China Sample
California's costal ocean region is characterized with both positive and negative attributes. The California Coastal Region is along the coast of the Pacific Ocean. This area is a beautiful, desirable area to live in, causing real estate to be among the highest in the United States. In fact, this area was one of the fastest to recover after the great recession of 2008, due primarily to its natural beauty. In addition, the per capita income for families in the area is also usually higher than the general population in the country. This fact is intuitive as higher income families are those best able to afford the beauty and natural elements in which the California costal region offers. There are many rivers and streams that lead out to the ocean. The popular Redwood Forest is also within the vicinity of the costal region. There are beautiful mountains and sand dunes to enjoy. California Coastal Region has many delightful natural resources to enjoy (Skinner, 2006)
The major physical features and costal land forms of the region are varied and diverse. The region, contrary to popular belief is home to many mountain ranges and tectonic activity. In fact, pundits have argued that California, due to seismic activity could actually disconnect from the United States geographically. Tectonic and volcanic activity, occurring over the past 250 million years, created many of the coastal mountain ranges prevalent today. Both the Farallon and Channel Island systems are the result of similar geologic process. Tectonic activity has created the islands as tectonic plates collide against one another. This occurrence seemingly does nothing in regards to geographic creation. Over time however, as the plates continue to slide and collide with one another, islands begin to form. This is what has occurred throughout the cost of California as small fertile islands have been created through earthquakes another natural phenomenon.
Coastal streams and rivers, along with wind and rain, shape and tear down these mountains through erosion. The powerful, ceaseless waves of the Pacific also cut into the coast mountain ranges and carve vertical cliffs, terraces, and bluffs into the rock. These physical features are what create the massive ecosystem within the coast. Through erosion, natural rivers, streams, lakes, and ponds are formed. Much like the tectonic activity mentioned above, this occurs through natural means and gives rise to varying land forms. For example, erosion creates sand beaches; it creates fertile soil that supports many of the nation's most beloved animals and ecosystems. It also allows oak tress and other forms of foliage to live and prosper independent from human interference. Elsewhere along the California coast, debris from wave erosion and sand deposited by streams and rivers accumulates and forms California's sandy beaches. Inland, where wind-blown sand from the beaches collects, one can find fragile systems of coastal dunes, home to rare and unique wide life. Coastal rivers and streams meet with the salty waters of the Pacific and create the marshes and lagoons which constitute California's coastal wetlands. In other areas, abrasive sand and wave motion cut grooves and pockets into the rock and intertidal communities and tide pools form. And even below the Pacific's waters geologic forces act, through many of the same processes, on the sea floor. All of these occurrences help create many of the physical features and costal land forms that characterize the California costal region. Although many of these aspects have occurred through various means, they all constituted an ecosystem which is unique and unparalleled in regards to its diversity and intrinsic value (Beckey, 2006).
The coast's climate is very different in the northern coast and the southern coast. Dramatic changes in elevation and a variety of climatic zones contribute to a diversity of plant life in California's coastal mountains. Elevation in particular is key as air quality, atmospheric pressure, and overall weather are altered dramtically. As such species that live further below the mountains would have a difficult time surviving in the upper regions of the mountains. Likewise, species of plants and animals in the upper region would have difficulty living in the lower region as well. Heavy winter rainfall, summer fog, and moderate temperatures have produced redwood groves where 2,000-year-old trees tower more than 300 feet above the forest floor. This redwoods are the tallest trees known to man and can live for long periods of time. South of San Francisco Bay, the slopes of the Santa Cruz Mountains is covered with stands of redwood while the drier regions of the southern Coast Ranges are vegetated with oaks, pines, and chaparral. Again, this is due primarily to the varying climates that are predominate in each region. As precipitation decreases southward, in the central and southern Coast Ranges, stands of hardwoods including tanbark oak, coast live oak, big- leaf maple, and marine begin to outnumber conifers. On steeper slopes and exposed ridges where thin soils lose moisture rapidly, drought-resistant chaparral species such as chemise, manzanita, sage, and scrub oak take hold
One of the most notable islands within the region is Angel Island which was a conduit for immigration. The island...
Virgin.net/john.cletheroe/usa_can/usa/cascade.htm Early California history: An overview. Retrieved January 16, 2005 from Web site: http://memory.loc.gov/ammem/cbhtml/cbintro.html Introduction to a Sierra Nevada Gallery. The Sierra Nevada Gallery. Retrieved January 16, 2005 from Web site: http://www.sierranevadaphotos.com/intro.html Klamath Mountains. Encyclopedia Britannica. Retrieved January 16, 2005 from Web site: http://www.britannica.com/eb/article?tocId=9045718 Michaelsen, J. And Chamberlin, S. Queen Calafia slept here. University of California, Santa Barbara. Retrieved January 16, 2005 from Web site: http://www.geog.ucsb.edu/~joel/g148_f04/readings/intro_04.html Parsons, J.J. (1987). A geographer looks at the San
Trees cover nothing less than one-third of the earth's surface, and it is estimated that around 3 trillion trees exist worldwide. Forests are found in different climates and locations, and they exist in wet, dry, sweltering and bitterly climates. Each of these forests types have the natural peculiarities that allow them to develop in their respective climates (Motivans). Unfortunately, in the past few decades, there has been an enormous level
Trees cover nothing less than one-third of the earth's surface, and it is estimated that around 3 trillion trees exist worldwide. Forests are found in different climates and locations, they exist in wet, dry, sweltering and bitterly climates. Each of these forests types have the natural peculiarities that allow them to develop in their respective climate (Motivans). Unfortunately, in the past few decades, there has been an enormous level of
Oil was tucked deep in the belly of the earth and was often mixed with brine. It required innovations in drilling and refinery. In timber production, it demanded innovation in the felling of trees, sawing mills and processing of wood. California was the first place to have an offshore drilling station. Water had to be moved for long distances for hydroelectric power and irrigation. Technological innovations allowed all this
Coastal Animals Sea Turtles (SeaWorld, 2004) From a taxonomy perspective, sea turtles belong to the overall class of reptilia. The order is testudines. The suborder cryptodira also includes fresh water turtles. There are two families of sea turtles. Based on their carapaces, sea turtles are divided into two families: bony -- covered with horny scutes -- turtles and leatherback turtles. There are eight species of sea turtles: green Chelonia mydas, black Chelonia
Region of Megalopolis (urban area in Northern America) and its sub-Region of Nantucket (off Cape Cod) This paper describes the geographic region of Megalopolis (urban area in Northern America) and its sub-region of Nantucket (off Cape Cod). It also deals with the history of Nantucket and the causes that led to the formation of the megalopolis in northeastern USA. Megalopolis comes from the Greek words for 'very large' (Mega) and city
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