edgecumbe earthquake facts

Before The Earthquake Event Natural Processes Beneath The Surface Of The Earth Convection currents within the mantle of the earth cause tectonic plates to move. Shops were destroyed or lost stock from their shelves. / 0 1 2 3 4 5 6 8 9 : ; = > ? � � � � � � � � � � � � � � � � � � � � � � � � � � � � � $a$gdt� $a$gd�2i � � � � � � � � � � � � � � P Q � � � � $ % � � S T � � � � � � � � � � � � � � � � � � � � � � � � � � � $a$gd�w� $a$gdt� � � � � � � � � � � � � � 5 ; � � � � � " � � � � + 0 = Q R S ��ଛ��wfwfwfwfwfwfwfwfwfwS $ht� ht� CJ OJ QJ aJ mH sH !ht� 5�CJ OJ QJ aJ mH sH ht� CJ OJ QJ aJ mH sH 'h�w� h�w� >*CJ OJ QJ aJ mH sH !h�w� >*CJ OJ QJ aJ mH sH h�w� CJ OJ QJ aJ mH sH hf CJ OJ QJ aJ mH sH 'h�v� h�v� CJ H*OJ QJ aJ mH sH h�v� CJ OJ QJ aJ mH sH h�2i CJ OJ QJ aJ mH sH S � � � � � � � � � � � � � � � � � � � � � � S . Poor ability to predict earthquakes. You may use both diagrams and paragraphs. Civil Defence procedures are published. The earthquake caused a lot of damage to the land. The land to the east moved 0.5m away from the fault, while to the north, land dropped by 7m in places. Also everybody would trip and fall into the earthquake edgecumbe.There was a depth of 8 km and it was the most damaging earthquake New Zealand has experienced in a long time. The 1987 Edgecumbe earthquake measured 6.5 on the moment magnitude scale and struck the Bay of Plenty region of New Zealand at 1:42 pm on 2 March. People have poor emergency plans. Describe two economic effects of the extreme natural event. 1987 Edgecumbe earthquake 1987 Edgecumbe earthquake; Date: Monday 2 March 1987, 1:42 pm NZDT (): Magnitude: 6.5 M w: Depth A fissure (crack) up to 4 metres wide in places ran for 7km along the Edgecumbe fault. 4.) All information you need to know about Edgecumbe. The Damage Done The most shaken area was the town of Edgecumbe. There may be a number of aftershocks. You must refer to the Edgecumbe case study. Minutes later a much stronger quake rocked the region. Liquefaction occurred in coastal areas (when loose soils behave like liquids). The 1987 Edgecumbe earthquake measured 6.5 on the moment magnitude scale and struck the Bay of Plenty region of New Zealand at 1:42 pm on 2 March. ! " 3), was associated with renewed tectonic rupture on the Edgecumbe Fault, renewed movement on the Onepu and Rotoitipakau Faults, and several new surface breaks—the Awaiti, Otakiri, Te Teko, and Omeheu Faults.These northeast trending tectonic ruptures are widely distributed across the Rangitaiki Plains, range in length from 0. 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The hypocentre was at a shallow depth of 8 km. q � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � � $a$gdt� $a$gdt� � � R �� $a$gd�2i $a$gdt� � � � � � � � ! %&'()*456789:CDEFGHIJSTUVWXYZcdefghijstuvwxyz�� w !1AQaq"2�B�� #3R�br� This is a place where I will be able to share my learning with you. A massive 8.8 earthquake in Chile moved the city of Concepción 10 feet to the west on February 27, 2010. In the Napier earthquake. C �* A � � s c a n 0 0 0 9 � �R �T� Ѥ�u�zLU�`�]d�� 0� D �F�(� Ѥ�u�zLU�`�]d��~Exif II* HP z � � ( � i� � HP Scanjet djf300 � � � � � � � GeoNet. The 1987 Edgecumbe earthquake measured 6.5 on the moment magnitude scale and struck the Bay of Plenty region of New Zealand on 2 March. 5.) Financial Information; Warranty Policy; F.A.Q. These were reopened by night as emergency repairs were made. 8.) Recovery Oeriod (Shortly After) A State of Emergency is declared. - A shallow crustal earthquake of magnitude ML 6.3 occurred on March 2, 1987, at 01:42:34 UT, close to the town of Edgecumbe, North Island, New Zealand. Although not of an exceptional magnitude, it was damaging because it was very shallow. Subsequent simplified CPT-based liquefaction assessments undertaken using modelled Peak Ground Accelerations (PGA) and depth to ground-water for the Edgecumbe earthquake predicts moderate-to-severe … The 1968 Īnangahua earthquake. . Poor, under advertised Civil Defence procedures. Earth’s 80% of earthquakes occur near Pacific Ring of Fire. The Edgecumbe earthquake, 1987 March 2 (M L 6. Emergency Response Immediately after the event, emergency response can minimise loss of life, injury and damage to property. Rail Trails was breaking down, everything was breaking down and lots of people’s houses breaking down. On the afternoon of 2 March 1987, at 1:42pm, the Bay of Plenty region was rocked by a magnitude 6.3 earthquake. New Zealand. Edgecumbe earthquake. It is a region in Pacific Ocean which resembles the shape of a horse-shoe. 5 … Approximately 50% of all the houses in Edgecumbe had been damaged by the quake. The probable cause of the Edgecumbe earthquake was a sudden release of energy from an overstretched part of the underlying Pacific Plate. Rebuilding Napier. EDGECUMBE CASE STUDY PROJECT 1.) You may use both diagrams and paragraphs. Edgecumbe. Land use zoning to prevent people living on or near active fault lines. Draw a map of New Zealand and label on it the location of the Edgecumbe earthquake. The magnitude 6 earthquake which struck the Bay of Plenty area on the 2nd of March 1987 is remembered as the â€œEdgecumbe Earthquakeâ€ even though it was centred close to the coastal town of Matata. Strict building design codes. One of the local milk factories had some of their storage tanks topple over. Give me some ideas for next time or ask me a question. You must refer to the Edgecumbe case study. This stage can take a long time and can be very expensive. Describe two social effects of the extreme natural event. To support my learning I ask you to comment as follows:1. Mount Edgecumbe, a 970-m-high stratovolcano with a well-defined crater, is the largest volcano of the Edgecumbe field. You may use both diagrams and paragraphs. Describe the natural processes that occurred before the extreme natural event. Two milk tankers were thrown over onto one side by the force of the quake.Â An 80 tonne train toppled sideways in the Edgecumbe railway yards, and several kilometres of railway line in the area buckled in the earthquake. These and other vents of the volcanic field are oriented along a SW-NE line. Abstract. A shallow crustal earthquake of magnitude ML 6.3 occurred on March 2, 1987, at 01:42:34 UT, close to the town of Edgecumbe, North Island, New Zealand. Telephones, water and sewerage were also cut in many surrounding areas. Volcanic activity originated about 600,000 years ago along fissures cutting Kruzof Island. Facts about the 1987 Edgecumbe Earthquake: There was an earthquake at 1987 Edgecumbe It was measured 6.5 everybody was afraid and they would take photos of the big earthquake. The Edgecumbe earthquake has given rise to many informative studies. People seeking structural shelter in the event. Edgecumbe vulkaan Stratovolcanoes 970 m / 3,182 ft, United States, Eastern Alaska, 57.05°N / -135.75°W In de buurt van recente aardbevingen (binnen een straal van 30km): r t � ~ � � � ��ʴ��ڞʞ�ڎ�z�jZjD *j h�2i CJ OJ QJ UaJ mH nH u h�v� CJ OJ QJ aJ mH sH ht� CJ OJ QJ aJ mH sH 'ht� h�2i CJ H*OJ QJ aJ mH sH h,7 CJ OJ QJ aJ mH sH *j h,7 CJ OJ QJ UaJ mH nH u *j h|� CJ OJ QJ UaJ mH nH u h�UK CJ OJ QJ aJ mH sH h�2i CJ OJ QJ aJ mH sH *j h�UK CJ OJ QJ UaJ mH nH u The eruption of Mount Tarawera in 1886 and the 1987 Edgecumbe earthquake were two disasters related to geological activity in the volcanic plateau. � First we ... Ki Ora Today in Hurumanu1 we have been doing some research about the Christchurch Earthquake and we have to make a blog about the Christchur... 24th June: Aotearoa History Show/New Zealand War. The 1987 M L 6.3 Edgecumbe earthquake triggered localized liquefaction and associated lateral spreading in the township of Whakatane in the North Island of New Zealand. A fissure (crack) up to 4 metres wide in places ran for 7km along the Edgecumbe fault. Shaking can cause earth deformation. Tsunami may occur � shortly after main shocks. By Karin Lehnardt, Senior Writer. I would love your feedback, comments, thoughts and ideas. good soil and natural beauty. Edgecumbe earthquake latest breaking news and updates, information, look at maps, watch videos and view photos and more. Edgecumbe was linked with Tauranga and Auckland by rail, with the opening of the East Coast Main Trunk Railway and Taneatua Express in 1928. Crater Ridge is truncated by a 1.6-km-wide, 240-m-deep caldera. Registering magnitude 6.25 on the Richter Scale, this earthquake and its aftershocks caused damage of over NZ$400 million. The 1929 Arthur’s Pass and Murchison earthquakes. Earthquake Facts; 61 Fascinating Facts about Earthquakes. An earthquake 30 years ago could be the reason why the Bay of Plenty town of Edgecumbe was so badly affected by flooding this week. Pressure is released by failure along a fault line. Please note....some work won't be edited - just my first drafts, so there may be some surface errors. I am a student at in Uru Mānuka. Explain three things people could do which would increase the effects of the earthquake. ��( ��( ��( ��( ��( ��( ��( ��( ��( ��( ��( ��( ��( ��( ��( ��( ��( ��( ��( ��( ��|q� �7��(��Aua��G=��^C�i:F��-֫��_�Ammei��,��G�%�u��ݵ��7~��)��Sg�=��%{�m��F��:�(`֬�ɲ�|�V?�{[�$��\��m"�};��Ն��m��֭�9*�y�Z��u8��'�VQ^�?�OῊ. The 1987 Edgecumbe earthquake. During The Earthquake Event Natural Processes On The Surface Of The Earth The earth moves and shakes as earthquake waves radiate from the focus (origin). Also everybody would trip and fall into the earthquake edgecumbe.There was a depth of 8 km and it was the most damaging earthquake New Zealand has experienced in a long time. # + , - / 0 1 2 4 6 7 = ? The focus of the earthquake was 8kn below the surface. Cultural Processes People live in seismic areas due to e.g. ��A!�"�#��$��%� �� D d ��:9 �N � It was, with the exception of the Inangahua earthquake in 1968 , the most severe and damaging earthquake to hit New Zealand in 45 years. at a shallow depth of approximately 8 km. 0 that occurred in an area of about 70 × 50 km in the Bay of Plenty, New Zealand, between 1987 February 21 and March 18. New Zealand�s most damaging earthquake in recent years took place at 1.42pm on 2nd March 1987 at Edgecumbe in the Bay of Plenty. People re-entering earthquake areas which may be affected by after shocks. Bridges were damaged and roads into the region were forced to close. Historically, Edgecumbe is prone to floods, earthquakes, and debris flows. Today we watched the Aotearoa History Show about the New Zealand Wars. The shock was centred on the town of Edgecumbe and occurred just after 1:42 pm. Lack of insurance. Over 500 people were evacuated in case the Matahina dam burst. � 0220� J � � 0100� � � � � � In 1987, a large earthquake centered on Edgecumbe shook the Bay of Plenty, causing widespread damage and causing much of the population to leave Edgecumbe. Liquefaction primarily manifested proximal to the Whakatane River in areas underlain by recent fluvial and marine sediments. } !1AQa"q2��#B��R��$3br� The hypocentre was at a shallow depth of 8 km. Max 125. The Edgecumbe Earthquake of 1987. Services fully re-established. At 1.35 p.m. on 2 March 1987, a magnitude 5.2 earthquake struck the Bay of Plenty region, cutting power and sending many people outdoors. You may use both diagrams and paragraphs. Facts about the 1987 Edgecumbe Earthquake: There was an earthquake at 1987 Edgecumbe It was measured 6.5 everybody was afraid and they would take photos of the big earthquake. The M6.5 event was soon named after the town. Fun Facts for Kids on Earthquakes – Image of a Road Damaged by Earthquake. Business activity normalised. The centre of greatest destruction was in the Edgecumbe area where houses either collapsed or lost roves, chimneys fell and bridges were damaged. Another 500 slept in shelters the first night. It took up to three days for basic services (water, power, sewerage) to be re-established in all local areas. This main shock, at 1.42 p.m., had a magnitude of 6.3 and was centred north of Edgecumbe. There was another earthquake and it made it bigger so the grass was destroyed and everybody was talking about it in the (News.) Edgecumbe earthquake. The 1987 Edgecumbe earthquake. [1] �( �( �( 8 ) 4 R) D �7 � �) �) �) �) �) �/ �/ �/ !7 #7 #7 #7 #7 #7 #7 $ �8 h ; � G7 4 c. � �/ 4 4 G7 �) �) � \7 �6 �6 �6 4 � p �) �) !7 �6 4 !7 �6 �6 � � �6 �) �) @��=�� ( �4 �6 !7 r7 0 �7 �6 �; 6 � �; �6 �; �6 \ �/ � �0 � �6 �1 � 2 � �/ �/ �/ G7 G7 �6 " �/ �/ �/ �7 4 4 4 4 � �( �( $ 4 X " z �� The Edgecumbe Earthquake CASE STUDY PROJECT The Australian Plate lies to the west of New Zealand and the Pacific Plate lies to the east of New Zealand. A State of Emergency was declared at 2.50pm on 2nd March, lasting until 13th March. People are avacuated, emergency medical facilities are set up, fires put out, basic infrastructure is repaired.
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