What Is Macquarie Island?

The Reef was declared a World Heritage site by UNESCO in 1981, as the world’s most extensive coral reef ecosystem, meeting 4 of the 10 possible criteria.

Rock Canyon is an excellent site for geologic research and has been investigated by geologists from around Utah and neighboring states. With outstanding extrusions of quartzite, tillite and limestone, it’s a favored destination for hikers, rock climbers and scientists. The quartzite is considered the most unique feature of Rock Canyon as it’s one of the few clear and distinct examples of the sedimentary processes involved with a shallow marine setting. The tillite beneath the quartzite draws attention to the ancient glaciers to the past. In conjunction with the active Wasatch Fault found at its doorstep, Rock Canyon is an important place in Utah for geologists.

Evidence of almost 100 of the stones has revealed without the need to excavate the site, due to remote sensing, ground-penetrating radar and geographical imaging technologies. These advancements in science and technology allow researchers to discover the historical monuments full extent. Fragments of bones, stones and the foundation pits in which they were situated have all been uncovered during excavations and technological mapping indicating the true size and importance the site was to the Neolithic

Rottnest Island, located off the coast of Western Australia greatly known for the 63 beaches and bay along with popular tourist mark. Most visitors of Rottnest are oblivious and unfamiliar with the history of the Island.

The Great Barrier Reef is known as one of the Seven Wonders of the World. It is believed to be one of the most incredible places on this earth. This reef is the largest living organism on this planet and the only living thing on earth visible from space (2011). The warm waters of the southwest Pacific Ocean are the perfect environments to create the world's largest system of coral reefs. The Great Barrier Reef is in such pristine condition that it was listed by the World Heritage Trust as a protected site and is therefore, managed by the Great Barrier Reef Marine Park Authority to ensure that its beauty is maintained for many travelers and sightseers (Edgar 2010). Due to the complexity of this natural phenomenon, human practices have led

Tourism in Australia has evolved over the years and continues to increase to this day, however it is the effects that tourists have the ability to place on the Southern Great Barrier Reef which are potentially threatening for, not only the reef of lady Elliot Island, however, the corals surrounding it. “International visitations within Australia alone reached 3.9 million visitors within the first 7 months of 2014, which was an increase of approximately 9.5%, a number which continues to rise” (Tourism Australia, 2015). However, with this increasing number, comes possible damaging effects to the surrounding reefs of Lady Elliot Island, possibly leading to the excessive damage of corals due to activities and infrastructure requirements

Surrounding the Great Barrier Reef are the aboriginal inhabitants and Torres Strait Islanders. Their connection goes back for 60,000 years. There are 70 tribes across the Great Barrier Reef relying on the reef but are experiencing major problems, pollution and mining.

Cronulla is a beachside suburb in southern Sydney, it is located 34.0574° S, 151.1522° E which is 26 kilometres south of the Sydney CBD (see figure 2). It is governed by the Sutherland Shire Council. Cronulla’s coastal environment is on the Kurnell Peninsula, which is made up of a tombolo. A tombolo is a sand spit connecting a rocky outcrop or island to the mainland. So this forms a barrier between Botany Bay and Bate Bay. The two areas of study visited were Wanda Beach and the Greenhills Beach development.

The Cronulla, Kurnell and Wanda region sites are ecologically and culturally significant. The Cronulla, Wanda and Kurnell areas are filled with beautiful beaches, magnificent

The human impact on the reef has caused a lot of damage and so in 1971 the City of Onkaparinga, State Government, Coast care groups and environmental organisations all had supported a decision to protect the reef. So the reef has now a reserved part which is protected and separated from the one open to tourists. The positive effect of human intervention has been creating this 300 ha of aquatic reserve to safe

Lacustrine deposits at profiles 13-6 and 13-5, located within the maar crater near its eastern wall, occur at elevations of 1921.5 ± 0.2 m and 1919.4 ± 0.2 m, respectively. The profile 13-6 deposits are ~25 m higher than the modern lake level (1895.9 m) and ~10 m higher than highstand deposits at ~1911 m previously documented and radiocarbon dated by Bradbury (1967) on the northeast flank of the west cinder cone. The ~1921.5 m lacustrine deposits in the eastern part of the crater thus appear to represent the highest documented level of ZSL. Although Bradbury (1967:Figure 13) apparently also documented the same lacustrine highstand deposits as we did at profiles 13-5 and 13-6, it appears he mapped them ~50 m west (and downslope) of their actual location. We were able to more accurately plot their location and elevation using a

Our planet is over 4.5 billion years old and yet we have only touched the surface of knowledge that it withholds. I am naturally very curious, so the mysteries of our planet have fascinated me. My enthusiasm in Geology grew when I was introduced to physical Geography at GCSE level and thoroughly enjoyed the topic of plate tectonics leading me to further pursue Geology at A level. My interest in Geology encouraged me to join the Liverpool Geological Society and attend several lectures.

“The old map suggests much of the Southern Ocean around Australia is mainly covered by clay blown off the continent, whereas our map shows this area is actually a complex patchwork of microfossil remains,” said study author Adriana Dutkiewicz, a sedimentologist at the University of Sydney in a statement. “Life in the Southern Ocean is much richer than previously thought.”

Kharg Island is located 25 km (16 mi) off the coast of Iran and 483 km (300 mi) northwest of the Strait of Hormuz. Administered by the adjacent coastal Bushehr Province, Kharg Island provides a sea port for the export of oil and extends Iranian territorial sea claims into the Persian Gulf oil fields. Located on Kharg Island is Kharg, the only city in the Kharg District. Once it was the world's largest offshore crude oil terminal and the principal sea terminal for Iranian oil. This area is located in a heavy transportation area and serves as the main transit point for most of the goods (e.g., crude oil, finished products and raw materials) to and from Iran.

Norfolk Island is a small Pacific Island, located on the east of Australia, northward New Zealand, and southward New Caledonia (In Wikipedia, The Free Encyclopedia, 2016). The island’s geographic coordinates are 29.02 S, 167.57 E; and the island has a marine sub-tropical climate (In Wikipedia, The Free Encyclopedia, 2016). Also, the island is an eroded Baltic rock, volcanic Island, and the island’s physical features include: rolling plains, evergreen pines, cold hardy plants, and a few palm trees (In Wikipedia, The Free Encyclopedia, 2016). The research contains the five geographic themes of Norfolk Island, including: culture region, cultural diffusion, cultural ecology, cultural interaction, and cultural