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This study commenced in July of 2005 to help address the many shoreline and <br />hazard issues associated with the Kapoho area. This report helps to determine the <br />extent of inundation and provide suggested solutions, alternatives and options. This <br />is not an easy task, since the area is at high risk from natural hazards, which is <br />compounded by the issue of subsidence. In addition, many homeowners and <br />landowners have invested much time and money into their property. Many are <br />attached to the property, both financially and emotionally. <br /> A major task of this study was to determine the magnitude of the subsidence <br />problem so that options and alternatives could be created that are related to the <br />dynamics of the area. Thus it was very important to determine if he subsidence at <br />Kapoho was simply episodic such as occurred during the 1975 Kalapana event, or if <br />there is a possibility that the subsidence is continuous and episodic. The later would <br />be significantly more difficult to plan for. Prior to this study, there was some <br />2 <br />evidence of on going subsidence in a letter from the Hawaii Volcano Observatory <br />and in documents from the Hawaii County Planning Department. However, the <br />information was not sufficiently specific in terms of the methodology and location to <br />determine if on going subsidence was applicable to the study area. Thus planning <br />decisions based on this evidence for the Kapoho Beach Lots and Vacationland area <br />could not be made. <br /> During the spring of 2006, a six month extension to the study contract was <br />granted so that the data collection from satellite measurements to determine the <br />extent, level, or magnitude of subsidence could be further evaluated. This would <br />allow the period of study to be extended from 26 months to 37 months (satellite <br />measurements from February 2003 to March 2006). With the extended period of <br />study, a greater level of confidence in the measurements was allowed, as well as <br />providing insight into any subsidence trends, or temporal variability. <br /> This report is divided into three parts to meet the three main objectives of the <br />study. Each of these objectives are covered in a specific chapter of this report. In <br />Chapter 2 and Appendix A, the subsidence was measured by satellite and analyzed to <br />determine if the problem is episodic only, or episodic and continuous. Specifically, <br />2 <br />September 17, 2001 Letter from Don Swanson of the United States Geological Observatory to Don <br />Swanson of the Hawaii County Planning Department. Based on leveling surveys along Highway 137 in <br />1976, 1986, 1987, 1989, and 1995, the Highway dropped about 0.4-0.5 inches each year relative to Hilo, <br />totaling 8.25 inches between 1976 and 1995. When combined with relative sea-level rise at Hilo of .16 <br />inches per year, the relative sea-level rise for the area near the highway should be .56-.66 inches per year. <br />Thus total subsidence along the highway was about 13-16 inches in the 24 year period after 1976. In the <br />letter, there is a question if the measurements along the highway are representative of the coastline. <br />Although no firm answer is provided, it is stated that the measurements are probably reasonable estimates <br />of the shoreline as well. Since a definite answer is not provided for the shoreline area, it was a major point <br />of this study to determine if the coastal area is also subsiding on an ongoing basis. This was confirmed in <br />this report (See report and Appendix A). <br />6 <br /> <br />