Determination of Shoreline Changes from 2002 to 2014 in the Mangrove Conservation Areas of Pamurbaya Using GIS

Prasita, Viv Djanat

doi:10.1016/j.proeps.2015.07.081

Cited by 20 publications

(20 citation statements)

References 1 publication

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“…Beberapa kajian yang pernah menggunakan data Google Earth adalah Li (2016) dan Boardman 2016, Raihansyah et al (2016), Hidayat et al (2016), dan Prasita (2015). Namun belum ada penelitian serupa yang dilakukan di pesisir Pantai Kabupaten Tangerang Serang.…”

Section: Pendahuluanunclassified

Coastal Morphological Dynamics of Tangerang Regency Banten and Indah Kapuk Beach Jakarta through Google Earth Imagery Analysis

Suwandana¹

2019

JPK UNTIRTA

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Section: Pendahuluanunclassified

Coastal Morphological Dynamics of Tangerang Regency Banten and Indah Kapuk Beach Jakarta through Google Earth Imagery Analysis

Suwandana¹

2019

JPK UNTIRTA

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“…The sedimentation process taking place causes the shoreline to move seaward. On the contrary, the process of erosion causes the shoreline to move landwards [14].…”

Section: Shoreline Changementioning

confidence: 99%

Determination of shoreline change along the East-Java coast, using Digital Shoreline Analysis System

Boer¹,

Suntoyo²,

Oele³

2018

MATEC Web Conf.

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Abstract. This study focused on determining the shoreline change at the East-Java coast by comparing the shorelines between 2006 and 2015, using digital shoreline analysis system (DSAS) techniques to identify and measure erosion (shoreline retreat) and accretion (shoreline advance). Shoreline change rates are calculated according to Shoreline Change Envelope (SCE), Net Shoreline Movement (NSM), End Point Rate (EPR), and Linear Regression Rate (LRR). Results present local variations in shoreline change distance as well as in shoreline change rates. The statistical methods showed similarities with the highest accretion distance of 991.57 meters in the region of Mulyorejo and highest erosion distance of 928.75 meters in Sidoarjo. The EPR shows a rate with a maximum of 169.98 m/year and a minimum of 3.428 m/year. As for the LRR a maximum of 189.58 m/year and a minimum of 5.467 m/year were conducted from calculations.

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“…Shoreline changes occur because of erosion and accretion processes. The erosion is a condition of the coast on the skids because of the activities of seawater, whereas the accretion represents the material addition caused by the deposition of material from a river (Prasita, 2015). The shoreline represents the area where the ocean and continent interact and where geomorphological processes develop quite fast compared to other oceanic and continental areas.…”

Section: Coastal Deposition Landformsmentioning

confidence: 99%

Coastal landforms caused by deposition and erosion along the shoreline between Punta Brava and Punta Betín, Santa Marta, Colombian Caribbean

Vargas-T.

Uribe-P.

Castellanos-A.

et al. 2016

Rev. Acad. Colomb. Cienc. Ex. Fis. Nat.

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Coasts are natural dynamic systems that are constantly changing. Several factors, such as sea level change, sediment availability and coastal processes strongly influence the evolution of the coastal landscape. However, the tectonic setting of the coast and the rate of sea level rise can also be important factors to consider. Coastal landforms are a consequence of the simultaneous operation of erosion, transportation and deposition processes and have evolved over a geologically short time, with several of them being almost exclusively the result of the action of ocean waves. The world's most spectacular and dramatic erosional landforms are due to wave action, whereas the reduction of wave energy created deposition landforms. This paper presents an analysis of the coastal landforms caused by deposition and erosion along the shoreline in the sector between Punta Brava and Punta Betín, Santa Marta region, Colombian Caribbean. On the other hand, it is a contribution to the geological knowledge of the Geotectonic Province of Santa Marta and emerges as an alternative solution to various problems. It also promotes research on this region regarding other factors such as the increasing marine activity, population in coastal areas, development of tourism, as well as a series of geological evolutionary processes that reflect in coastal morphology. Coastal landforms are valuable environmental, aesthetic, and recreational resources that are subject to natural processes as well as to the effects of human activities. The results of this study can provide a sound basis for sustainable planning and management of the territory. © 2016. Acad. Colomb. Cienc. Ex. Fis. Nat. Key words: Coastal landforms; Santa Marta; Geotectonic province; Colombian Caribbean; Evolutionary processes.Geoformas costeras causadas por depositación y erosión a lo largo de la línea costera entre Punta Brava y Punta Betín, Santa Marta, Caribe Colombiano ResumenLas costas son sistemas naturales dinámicos que cambian constantemente. La evolución del paisaje costero está fuertemente influenciada por varios factores, tales como el cambio del nivel del mar, la disponibilidad de sedimento y los procesos costeros. Sin embargo, la configuración tectónica de la costa y la tasa de aumento del nivel del mar pueden ser también factores importantes a tener en cuenta. Las geoformas costeras son una consecuencia de la operación simultánea de procesos de erosión, transporte y deposición y han evolucionado durante un periodo de tiempo geológicamente corto; varios de dichos procesos han sido el resultado casi exclusivo de la acción de las olas del mar. Las geoformas costeras de erosión más espectaculares y dramáticas del mundo se deben a la acción del oleaje, mientras que las formas deposicionales se producen por la reducción de la energía de las olas. En este trabajo se presenta un análisis de las geoformas costeras entre Punta Brava y Punta Betín, en Santa Marta, Caribe colombiano. Por otra parte, es una contribución al conocimiento geológico de la Provincia Geotectó...

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Determination of Shoreline Changes from 2002 to 2014 in the Mangrove Conservation Areas of Pamurbaya Using GIS

Cited by 20 publications

References 1 publication

Coastal Morphological Dynamics of Tangerang Regency Banten and Indah Kapuk Beach Jakarta through Google Earth Imagery Analysis

Coastal Morphological Dynamics of Tangerang Regency Banten and Indah Kapuk Beach Jakarta through Google Earth Imagery Analysis

Determination of shoreline change along the East-Java coast, using Digital Shoreline Analysis System

Coastal landforms caused by deposition and erosion along the shoreline between Punta Brava and Punta Betín, Santa Marta, Colombian Caribbean

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