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All Journal Bulletin of Scientific Contribution : Geology Jurnal Ilmiah Pariwisata
Sapari Dwi Hadian
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Civil Engineering, Building, Construction & Architecture Earth & Planetary Sciences Education Energy Environmental Science Social Sciences Transportation Other

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Mengenal Media Promosi Konvensional Sebagai Sarana Penyebaran Informasi Mengenai Destinasi Wisata Kedunglumpang Pangandaran Ute Lies Siti Khadijah; Edwin Rizal; Sapari Dwi Hadian; Lutfi Khoerunnisa
Jurnal Ilmiah Pariwisata Vol 26 No 3 (2021): Jurnal Ilmiah Pariwisata
Publisher : Pusat Penelitian dan Pengabdian Kepada Masyarakat, Sekolah Tinggi Pariwisata Trisakti

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.30647/jip.v26i3.1423

Abstract

In the midst of the current modern globalization, the use of social media has almost been enjoyed by most people. However, it turns out that not all elements of society have the ability to use social media. The existence of this conventional media is still sustainable and is used today, in fact it is still a favorite media for villagers in Kedungwuluh, Pangandaran. The method used in this research is a qualitative descriptive method, in which the writer tries to describe in detail and detail a certain phenomenon. This study emphasizes the development of concepts and collects facts found in the field and does not carry out hypotheses. The purpose of this study was to determine the reasons for tourism managers and local village officials to maintain this conventional promotional media as one of the important media in promoting Kedung Lumpang tourism. The next goal is to find out what conventional media are used in the promotion. The result of this research is that there are several conventional media which are considered effective in the current promotion process. First, through word of mouth. The second is through parades or mobile announcements, and the last is through a carnival. Keywords: Conventional promotion media, Kedung Lumpang tourism, Public information, Rural communities
MANAJEMEN AIRTANAH PADA ENDAPAN ALUVIUM RAWA LAKBOK, JAWA BARAT Sapari Dwi Hadian; Bombom Rahmat
Bulletin of Scientific Contribution: GEOLOGY Vol 13, No 3 (2015): Bulletin of Scientific Contribution
Publisher : Fakultas Teknik Geologi Universitas Padjadjaran

Show Abstract | Download Original | Original Source | Check in Google Scholar | Full PDF (347.003 KB) | DOI: 10.24198/bsc geology.v13i3.8406

Abstract

Rawa Lakbok revealed as depression of Citanduy River, developed as peat swamp with type B overflow. Geographically, area of study located on 108° 35’ 29,3” – 108° 36’ 34,6” east longitude and 7° 23’ 33” – 7° 24’ 37, 7”south latitude. Area of study located on Puloerang Village, Sub-district of Lakbok, District of Ciamis, West Java. Geology success-ion of study area will be described in several aspect; Geomorphology, Stratigraphy, and Geological history. Geomorphologically, area of study consist of alluvium plain unit, and moderately steep volcanic unit From stratigraphy aspect, area of study consist of sandstone unit (Tpbp), Andesite unit (Tpa), and Alluvium unit (Qa). With Structural Geology heading South East – North West. Geological history of study area began in Early Pliocene with deposition of sand material. Afterwards, volcanic activity occurred and erupted andesite lava. At the end, alluvium was deposited as response of depression which formed in area of study.From the water balance calculation at Cibeber rivers area with width ± 10.12 kM2, known that : precipitation value 2,805.82 mM/Annual, 58.48% of pouring rain will evaporate, 21.11% will be run off, and 6.25% will infiltrate into the soil. Study area have 17.92% (5,088,437.2 M3/Annual) of axcess water of depression storage, means amount of water that accumulate in the surface of depression bowl from the study area surface run off. Hidrogeology of study area consist of hydraulic gradient values ranging from 0.0008 – 0.004. Hydraulic T Parameter ranging from 5 – 10 M2/day, K values ranging from 1 – 5 M/day, S value ranging from 1 – 5, and Sc value ranging from 17 – 37 M3/day/Mdd. Influence radius of Cone of depression rangingfrom 1.2–2 M. Keywords: depresion zone, groundwater manajemen
Co-Authors Bombom Rahmat Edwin Rizal Lutfi Khoerunnisa Ute Lies Khadijah