Coastal Uplift in New Zealand

We use a pair of Geranium Gamma Detectors to measure the levels of the Cs and Pb isotopes in cores. The presence of Cs preserved in the sediments is associated with nuclear weapon testing, and its initiation is interpreted to correspond to around We use the peak trace of Cs to determine the stratigraphic interval that was deposited in Pb activity within sediment can be used to estimate accretion rates. Pb is a product of the uranium-decay series where Ra within the crust decays to Rn A fraction of the Rn enters the atmosphere where it in turn decays to Pb, and then quickly precipitates out of the atmosphere, is deposited at the surface, and decays with a half-life of Both isotopes when coalescing with raindrops, will fall to the atmosphere and be absorped and adsorped by plant matter in a marsh. As sea level rises, the sediments accumulate vertically covering older sediments and seasonal plant matter.

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We present an overview on different environmental zones within coastal areas and summarise the physical basis behind the three most important methods that are available to date Holocene coastal sediments. Besides radiocarbon and uranium series dating, Optically Stimulated Luminescence O sl has increasingly been applied for dating in coastal settings over the past decade.

This is illustrated by a number of case studies showing that O sl can be applied to sediments from almost any kind of coastal environment, covering a potential dating range from some years up to several hundred thousand years. O sl dating may hence be the method of choice for deciphering natural environmental change along coasts as well as the presence and the impact of human occupation in such areas.

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Scientists hope to use the 3D images they’ve taken so far to also help identify which historic sites are most vulnerable to hurricanes, erosion and other dangers before it’s too late to save the island’s patrimony. The first site scientists targeted was a large swath along the U. Scientists discovered what appears to be a large settlement just east of the ceremonial site thanks to drones and technology including 3D images, she said.

They were also able to determine the shape of the ceremonial site, she added. Armed with that information, scientists used excavations to determine that one of six plazas previously discovered appears to have been used for ceremonial dances and the veneration of ancestors. The Tainos populated various Caribbean islands but were eventually wiped out after the arrival of Christopher Columbus and European settlers.

Puerto Rico’s Department of Natural Resources has said the sea level around the island is rising by more than 3 millimeters – a little over a tenth of an inch – per year. But climate change has more immediately dramatic effects as well, destroying habitats, eroding coastlines and causing more powerful storm surges when hurricanes hit.

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The findings, reported in the Bulletin of the Seismological Society of America , could shape new evaluations of seismic hazard in New Zealand. They suggest that earthquakes rupturing multiple faults may contribute more than subduction earthquakes to damaging uplift in the area. Using radiocarbon and other methods to date the marine terraces at two North Island sites, Puatai Beach and Pakarae River mouth, Nicola Litchfield of GNS Science and her colleagues conclude that the uplift events that created the terraces occurred at different times between the two sites.

This suggests that the uplift was not the result of subduction earthquakes or single-fault upper plate earthquakes. The pattern of uplift seen in the marine terraces led the researchers to map new offshore faults in the region, which they think may be one source of these upper-plate earthquakes, said Litchfield. The Hikurangi Subduction Margin lies along the eastern edge of North Island, where the Pacific and Australian tectonic plates collide and the Pacific plate slips under the island.

Recent New Zealand earthquakes involving multiple fault ruptures and coastal deformation, such as the magnitude 7. Marine terraces are created when shorelines are raised above sea level by uplift at the coast, and they record the time and amount of uplift. Previous radiocarbon dating studies suggested that the youngest marine terraces at Puatai Beach and Pakarae River mouth were created at the same times.

But Litchfield and colleagues decided to revisit these dates with a more comprehensive examination of the terraces. The researchers were able to use a layer of volcanic ash, along with radiocarbon dating of beach shells, to determine ages for each terrace at each site. At Puatai Beach, the terraces correspond to three earthquakes that occurred between and years ago, and years ago, and and years ago. At Pakarae River mouth, the terraces correspond to earthquakes that took place between and years ago and between and years ago.

The different terrace ages at each site combined with modeling of uplift from earthquakes on newly mapped offshore faults allowed the researchers to rule out a subduction earthquake or single-fault upper-plate earthquake as the cause of uplift.

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We report the results of underwater archaeological investigations at the submerged Neolithic settlement of Tel Hreiz — BP , off the Carmel coast of Israel. The underwater archaeological site has yielded well-preserved architectural, artefactual, faunal and human remains. Based on archaeological context, mode of construction and radiometric dating, we demonstrate the feature was contemporary with the inundated Neolithic settlement and conclude that it served as a seawall, built to protect the village against Mediterranean Sea-level rise.

The seawall is unique for the period and is the oldest known coastal defence worldwide. Its length, use of large non-local boulders and specific arrangement in the landscape reflect the extensive effort invested by the Neolithic villagers in its conception, organisation and construction. However, this distinct social action and display of resilience proved a temporary solution and ultimately the village was inundated and abandoned.

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Coastal data are important for land use managers, planners, emergency management personnel, municipal officials and property owners alike. A number of agencies actively collect and maintain coastal data, and produce maps that can be very informative and useful to many people. The New Jersey Coastal Management Program seeks to increase awareness of, and facilitate access to these data. This page is provided as a descriptive reference of access links for a variety of New Jersey coastal maps and data.

For a more extensive listing of Internet sites that provide coastal information, please click ” Coastal Links ” on the toolbar above. This information includes land use and land cover, soils, slopes, wetlands, lakes, streams, tidelands, geology, watershed locations and boundaries, color infrared digital imagery and much more. Hard copies of various maps and environmental reports can also be obtained from the Department’s Maps and Publications Office: www.

Historical shoreline maps can be used to evaluate changes over time and predict areas of future shoreline change.

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