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5 themes of geography for new zealand
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Reasons why New Zealand is a Dangerous Place to Live
New Zealand is located in the southwest of the Pacific Ocean,
southeast of Australia. This beautiful country has many high lands,
huge rivers and mountains, which are steep, very jagged and glaciated.
There is plenty of ash over the North Island resulting from volcanic
eruptions.
What makes this amazing country so dangerous is that so many natural
hazards exist here. New Zealand situated right through the ring of
fire. This is a zone where frequent earthquakes and volcanic eruptions
happen. New Zealand's volcanoes occur by the Indo-Australian plate
going underneath the Pacific plate which melts causing the burst of
lava, and the treacherous volcano. There is a long string of volcanoes
here, some are extinct and some are active. This area is called the
subduction zone.
One big volcano, called White Island erupts every year. In Wellington
there is a volcano that is next to an enormous fault. This could erupt
at any time and if it does there will be disastrous results. 50
volcanoes surround the popular city of Auckland. In some places there
is so much molten rock that the volcano could go underwater. If the
water gets in, the whole city could be destroyed. Lake Taupo was
formed 3000 years ago by a mammoth volcanic eruption.
Another major natural hazard in New Zealand is the earthquakes. In
1931 Napia - South Island a massive earthquake hit this city. It
destroyed many homes and buildings.
The climate of the country is spectacular. When the wind, water and
warm air from Australia meet the cold air from Antarctica the air is
forced to rise above the Southern Alps causing immense rainfall. It is
known that 9m of rain falls every year in New Zealand. This amount of
rain is called RELIEF RAINFALL. This often results in floods.
It also the impact of man on the environment that makes it so
dangerous to live here. People have chopped down many trees which
reduces infiltration and increases run-off, which also causes
Although volcanoes are difficult to predict, geologists have made many efforts in order to caution the people of Orting and other surrounding towns of possible lahar slides. Residents have been made aware of emergency response plans and they know the proper precautions to take in the case of a volcanic activity emergency. Sirens have been put into place by the fire department and governing bodies of surrounding communities that detect volcanic activity and warn the community of ...
Mauna Loa is located on a hot spot in the Pacific Ocean. It is not near a plate boundary, in fact it is 3,200 km from the nearest plate boundary, and is situated in the middle of the Pacific tectonic plate. This is actually a rarity, as 90% of volcanoes are along a tectonic plate boundary. A hot spot occurs where long, stationary vertical pools of magma rise up and towards the plate. Movement of the tectonic plates above the hot spot created Mauna Loa, along with the other Hawaiian volcanoes. The older Hawaiian Islands were once above this stationary hot spot, but have been carried northwest by the slowly moving Pacific plate. As the plate moves, it carries the previously formed, older, volcanoes with it, creating a trail of younger, new volcanoes behind. The islands are lined up along the Hawaiian Ridge-Emperor Seamounts chain, which is 3,750 miles and includes Kauai, Maui, Oahu and Hawai’i, from north to south, respectively. There are around 80 volcanoes in this chain; most of them underwater, consequently the term seamount refer to submarine volcanoes. Three volcanoes of Hawai’i, Mauna Loa, Kilauea and Loihi seamount, are all currently sharing the Hawaiian hot spot. Although, recent evidence has shown that all three volcanoes use have separate plumbing systems to expel the lava from the pool of magma deep below them. It has also been suggested that Loihi is slowly moving Mauna Loa from the center of the island, thus shifting directly over the hot spot. The closer to the hot spot a volcano is, the more active it will be. The Hawaiian hot spot has laid down layers of lava, building up enormous islands from the ocean floor.
Over the centuries, the making of the Big Island as we know it today eventually entailed the growth and conjoining of six separate volcanoes, building all the way up from the seafloor, some 18,000 feet below the ocean’s surface. These volcanoes, from northwest to southeast, are named Mahukona, Kohala, Mauna Kea, Hualalai, Mauna Loa and Kilauea, and become younger as one moves north to south. Mahukona Volcano, just off the Big Island’s northwest coast, was the first volcano to start forming. Now submerged beneath the surface of the ocean because it is sinking into the Earth’s crust under its own vast weight, Mahukona is no longer visible. As the Pacific Plate slowly continued moving northwestward over the hotspot, the location of the rising magma moved relatively southeastward, and through time the rest of the Big Island volcanoes formed along that path.After Mahukona, Kohala Volcano, the precursor to today’s Kohala Mountain, erupted next. As Kohala Volcano emerged from the sea and joined with Mahukona, a much larger Big
The Hot Zone is a true story of how Bio-safety level 4 hot agents have affected the lives of different people. The first incident is about Charles Monet a water-pump machinist at a sugar factory in Kenya, who went exploring with a friend in Kitman Cave; sixteen days later he lay dead in an intensive care unit. He bled out from every orifice in his body, his kidneys and liver destroyed, partially liquefied, his insides were that of a corpse. The cause of death was undetermined. Ten days after treating Monet, Dr. Muskoe falls ill.. Monet had vomited a black, bloody coffee ground substance all over him. The vomit had gotten into his eyes and even into his mouth. After several futile attempts to cure and diagnose himself he finally seeks the help of his physician. After exploratory surgery yielded no diagnosis Muskoe's physician suspects a virus. He sends a sample of Muskoe's blood to the National Institute of Virology and to the CDC. Muskoe's blood is positive for the filovirus Marsburg, a deadly sister to Ebola virus. Muskoe miraculously survives.
Basalt forms due to the partial melting of the layer of the mantle called the asthenosphere. The asthenosphere is the plastic zone of the mantle beneath the rigid lithosphere. Mantle plumes coming from the mesosphere can cause the asthenosphere to melt with heat or even if pressure decreases, which is called decompression melting (Richard 2011). The magma that forms from this melting is mafic magma that solidifies once it reaches the earth’s surface and cools quickly. The above process mainly occurs mainly during intraplate igneous activity which is the main explanation for volcanic activity that occurs a long distance away from a plate boundary. If the tectonic plate above the mantle plume is moving it can create a string of volcanic activity such as in Hawaii. See Fig 2.
Every performance horse owner has a very rigorous exercise and feeding program. Today there are so many feed supplements that it is very easy to ensure your animal gets every nutrient it needs to perform at its very best. However, even with all these extra additives every horse needs the basics in their diets. Primarily roughage, for those people who do not have access to year-round pasture the alternative is hay.
The eruption of Kilauea continues to flow at two places in the park. The vent within Halema'uma'u Crater and the Pu'u'' vent. In conclusion, the trip to the Hawaii Volcanoes National Park should be an experience to remember. On this trip you will experience a cultural, creative, inspirational, and memorable theme. The Park has many visitors each year, to my knowledge the experience is unimaginable.
Occupier's Liability Objective The objective of this document is to outline the obligations of the RSPB, as occupier of property. The obligations are set out in two Occupier's Liability Acts 1957 and 1984, and are owed to persons who enter RSPB property either as licensed visitors, or as unlicensed trespassers. The document does not purport to cover every particular situation and those in any doubt should consult Legal and Compliance as to secure their own position. Overview The RSPB owns large quantities of real estate, including many public reserves. It also owns many offices to which employees have access.
Already this year the World Health Organization has reported over twenty outbreaks of various diseases ranging from Brazil to Australia (World Health Organization). Who predicts and deters these disease outbreaks from spreading? What processes are instilled to prevent such outbreaks from becoming epidemics and pandemics?
It is important for children and young people to develop their own strategies to protect themselves
Food hazards can be generally defined as a state or pollutant that may have the potential to cause disease. The issues of food hazards have become widely recognized internationally in the last decade. With modern technology, scientists have been able to identify foodborne diseases prompted by food hazards on a global scale and have acknowledged these hazards as a primary cause of morbidity (Friis, 2012). I chose to focus on food hazards, their significance, and their effect on a global scale because this is an issue that most people have, at some point, encountered throughout life. In my own life, I’ve experienced mild illness as a result of food that had been exposed to harmful bacteria, and have known individuals who faced more serious health
In regards to the natural hazard by earthquakes, nearly 1,500 earthquakes per year shake Japan and magnitudes larger than M 4 are routine; Japan was hit by 20 % of the most powerful earthquakes in known history. Currently almost 2,000 active faults are monitored in Japan, but, as previous earthquakes unfortunately proved, there must be many other, so far unknown, active faults in the region!
Currently New Zealand is finally recovering from the rapid economic growth it experienced in the mid-90s, now that the worst of the Asian financial crisis effects are over. New Zealand lost many export markets in Asia, but looked to the U.S. and European markets to replace the lost customers. The country remains dependent on trade due to its small size and isolation; price and access to foreign markets are a constant concern.
Any educational plain or public campaign designed should be considerate to the fact that our new hazards come with an increased uncertainty. Unlike a traditional threat our new hazard is implemented by a person with the ability to learn and take advantage of our mistakes. We should also be concerned with implanting an idea in the mind of a person that hopes to cause harm but just does not know how or what would achieve the greatest destruction. A challenge for any instructor will be avoiding our weakness while highlighting the strengths of the new hazards. Because the public is the focus of this education plain, I would focus the information provided in this program to information the public will need prior to, during and immediately after an attack related to the five new hazards, their targets and potential terrorists.