs in easily accessible surface exposures. Many medieval churches and castles in Europe are made of limestone. Beer stone was a popular kind of limestone for medieval buildings in southern England.
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A limestone plate with a negative map of Moosburg in Bavaria is prepared for a lithography print
Limestone and marble are very reactive to acid solutions, making acid rain a significant problem. Many limestone statues and building surfaces have suffered severe damage due to acid rain. Acid-based cleaning chemicals can also etch limestone, which should only be cleaned with a neutral or mild alkaline-based cleaner.

Other uses include

* The manufacture of quicklime (calcium oxide) and slaked lime (calcium hydroxide);
* Cement and mortar;
* Pulverized limestone is used as a soil conditioner to neutralize acidic soil conditions;
* Crushed for use as aggregate—the solid base for many roads;
* Geological formations of limestone are among the best petroleum reservoirs;
* As a reagent in desulfurizations;
* Glass making;
* Toothpaste;
* Added to bread as a source of calcium

Are you interested in mult-player online internet games? Such as runescape and neopets?Internet Game Online-games, tips, cheats and kids forumsAnother good forum is the Internet Junction For Gamers IJFG.COM Internet Junction For Gamers, Runescape Market and More IJFG.COM Jokes, Pranks, Runescape and other cool games at IJFG.COM. RuneScape is set in a medieval fantasy world, similar to "Guild Wars" or "EverQuest", where players control character representations of themselves. As with most massive multiplayer online roleplaying games (MMORPG), there is no overall objective or end to the game. Players explore, form alliances, perform optional tasks, and complete quests for rewards and to build character's skills.

RuneScape has often been one of the top massive online role playing games. It is a unique game. But, with a unique game, comes unique players. Players get bored, and then try to develop cheats....autos or bots that will help them achieve success in their beloved games of Runescape 2.

RuneScape is a virtual world which is divided into two part: Members Areas and Non-Members areas. People who pay to play (p2p), receive access to the special areas. They also have access to the free areas. The members' places are much larger, offer "better" items for the gameplay of rs2, and much, much more. The character that you create when you first start playing runescape, moves around the game on foot; either by running, or walking. Players are challenged to their utmost skills by fighting new monsters, completing difficult quests, and manipulating marketing. As Runescape 2 is an RPG (Role playing game), there is no set path a person must take to play rs. They can choose what to do, and when, whether it be training their money-making skills, or fighting another player. Players usually interact with each other by chatting through public chat, or private chat.Internet Junction For Gamers, Runescape Market and More IJFG.COM IJFG.com was a runescape 2 based site. They have now, however, taken another look....

Of course the king of all game cheating websites is trick the trik (otherwise known as RPG Cheats Site), where you can find cheat forums, mmorpg topsite, arcade games and any mmo game related topics.

The master of massive multiplayer online role-playing games (MMORPG) cheats can be found at Trik.com Trik.com; this site is one of the best today. The forum section, Trik.com forum, originally came from IJFG.com (Internet Junction For Gamers) , which was one of the best websites that discussed various gamers' issues. The full name was Internet Junction For Gamers, Runescape Market and More. This site had Jokes, Pranks, RuneScape and other cool games. RuneScape is set in a medieval fantasy world, similar to "Guild Wars" or "EverQuest," where players control character representations of themselves. As with most MMORPG, there is no overall objective or end to the game. Players explore, form alliances, perform optional tasks, and complete quests for rewards and to build characters' skills.

Trik.com continues IJFG.com's success, but Trik.com has more to offer. Trik Topsite can be found at Trik Topsite; the TopSite is a great addition if you want to find the best MMO RPG site(s) or raise your site in the rankings. Trik.com also has a viciously competitive Arcade. If you want to be the #1 Arcade on Trik, then come prove yourself at Trik.com arcade: Trik arcade.  Trik.com ?Trik.com/topsite ?Trik.com/forum/arcade.php

With the rising popularity of commercial MMORPG games came the desire from ardent players of these games to run their own servers beside the ones run by the game's creator. Since the original server software is not usually available, the behavior of the server has to be re-engineered. This can be done by analyzing the data stream with the original server, or by disassembling and analyzing the client which is available.

Ultima Online was one of the first large MMORPGs. Due to its openness in implementation, server emulators arose very quickly, even during the beta stage of development. The destination to which the client connects was changeable by simply editing a text file. In beta stage the client-server data stream was not encrypted yet. The term server emulator became known through Ultima Online server reimplementation such as UOX, which was the pioneer. Many forks and reimplementations followed UOX, because its source code was released under the GNU General Public License relatively early. RunUO is today the most widely used UO-server emulator. After RuneScape implemented anti-cheating measures, many gamers left and started their own private servers. The best place to discuss the private server is at Trik- The Master of Private Server.
 

Another useful site is Rune Web ruwb.com . This site is about more serious RuneScape gold trading, account exchange, gold for real life cash and many services. It includes tips on how to avoid getting lured/scammed while using the marketplace. For programming, visual basics, java, C/C++, scar and all other languages such as PHP, HTML, ASP, Delphi. There are also sections for graphics talents, plus many cool videos and fun stuff.

A defining moment in internet gaming history was when a group of gamers called (hygo 7) decided to start an ultimate game forum, which they named hygo.com. It has the best financial backing, the friendliest game community, and the highest quality of information. Currently Hygo.com has entered a new phase...Hygo.com is offering the best private server game. With thousands of members, Hygo.com is your next place to visit, as they have an amazing game with a community and economy. Hygo.com - The Online Adventure Game. is definitely one of the top sites you want to join right now!

EZud is another popular site. ezud.com. It has the best runescape bug abuse, bugs and trik. ezud.com - The runescape bugs. is definitely one of the best sites you want to join right now!

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