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The Alpine fault is defined as the 650 km long feature that extends the length of the South Island. Alpine Fault Tours: The earth moves - See 26 traveler reviews, 47 candid photos, and great deals for Whataroa, New Zealand, at Tripadvisor. Figure 1 Active fault map (black & grey lines) of South Island highlighting the Alpine Fault (bold within West Coast region). The Alpine Fault • Running about 600km up the spine of the South Island, the Alpine Fault is the on-land boundary of the Pacific and Australian tectonic plates. Because many faults show a combination of dip-slip and strike-slip motion, geologists use more sophisticated measurements to analyze their specifics. Geologists working on Project AF8 believe that the next severe earthquake on the Alpine Fault is most likely to be a rupture that begins in South Westland and “unzips” northwards and will … Piqiang Fault O Reverse Left lateral O Normal O Right lateral Their fault, not mine An anticline is best described as: An arching fold of rock caused by tension (pulling) O A U-shaped fold of rock caused by tension (pulling) An arching fold of rock caused by compression (pushing) O A U-shaped fold of rock caused by compression (pushing) The sister of Patsy's mom. The type of plate boundary at the Alpine Fault is a transform boundary. Where will the next earthquake centred on the Alpine Fault begin? There is dextral strike-slip motion as well as convergence between the Australian and Pacific plates. The seismicity rate of the Alpine fault is low but comparable to locked sections of the San Andreas fault, with large earthquakes expected. Seismicity decreases north of Bruce Bay at the Alpine fault and within a triangular region along the Alpine fault located between the Hope and Porters Pass fault zones. Here he explains what they were up to and shares some photos of the damage. The Deep Fault Drilling Project (DFDP) is an international science project studying the Alpine Fault in western South Island. Describe how rock bodies are moving at the fault plane. One indication that things have not always been quite so calm on the Alpine fault is the presence of a rock type called psuedotachylite, which is thought to form either during an earthquake or with a meteor impact. Cochran said data from the two sites gave evidence for 26 Alpine Fault earthquakes in the past 8000 years. In New Zealand they are formed along the Alpine fault by earthquakes. The alpine fault runs along the west side of the South Island of New Zealand and is "one of the longest, straightest, and fastest-moving plate boundary transform faults on Earth."(eg. The Marlborough Fault System is a major sequence of faults in the upper South Island. Each type is the outcome of different forces pushing or pulling on the crust, causing rocks to slide up, down or past each other. It is the on-land boundary of the Pacific and Australian plates.But where exactly is it? == Philippine Mobile Belt == The Philippine Mobile Belt is composed of a large number of accretionary blocks and terranes. The uncertainty is an estimate of how well-mapped or located the fault is at any given point, based on the type of data that One indication that things have not always been quite so calm on the Alpine fault is the presence of a rock type called psuedotachylite, which is thought to form either during an earthquake or with a meteor impact. 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