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  1. How did the Pacific Ocean get its name? › facts › pacific

    Explorer Ferdinand Magellan named the Pacific Ocean in the 16th Century. Covering approximately 59 million square miles and containing more than half of the free water on Earth, the Pacific is by far the largest of the world's ocean basins.

  2. Ocean Pacific - Wikipedia › wiki › Ocean_Pacific

    History The first "Ocean Pacific" trademark brand was started by John Smith in the 1960s as a surfboard brand, which he sold out of his shop, North County Ding Repair. Later, Fred Ryan purchased North County Ding Repair from John Smith along with the Ocean Pacific surfboard label.

  3. The Pacific Ocean—facts and information › article › pacific-ocean

    Mar 04, 2019 · The name Pacific is a version of pacify or peaceful. It was named by the explorer Ferdinand Magellan in 1520 as he sailed through a calm patch of water on the ocean. Despite its name, the Pacific...

  4. Ocean Pacific Apparel Designs, 1979 – 1989 › 2018/07/31 › ocean-pacific

    Jul 31, 2018 · Ocean Pacific was founded in 1972 by Jim Jenks, a San Diego-based surfboard maker and former sportswear rep.

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    • Stages of Pier Rebirth
    • Building Pacific Ocean Park
    • A Grand Opening
    • Pacific Ocean Park Attractions
    • Eventual Decline

    The story of the Pier itself begins long before the opening of the POP. The Pier had many rebirths over the 20th century, due in large part to several fires that devastated the structure. The Pier first opened as the Million Dollar Pierin 1911—this incarnation of the space was short-lived though, as a fire burned it to the ground just fifteen months later. The Pier and attractions were reconstructed for a new opening in 1913 and renamed to Pickering Pierin 1919 when Ernest Pickering purchased it and expanded the land by 400,000 square feet. His expansion brought on five new rides and kept local business owners and concessionaires happy. A 1920 re-opening saw 85,000 visitors on the first weekend, but within three years, another fire left the Park in shambles. Later, the Pier was purchased and rebuilt by Charles Lick as Ocean Park Pier. In 1925, the Pier re-opened for business and flourished for a number of years, undergoing several renovations and improvements. Over time, however, re...

    Purchased in 1956 by CBS and Los Angeles Turf Club, Ocean Park Pier underwent two years of renovations before re-opening as the beloved sea-themed Pacific Ocean Park. When CBS and Los Angeles Turf Club first acquired the Pier’s lease, they proposed a $10 million investment in a nautical-themed park that would compete with Disneyland. In order to make this happen, they hired top-notch amusement park designers and renowned Hollywood special effects artists. New, innovative attractions were created for the Park by over 80 people, who worked on the project for more than a year. Since competing with Disney was an expensive venture, POP owners decided to use a Disney-inspired strategy, procuring corporate sponsors to split some of the exhibit costs. Additionally, they opted to repair and refurbish existing structures and integrate old attractions into the new design. Some of these historic attractions featured at POP included the merry-go-round, fun house, and roller coaster. When it open...

    When it finally opened to the public on Saturday, July 28, 1958, POP drew a crowd of nearly 20,000 people and dozens of Hollywood celebrities. The second day saw nearly double the attendance with 37,262 guests—enough to cause significant traffic jams in the area. Famously, POP outperformed Disneyland in visitor numbers during its first week. Entering the Park was a spectacle in its own right. Visitors entered the Park through Neptune’s Kingdom, descending a submarine elevator to the oceanic corridors below and emerging at a large sea tank display with sharks and other fish. Visitors could see a massive diorama that featured some of the other local sea life, like artificial turtles, manta rays, and sharks glided by over coral reefs and hanging seaweed. Getting into the Park cost ninety cents for adults, with a slightly discounted rate for children. The fee included access to Neptune’s Kingdom, the Sea Circus, and the Westinghouse Enchanted Forest exhibit, but rides and other attracti...

    There were several impressive featuresthat attracted visitors to Pacific Ocean Park during its heyday. The Westinghouse Enchanted Forest and Nautilus Submarine Exhibit were major draws for the Park, even including a 150-foot model of the atomic reactor section of a former submarine. The Sea Circus, which featured dolphin and sea lion shows, was another popular attraction, and the auditorium was home to major rock shows including Ritchie Valens, Sam Cooke, The Beach Boys, and Pink Floyd. There were also two dining and shopping areas for visitors to enjoy meals and hunt for souvenirs. As for rides, POP had a roller coaster, two Ferris wheels, and an artistic carousel, as well as popular attractions like the Flying Dutchman and Deepest Deep, where riders took a fake submarine ride with mermaids and other sea life. Like many amusement parks, simple carnival rides like bumper cars, and a tilt-a-whirl also provided hours of fun to visitors.

    POP’s popularity lasted about a decade before its closing in 1967. The Park’s second season was worse than the first, and the owners closed it for winter, later selling the property for $10,000,000. The sixties saw rides left in disrepair and a decline in the safety of the surrounding neighborhood. A change in ticket sales to one general admission price without separate ride tickets also contributed to financial trouble. Even bringing in money up front, there were high overhead costs which caused maintenance to fall by the wayside. After changes in ownership and management, POP had a successful 1964 season. However, the city of Santa Monica began its Ocean Park urban renewal project soon after, which led to construction and demolitions near the Pier. The spate of street closures near the Park that resulted from this initiative eventually put POP in dire financial straits. By 1967, POP’s creditors acted on several months of non-payments, forcing it into involuntary bankruptcy. The Pa...

  6. History Of The Ocean ~ MarineBio Conservation Society › oceans › history
    • Introduction
    • Distribution
    • Classification
    • Scope
    • Formation
    • Composition
    • Geology

    The presence of large amounts of liquid water makes our planet unique. Most other planets have very little water, and on those that do, the water exists only as perpetually frozen ice or as vapor in the atmosphere. The earth, on the other hand, is very much a water planet. The ocean covers most of the globe and plays a crucial role in regulating our climate and atmosphere. Without water, life itself would be impossible.

    Our ocean covers 72% of the earths surface. It is not distributed equally with respect to the Equator. About two-thirds of the earths land area is found in the Northern Hemisphere, which is only 61% ocean. About 80% of the Southern Hemisphere is ocean.

    The ocean is traditionally classified into four large basins. The Pacific is the deepest and largest, almost as large as all the others combined. The Atlantic Ocean is a little larger than the Indian Ocean, but the two are similar in average depth. The Arctic is the smallest and shallowest. Connected or marginal to the main ocean basins are various shallow seas, such as the Mediterranean Sea, the Gulf of Mexico and the South China Sea.

    Though we usually treat the oceans as four separate entities, they are actually interconnected. This can be seen most easily by looking at a map of the world as seen from the South Pole. From this view it is clear that the Pacific, the Atlantic and Indian oceans are large branches of one vast ocean system. The connections among the major basins allow seawater, materials, and some organisms to move from one ocean to another. Because the oceans are actually one great interconnected system, oceanographers often speak of a single world ocean. They also refer to the continuous body of water that surrounds Antarctic as the Southern Ocean.

    The earth and the rest of the solar system are thought to have originated about 4.5 billion years ago from a cloud or clouds of dust. This dust was debris remaining from a huge cosmic explosion called the big bang, which astrophysicists estimate occurred about 15 billion years ago. The dust particles collided with each other, merging into larger particles. These larger particles collided in turn, joining into pebble-sized rocks that collided to form larger rocks, and so on. The process continued, eventually building up the earth and other planets. So much heat was produced as the early earth formed that the planet was probably molten. This allowed materials to settle within the planet according to their density. Density is the weight, or more correctly, the mass, of a given volume of a substance. Obviously, a pound of styrofoam weighs more than an ounce of lead, but most people think of lead as heavier than styrofoam. This is because lead weighs more than styrofoam if equal volumes of the two are compared. In other words, lead is denser than styrofoam. The density of a substance is calculated by dividing its mass by its volume. If two substances are mixed, the denser material will tend to sink and the less dense will float. During the time that the young earth was molten, the densest material tended to flow toward the center of the planet, while lighter materials floated toward the surface. The light surface material cooled to make a thin crust. Eventually, the atmosphere and oceans began to form. If the earth had settled into orbit only slightly closer to the sun, the planet would have been so hot that all the water would have evaporated into the atmosphere. With an orbit only slightly farther from the sun, all the water would be perpetually frozen. Fortunately for us, our planet orbits the sun in a narrow zone in which liquid water can exist. Without liquid water, there would be no life on earth.

    The earth is composed of three main layers: the iron-rich core, the semiplastic mantle and the thin outer crust. The crust is the most familiar layer of earth. Compared to the deeper layers it is extremely thin, like a rigid skin floating on top of the mantle. The composition and characteristics of the crust differs greatly between the oceans and the continents. The characteristics of seawater are due both to the nature of pure water and to the materials dissolved in it. The solids dissolved in seawater come from two main sources. Some are produced by the chemical weathering of rocks on land and are carried to sea by rivers. Other materials come from the earths interior. Most of these are released into the ocean at hydrothermal vents. Some are released into the atmosphere from volcanoes and enter the ocean in rain and snow. Seawater contains at least a little of almost everything, but most of the solutes or dissolved materials, are made up of a surprisingly small group of ions. In fact, only six ions compose over 98% of the solids in seawater. Sodium and chloride account for about 85% of the solids, which is why seawater tastes like table salt. The salinity of the water strongly affects the organisms that live in it. Most marine organisms, for instance, will die in fresh water. Even slight changes in salinity will harm some organisms.

    The geological distinction between ocean and continents is caused by the physical and chemical differences in the rocks themselves, rather than whether or not the rocks happen to be covered with water. The part of earth covered with water, the ocean, is covered because of the nature of the underlying rock. In the years after World War II, sonar allowed the first detailed surveys of large areas of the sea floor. These surveys resulted in the discovery of the mid-oceanic ridge system, a 40,000 mile continuous chain of volcanic submarine mountains and valleys that encircle the globe like the seams of a baseball. The mid-oceanic ridge system is the largest geological feature on the planet. At regular intervals the mid-ocean ridge is displaced to one side or the other by cracks in the earths crust known as transform faults. Occasionally the submarine mountains of the ridge rise so high that they break the surface to form islands, such as Iceland and the Azores. The portion of the mid-ocean ridge in the Atlantic, known as the Mid-Atlantic Ridge, runs right down the center of the Atlantic Ocean, closely following the curves of the opposing coastlines. The ridge forms an inverted Y in the Indian Ocean and runs up the eastern side of the Pacific. The main section of ridge in the eastern Pacific is called the East Pacific Rise. Surveys also revealed the existence of a system of deep depressions in the sea floor called trenches. Trenches are especially common in the Pacific.

  7. Op - Ocean Pacific › op-uo

    Op was the first company to successfully translate the surfing lifestyle into a comprehensive fashion idea by focusing on the west coast youth scene

  8. Jan 29, 2021 · Highway 1 is best known for the Southern California portion designated the Pacific Coast Highway, which provides drivers with gorgeous views of the Pacific Ocean. ... the history of Highway 1 ...

  9. Tale of Two Haystack Rocks on Oregon Coast › news › haystacks120212_1123

    Pacific City's is a tad higher than the one at Cannon Beach, by more than 100 feet. ... until they reached the ocean. These are known as the Columbia Basalts, since they created the Columbia Gorge ...

  10. The Ocean Cleanup says it could rid the GPGP of 50% of its waste in five years. Conventional methods of clearing the water, like vessels and nets, would take vast sums of money and thousands of years. The area is the biggest ocean garbage patch on the planet, but it’s just one of five around the world’s major ocean gyres.

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