Google, The Top Tech Companie And World's Most Attractive Employer (Offices Around The World)

Founded - 1998

Founders - Larry Page and Sergey Brin

Incorporation - September 4, 1998

Initial public offering (NASDAQ) - August 19, 2004

The Google story begins in 1995 at Stanford University. Larry Page was considering Stanford for grad school and Sergey Brin, a student there, was assigned to show him around. By some accounts, they disagreed about nearly everything during that first meeting, but by the following year they struck a partnership. Working from their dorm rooms, they built a search engine that used links to determine the importance of individual pages on the World Wide Web. They called this search engine Backrub.

Soon after, Backrub was renamed Google (phew). The name was a play on the mathematical expression for the number 1 followed by 100 zeros and aptly reflected Larry and Sergey's mission “to organize the world’s information and make it universally accessible and useful.”

Over the next few years, Google caught the attention of not only the academic community, but Silicon Valley investors as well. In August 1998, Sun co-founder Andy Bechtolsheim wrote Larry and Sergey a check for $100,000, and Google Inc. was officially born. With this investment, the newly incorporated team made the upgrade from the dorms to their first office: a garage in suburban Menlo Park, California, owned by Susan Wojcicki (employee #16 and now CEO of YouTube). Clunky desktop computers, a ping pong table, and bright blue carpet set the scene for those early days and late nights. (The tradition of keeping things colorful continues to this day.)

Even in the beginning, things were unconventional: from Google’s initial server (made of Lego) to the first “Doodle” in 1998: a stick figure in the logo announcing to site visitors that the entire staff was playing hooky at the Burning Man Festival. In the years that followed, the company expanded rapidly hiring engineers, building a sales team, and introducing the first company dog, Yoshka. Google outgrew the garage and eventually moved to its current headquarters (a.k.a.“The Googleplex”) in Mountain View, California. The spirit of doing things differently made the move. 

The relentless search for better answers continues to be at the core of everything we do. Today, with more than 50,000 employees in 50 different countries, Google makes hundreds of products used by billions of people across the globe, from YouTube and Android to Smartbox and, of course, Google Search. Although we’ve ditched the Lego servers and added just a few more company dogs, our passion for building technology for everyone has stayed with us from the dorm room, to the garage, and to this very day.

Google is often ranked as one of the top tech companies to work for and with good reason. The company is extraordinarily employee-friendly.

On Fortune magazine's list of the best companies to work for, Google ranked first in 2007, 2008 and 2012 and fourth in 2009 and 2010. Google was also nominated in 2010 to be the world's most attractive employer to graduating students in the Universum Communications talent attraction index. Google's corporate philosophy includes principles such as "you can make money without doing evil," "you can be serious without a suit," and "work should be challenging and the challenge should be fun.

As a motivation technique, Google uses a policy often called Innovation Time Off, where Google engineers are encouraged to spend 20% of their work time on projects that interest them. Some of Google's newer services, such as Gmail, Google News, Orkut, and AdSense originated from these independent endeavors. In a talk at Stanford University, Marissa Mayer, Google's Vice President of Search Products and User Experience until July 2012, showed that half of all new product launches in the second half of 2005 had originated from the Innovation Time Off.

New employees are called "Nooglers," and are given a propeller beanie cap to wear on their first Friday.

In addition to a great array of benefits and employee perks, Google takes measures to ensure its employees work in extremely unique environments that are designed to foster creativity and out-of-the-box thinking. Additionally, it makes going to work a far more enjoyable experience when there are slides, bikes, basketball courts, ping pong tables and video games to enjoy. 

As it stands now, Google has offices across the globe, and each one of its major offices has its own unique vibe and design sensibility. That said, we’ve compiled some of the more intriguing photos of Google office photos from around the world. From the insane and creative layout of the company’s Zürich office to a rooftop mini-golf course in Toronto, Google’s offices are anything but boring.

Google's headquarters in Mountain View, California, is referred to as "the Googleplex", a play on words on the number googolplex and the headquarters itself being a complex of buildings. The lobby is decorated with a piano, lava lamps, old server clusters, and a projection of search queries on the wall. The hallways are full of exercise balls and bicycles. Many employees have access to the corporate recreation center. Recreational amenities are scattered throughout the campus and include a workout room with weights and rowing machines, locker rooms, washers and dryers, a massage room, assorted video games, table football, a baby grand piano, a billiard table, and ping pong. In addition to the recreation room, there are snack rooms stocked with various foods and drinks, with special emphasis placed on nutrition. Free food is available to employees 24/7, with the offerings provided by paid vending machines prorated based on and favoring those of better nutritional value.

Google's extensive amenities are not available to all of its workers. Temporary workers such as book scanners do not have access to shuttles, Google cafes, or other perks.

For more details =

•   Google Careers
•  Goole Official Websit 
•  Google Office Locations Around World 

La Tomatina ( The Tamato Fight), Valencia, Spain

La Tomatina is a festival that is held in the Valencian town of Buñol, a town located in the East of Spain 30 km / 19 miles from the Mediterranean, in which participants throw tomatoes and get involved in this tomato fight purely for entertainment purposes. Since 1945 it has been held on the last Wednesday of August, during the week of festivities of Buñol.

The festival is in honor of the town's patron saints, Luis Bertran and the Mare de Deu dels Desemparats (Mother of God of the Defenseless), a title of the Virgin Mary. The tomato fight (or La Tomatina) has been a strong tradition in Buñol since 1944 or 1945. No one is completely certain how this event originated, but there is one popular theory that disgruntled townspeople rioted and attacked city councilmen with tomatoes during a town celebration. Whatever did happen to begin the tradition, it was enjoyed so much that it was repeated the next year, and the year after that, and so on. Other theories include a food fight among friends, a juvenile class war between bare-footed Trotskyist macarras and upper class pijos from Madrid on summer vacation, a volley of tomatoes from bystanders at a carnival parade, a democratic protest against the city council and the ensuing aftermath of an accidental truck spillage. The holiday was banned in the Spanish State period under Francisco Franco for having no religious significance, but returned in the 1970s after his demise. In 1957, demand for the popular festival led to its becoming official, with certain rules and restrictions. These rules have gone through many modifications over the years.

Another important landmark in the history of this festival is the year 1975. From this year onward, "Los Clavarios de San Luis Bertrán" (San Luis Bertrán is the patron of the town of Buñol) organized the whole festival and brought in the tomatoes, which had previously been brought by the local people. Soon after this, in 1980, the town council took over responsibility for organizing the festival.

Since then, the number of participants has increased year after year. In 2002, in the month of August La Tomatina of Buñol was declared a Festivity of International Tourist Interest by the Secretary Department of Tourism due to its success. In 2013, town officials introduced an entry fee and limited the number of participants, citing concerns over safety.

 

At around 11am many trucks haul the bounty of tomatoes into the centre of the town, Plaza del Pueblo. The tomatoes come from Extremadura, where they are less expensive. Technically the festival does not begin until one brave soul has climbed to the top of a two-story high, greased-up wooden pole and reached the coveted ham at the top. In practice this process takes a long time and the festival starts despite no one reaching the meaty prize. The signal for the beginning of the fight is firing of water cannons, and the chaos begins. Once it begins, the battle is generally every man for himself.

After an one hour the fighting ends. At this point, no more tomatoes can be thrown. The cleaning process involves the use of fire trucks to spray down the streets, with water provided from a Roman aqueduct. The authorities seem more concerned with cleaning the town than cleaning the visitors, so some people find water at the Bunol River to wash themselves, although some kind residents will hose passers-by down. Once the tomato pulp is flushed, the ground is clean due to the acidity of the tomato. 

Since 2013, the capacity of La Tomatina is regulated by selling tickets for the event, a measure that "guarantees the sustainability of the party, better security and  fun for the attenders [sic]”. In 2015, it is estimated that almost 145000 kg of tomatoes were thrown. As with previous years, participants of many nationalities are expected.

The Rules of La Tomatina

•     Do not bring bottles or hard objects as they can cause accidents.
  
•     Do not rip other people's T-shirts
•     You must squash the tomatoes before throwing them as this reduces the impact
•     Ensure you keep a safe distance from the lorries
•     As soon as you hear the second shot, you must stop throwing tomatoes

For more details - official website of La Tomatina

The Eisriesenwelt (World of the Ice Giants), Werfen, Austria

The Eisriesenwelt (German for "World of the Ice Giants") is a natural limestone and ice cave located in Werfen, Austria, about 40 km south of Salzburg. The cave is inside the Hochkogel mountain in the Tennengebirge section of the Alps. It is the largest ice cave in the world, extending more than 42 km and visited by about 200,000 tourists every year.

The Tennengebirge mountains were formed during the late Tertiary period, during the Würm glaciation period of the Pleistocene. The mountain range, one of the massifs in the Austrian Alps, is the largest karst plateau in the Salzburger Alps, and the Eisriesenwelt is located at the rim of this plateau. Although the cave has a length of 42 km, only the first kilometer, the area that tourists are allowed to visit, is covered in ice. The rest of the cave is formed of limestone.

Eisriesenwelt was formed by the Salzach river, which eroded passageways into the mountain. The ice formations in the cave were formed by thawing snow which drained into the cave and froze during winter.

Since the entrance to the caves is open year-round, chilly winter winds blow into the cave and freeze the snow inside. In summer, a cold wind from inside the cave blows toward the entrance and prevents the formations from melting.

The first official discovery of Eisriesenwelt was by Anton Posselt, a natural scientist from Salzburg, in 1879, though he only explored the first two hundred meters of the cave. Before his discovery, the cave was known only to locals, who, believing that it was an entrance to Hell, refused to explore it. In 1880, Posselt published his findings in a mountaineering magazine, but the report was quickly forgotten.

Alexander von Mörk (de), a speleologist from Salzburg, was one of the few people who remembered Posselt's discovery. He led several expeditions into the caves beginning in 1912, which were soon followed by other explorers. Von Mörk was killed in World War I in 1914, and an urn containing his ashes is inside a niche in the cave. In 1920, a cabin for the explorers, Forscherhütte, was built and the first routes up the mountain were established. Tourists began to arrive soon after, attracted by the cave's sudden popularity. Later another cabin, the Dr. Oedl House, and paths from Werfen and Tänneck were constructed.

In 1955 a cable car was built, shortening the 90-minute climb to 3 minutes. Today the Eisriesenwelt cave is owned by the National Austrian Forest Commission (de), which has leased it to the Salzburg Association of Cave Exploration since 1928. The Forest Commission still receives a percentage of the entrance fees.

The cave is open from May 1 to October 26 every year. Its operating hours are 9:00 a.m. to 4:30 p.m. in July and August and 9:00 a.m. to 3:30 p.m. in May/June and September/October. Temperatures inside the cave are usually below freezing, and warm clothing is recommended. Photography is not permitted once visitors are inside the cave.

The tour begins at the entrance to the cave, and continues inwards to Posselt Hall, a large room with a stalagmite called Posselt Tower in the centre. Past the Posselt Tower, one encounters an ashen cross on the wall of the cave, marking the farthest point of exploration of Anton Posselt. From there one can see the Great Ice Embankment, a massive formation that rises to a height of 25 metres and represents the area of greatest ice growth. Next is Hymir's Castle, named after a giant in Norse mythology. Here stalactites create a formation called Frigga's Veil, or the Ice Organ.

Next on the tour is the Alexander von Mörk Cathedral, one of the largest rooms in the cave and the final resting place of von Mörk's ashes. The final stop on the tour is the Ice Palace, a kilometre into the cave and 400 metres underground. From here, visitors must turn around and walk back through the caves to reach the entrance. The round-trip tour through the cave takes around one hour and 15 minutes.

The Richat Structure (Eye of the Sahara), Sahara Near Ouadane, West–Central Mauritania

The Richat Structure, also known as the Eye of the Sahara and Guelb er Richat, is a prominent circular feature in the Sahara near Ouadane, west–central Mauritania.

The Richat Structure is a deeply eroded, slightly elliptical dome with a diameter of 40 kilometers (25 mi). The sedimentary rock exposed in this dome ranges in age from Late Proterozoic within the center of the dome to Ordovician sandstone around its edges. The sedimentary rocks comprising this structure dip outward at 10°–20°. Differential erosion of resistant layers of quartzite has created high-relief circular cuestas. Its center consists of a siliceous breccia covering an area that is at least 30 kilometers (19 mi) in diameter.

Exposed within the interior of the Richat Structure are a variety of intrusive and extrusive igneous rocks. They include rhyolitic volcanic rocks, gabbros, carbonatites and kimberlites. The rhyolitic rocks consist of lava flows and hydrothermally altered tuffaceous rocks that are part of two distinct eruptive centers, which are interpreted to be the eroded remains of two maars. According to field mapping and aeromagnetic data, the gabbroic rocks form two concentric ring dikes. The inner ring dike is about 20 m in width and lies about 3 km from the center of Richat Structure. The outer ring dike is about 50 m in width and lies about 7 to 8 km from the center of this structure. Thirty-two carbonatite dikes and sills have been mapped within the Richat Structure. The dikes are generally about 300 m long and typically 1 to 4 m wide. They consist of massive carbonatites that are mostly devoid of vesicles. The carbonatite rocks have been dated as having cooled between 94 and 104 million years ago. A kimberlitic plug and several sills have been found within the northern part of the Richat Structure. The kimberlite plug has been dated to around 99 million years old. These intrusive igneous rocks are interpreted as indicating the presence of a large alkaline igneous intrusion that currently underlies the Richat Structure and created it by uplifting the overlying rock.

Spectacular hydrothermal features are a part of the Richat Structure. They include the extensive hydrothermal alteration of rhyolites and gabbros and a central megabreccia created by hydrothermal dissolution and collapse. The siliceous megabreccia is at least 40 m thick in its center to only a few meters thick along its edges. The breccia consists of fragments of white to dark gray cherty material, quartz-rich sandstone, diagenetic cherty nodules, and stromatolitic limestone and is intensively silicified. The hydrothermal alteration, which created this breccia, has been dated to have occurred about 98.2 ± 2.6 million years ago using the 40Ar/39Ar method.

Initially interpreted as an asteroid impact structure because of its high degree of circularity, the Richat Structure is now regarded by geologists as a highly symmetrical and deeply eroded geologic dome. After extensive field and laboratory studies, no credible evidence has been found for shock metamorphism or any type of deformation indicative of a hypervelocity extraterrestrial impact. While coesite, an indicator of shock metamorphism, had initially been reported as being present in rock samples collected from the Richat Structure, further analysis of rock samples concluded that barite had been misidentified as coesite. In addition, the Richat Structure lacks the annular depression that characterizes large extraterrestrial impact structures of this size. Also, it is quite different from large extraterrestrial impact structures in that the sedimentary strata comprising this structure is remarkably intact and "orderly" and lacking in overturned, steeply dipping strata or disoriented blocks. A more recent multianalytical study on the Richat megabreccias concluded that carbonates within the silica-rich megabreccias were created by low-temperature hydrothermal waters, and that the structure requires special protection and further investigation of its origin.

For More Details - Richat Structure