East Java

Rakyat Indonesia, sebagai sumber suara bagi kontestasi pemilihan elektoral, harus memiliki pengetahuan dan pemahaman yang lebih baik tentang para kandidat serta kepentingan-kepentingan para pendukung mereka, baik pada Pilkada Kabupaten dan Provinsi yang akan diselenggarakan serentak pada tahun 2018, serta pemilihan calon anggota legislatif dan DPD pada 2019. Seluruh momentum politik ini harusnya menjadi perhatian oleh khalayak umum, terutama terkait komitmen masing-masing calon terhadap keselamatan ekologis wilayah di Jawa Timur.

INTISARI Daerah Tambakrejo dianggap menarik untuk dilakukan penelitian, karena permasalahan geologi daerah tersebut cukup kompleks dan sebagai seorang mahasiswa jurusan Teknik Geologi dituntut dapat menyelesaikan permasalahan geologi daerah Tambakrejo tersebut. Daerah penelitian secara administratif terletak di daerah Tambakrejo dan sekitarnya, Kecamatan Tambakrejo, Kabupaten Bojonegoro Propinsi Jawa Timur. Secara astronomis terletak pada koordinat 07 o 07'15'' LS – 07 o 20'00'' LS dan 110 o 32'30 " BT – 110 o 37'30 " BT. Tujuan penulisan adalah untuk mengetahui keadaan geologi daerah penelitian, yang meliputi geomorfologi, stratigrafi, geologi struktur, sejarah geologi, dan geologi lingkungannya. Metode yang digunakan adalah pemetaan geologi permukaan meliputi beberapa tahapan, antara lain tahap pra-lapangan, tahap lapangan yaitu kolekting data, dan tahap pasca lapangan berup aanalisis laboratorium dan analisis di studio. Geomorfologi daerah penelitian dibagi menjadi 3 subsatuan yaitu: subsatuan geomorfik tubuh sungai (F2), subsatuan perbukitan lipatan kompleks berlereng miring-curam (S21), subsatuan geomorfik perbukitan berlereng landai terdenudasional (D1). Daerah penelitian mempunyai 2 pola aliran yaitu dendritik dan trelis dengan stadia daerah muda menuju dewasa. Stratigrafi daerah penelitian dibagi menjadi 4 satuan batuan. Urutan satuan batuan dari yang tertua sampai yang paling muda adalah satuan napal perselingan batupasir Kalibeng, napal Kalibeng, Napal Lidah serta endapan aluvial. Struktur geologi yang berkembang di daerah penelitian berupa sesar, kekar dan lipatan. Daerah penelitian terdapat 2 lipatan, 3 sesar naik dan 1 sesar mendatar yaitu, Antiklin Margomulyo, Sinklin Tambakrejo, Sesar Naik Jatimulyo, Sesar Naik Jumuk, Sesar Naik Ngraho, dan Sesar Mendatar Windu yang memiliki arah tegasan utama relatif dari utara-selatan dengan pola timur-barat sampai baratlaut-tenggara dan timurlaut-baratdaya. Sesumber yang terdapat pada daerah penelitian adalah air dan lahan.Bahaya geologi dalam bentuk gerakan tanah berupa longsoran (landslide). ABSTRACT Tambakrejo region is considered interesting to do a reasearch, because of the geological problem exist in that area is considered complex and as a geologist student of Geology engineering, we demanded to explain the geological information of Tambakrejo region. Administratively research area is located in approximately Tambakrejo region, Tambakrejo Subdistrict, Bojonegoro Regency of East Java. Astronomicaly located in 07 o 07'15 " – 07 o 20'00 " latitude and 110 o 32'30 " – 110 o 37'30 " longitude. The writing objective of this essay is to understand the geological condition of research area, including the geomorfology, stratigraphy, structural, historical and environmental geology. Methode used in this project is surface mapping including several stage, which is preliminary field study, field study or data collecting, and post field study in form of laboratory analysis and studio analysis. Research area geomorphofology is consist of 3 sub unit which is, river bed geomorphical subunit (F2), moderatly to steeply complex folding hilly subunit (S21), denudational slopes and hills subunit (D1). Research area is made of 2 stream pattern that is trellis and sub-trellis pattern with youth to mature regional stadia. Statigraphy of research area consist of 4 bedrock unit. Queu of the bedrock unit from the oldest to youngest is napal bedrock unit with sandstone (Kalibeng formation), napal kalibeng, napal lidah and alluvial sedimentation. Structural geology developed in research area consist of fault, joint and folds. Research area consist of 2 folds, 3 reverse fault, 1 slip fault which is, Margomulyo anticline, Tambakrejo Syncline, Jatimulyo reverse fault, Jumuk reverse Fault, Ngraho reverse fault, Windu slip fault, all of that have relatively north-south main force direction with east-west pattern to northwest-southeast and northeast-southwest. Natural reserve occured in research area is mainly water and fertile farm land. Geological hazzard in research area is mass movement spesifically landslide.

Berdasarkan Undang-Undang No. 26 Tahun 2007 tentang Penataan Ruang dalam pelaksanaan penataan ruang diwujudkan dalam bentuk perencanaan tata ruang. Perencanaan tata ruang secara hierarki dilakukan untuk menghasilkan rencana umum tata ruang dan rencana rinci tata ruang. Rencana umum tata ruang terdiri atas Rencana Tata Ruang Wilayah Nasional, Rencana Tata Ruang Wilayah Propinsi dan Rencana Tata Ruang Wilayah Kabupaten/Kota. Rencana rinci tata ruang terdiri atas rencana tata ruang pulau/kepulauan, rencana tata ruang kawasan strategis Nasional/Propinsi dan rencana detail tata ruang kabupaten/kota. Dalam tataran masing-masing produk perencanan tetap mengacu pada perencanaan di atasnya, selain itu produk rencana umum dan rencana rinci ini juga dapat ditetapkan sebagai peraturan daerah kabupaten/kota masing-masing.
Seperti halnya yang terjadi di Kota Surabaya, rencana umum tata ruang yang telah disusun berupa Rencana Tata Ruang Wilayah (RTRW) Kota Surabaya telah ditetapkan sebagai peraturan daerah Diman, Peraturan Daerah Nomor 3 Tahun 2007 tentang Rencana Tata Ruang Wilayah (RTRW) Kota Surabaya ini merupakan suatu pedoman dalam perencanaan dan pengendalian perkembangan Kota Surabaya.
Salah satu komponen perencanaan adalah Intensitas Pemanfaatan Ruang. Dalam Intensitas Pemanfaatan Ruang terdapat Koefisien Dasar Bangunan (KDB), Koefisien Lantai Bangunan (KLB), Koefisien Dasar Hijau (KDH), Garis Sempadan Bangunan (GSB), Garis Sempadan Sungai (GSS), serta Ketinggian Bangunan.

The research area is located in kendeng fold-thrust belt in the estimated form at Plio-Pleistocene deformation in Java. Wherein Kendeng Zone it self is the foreland basin which deposited of deepwater sediment. The provenance of Kendeng Zone came from Southern Mountain (Genevraye and Samuel, 1972). The purpose of the study thrust fault kinematic and implication for tectonic evolutionin Kendeng Zone is to determining factor of influence and cause how thrust fault can form from 2 kinematic factor that is translation and rotation on rigid deformation, so that can form the tectonic framework of Kendeng Zone in research area. The methods used in kinematic analysis in research area comprehend : compression analysis happens to each thrust fault, examaining each movement of fault from compression analysis or translation analysis and rotational of fault. Observed the thrust fault geometry and relation regionally through satellite imagery and morphology.From compression analysis in 3 faults with 4 stress data founded relative compression north-south to northeast-southwest trending. Movement vector from thrust fault be affected from change of compression that relative rotation to pattern of pacul strike slip fault and be affected from the pattern of sysnthetic fault from pacul pandan mountain strike slip fault. The distributing compression so have relative rotation clockwise trending and have 19,5 o movement of rotation axis. The Geometry from thrust fault in Kendeng Zone showed imbrication trailing type system. Moreover tectonic of kendeng zone the main in Central Kendengcan not be separated from the influence of pacul strike slip fault that similar formed to starts of Kendeng fold and thrust fault form, with the compression trend north-south that begin in Plio-Pleistocene.

East Java Province has high diversity of local banana cultivars with various local names and diverse morphological characteristics. The genome identification of those banana cultivars are needed to provide valid identity of the banana accessions to be used as basic data for in-situ and/or ex-situ banana conservation management and for further breeding banana material. Polymerase Chain Reaction – Restriction Fragment Length Polymorphism (PCR-RFLP) of the Internal Transcribed Spacer (ITS) region nuclear ribosomal Deoxyribo Nucleic Acid (nrDNA) using RsaI restriction endonuclease enzyme was conducted to 68 banana accessions collected from 17 Regencies in East Java Province. The RsaI digested fragments showed consistent polymorphic banding DNA patterns; in M. acuminata the wild species and cultivars produced two fragments of 530 bp and 120 bp whereas M. balbisiana species and its hybrid cultivars produced three fragments of 350 bp, 180 bp and 120 bp. From this study it was found that about 45 accessions were identified as M. acuminata species (AA/AAA genomes). It comprises of 3 wild species M. acuminata (AAw), 17 M. acuminata diploid cultivars (AA) and 25 M. acuminata triploid cultivars (AAA). Wild species M. balbisiana identified only one accession (BBw), and the hybrid cultivars comprises of 14 M acuminata × balbisiana (ABB) cultivars and 8 M. acuminata × balbisiana (AAB) cultivars. Clustering analysis result based on restriction fragment ITS region showed that BBw, ABB and AAB genome groups were close related and clustered as sister group whilst AA/AA genome group became the out-group with similarity coefficient between 0,635 to 1.00.

East Java (JATIM), the second largest province in Indonesia in terms of population and GDP contribution had experienced 50 percent of export growth from 2007 to 2013. The changes were not only in value but in composition and destination, meaning that a change in the pattern of exports of JATIM and export performance was observed in the seven years of analysis. This study looks at those changes from the point of view of comparative advantage and export specialization. JATIM kept 55 percent of their competitive industries since 2007 as the backbone of their exports, losing the other 45 percent, while allowing the creation of new industries. The gains in new industries are higher than the losses indicating that relocation of resources and the change of focus is bringing benefits to the province. Dynamic changes had occurred among commodities –gains and losses in comparative advantage and export specialization-, some presumed to be driven by commodity prices while others are more related to global integration.

Jawa Timur merupakan provinsi terluas di pulau jawa dengan luasan 4.796.300 hektar. Merujuk pada data BPS Provinsi Jawa Timur pada tahun 2017, luasan lahan yang dimanfaatkan sebagai area pertanian terutama untuk tegal/kebun sebesar 1.115.801,0 hektar, lalu untuk peruntukannya sebagai sawah sebesar 1.174.586,4 hektar. Komoditas utama yang dihasilkan berupa padi yang tingkat produktivitasnya dapat mencapai 12.432.703 ton untuk luasan lahan 2.136.412 hektar, sementara untuk jagung dapat mencapai 6.335.252 ton dalam satu tahun. Berbeda dengan data Kementerian Pertanian, luas  pada 2017 lahan panen padi mengalami peningkatan sebesar 4,17% menjadi 15,79 juta hektar.  Jawa Timur sendiri menurut Kementan merupakan provinsi dengan luasan lahan panen padi terbesar, dengan luas sekitar 2,29 juta hektar.

What personalities and processes need to be present for religious traditions to successfully establish new constituencies? In Aceh, for example, did recently arrived Arabs from Aden play key roles in the processes of "Islamisation?" While few claim rank outsiders to have been crucial in chapters of significant religious change, in this paper I argue that neither are individuals⎯albeit inadequately⎯described as insiders. Accounts provided by historians done with dissecting the dynamics of religious change note the presence of multi-lingual and mobile mediators, who have been described as "inbetweeners", who were adept at importing new ideas⎯including ways of dealing with the divine. Commerce across the Indian Ocean both before and after the rise in European presence centred on ports where being different was normal. Pre-colonial port-cities produced ethnolinguistical “creole” or “cosmopolitan” communities whose comfort with ethnoreligious diversity is lamentable scarce in present-day South and Southeast Asia. This paper considers the role of “mobile mediators” and “inbetweeners” in the importation of a range of Islamic movements in Thailand. I make suggestions about the personalities and processes through which ideas espoused by Imam Al-Ghazali (1058–1111), Sheikh Ahmad Ibn Idris (1760-1837), and Muhammad ‘Abduh (1849-1905) become known in Thai/Malay Peninsula. I describe the contributions and discuss the identity of local luminaries including Shaykh Ahmad al-Fatani, Ishmael Lutfi Japakiya, Direk Kulsriswasd, and Conrad Laurens Coolen to the spread of mystical, modernist, reformist, and revivalist Christian and Muslim movements.

The subsurface temperature has many impacts on geological phenomena such as hydrocarbon generation , geothermal energy, mineralization, and geological hazards. The Northeast Java Basin has various interesting phenomena, such as many oil fields, active faults, mud eruptions, and some active and dormant volcanoes. We measured temperature data from tens of wells along a 130 km survey line with an average spacing of 5 km. We also measured the thermal conductivity of rocks of various lithologies along the survey line to provide geother-mal heat flow data. We propose integrated modeling for profiling the subsurface temperature beneath the survey line from Mt. Lawu to Mt. Muriah in the Northeast Java Basin. The modeling of subsurface temperature integrates various input data such as a thermal conductivity model, surface temperature, gradient temperature, a geological model, and geothermal heat flow. The thermal conductivity model considers the subsurface geological model. The temperature modeling uses the finite difference of Fourier's law, with an input subsurface thermal conductivity model, geothermal heat flow, and surface temperature. The subsurface temperature profile along with survey line shows some interesting anomalies which correlate with either subsurface volcanic activity or the impact of fault activity .

Background: Indonesia is the third highest contributor to leprosy in the world. The prevalence of Pausi Basiler (PB) type leprosy in East Java has increased from 2015-2017, but the success rate of treatment is more common in PB leprosy compared to Multi Basiler leprosy (MB). Purpose: This study aimed to analyze the relationship between the numbers of PB type leprosy incidence with the success rate of leprosy treatment in East Java in 2015-2017. Methods: This study was an observational analytic study with cross-sectional design. The population used is leprosy patients who have successfully treated by leprosy therapy in East Java which was recorded from 2015 to 2017. The population sampling technique was performed in this study. Moreover, univariate and bivariate analysis were used. Specifically, Spearman correlation test was part of bivariate analysis. Results: This study showed the success presentation of leprosy treatment in male patients has increased for three consecutive years, namely 59.07% in 2015, 59.74% in 2016, and 63.96% in 2017. Oppositely, the success rate of leprosy in the female group decreased each year. There is a significant relationship between the number of PB type leprosy cases with the success rate of leprosy treatment in East Java from 2015 to 2017 (p= 0.00; p <0.05; Spearman correlation = 0.89). Conclusion: The highest success rate of leprosy treatment found in the male group. There is a relationship between the numbers of PB type leprosy cases with the success rate of leprosy treatment in East Java from 2015 to 2017.

The research area is located in kendeng fold-thrust beld in the estimated form at Plio-pleistocene deformation in java. Wherein kendeng zone it self is the foreland basin which deposite of deepwater sediment. The provenance of kendeng zone came from southern mountain (Genevraye and Samuel, 1972). The purpose of the study thrust fault kinematic and implication for tectonic evolutionin kendeng zone is to determining factor of influence and cause how thrust fault can form from 2 kinematic factor that is translation and rotation on rigid deformation, so that can form the tectonic framework of kendeng zone in research area. The method used in kinematik analysis in research area comprehend : compression analysis happens to each thrust fault, examaining each movement of fault from compression analysis or translation analysis and rotational of fault. Observe the thrust fault geometry and relation regionally through satellite citra and morphology observation. From compression analysis in 3 faults with 4 stress data founded relative compression north-south to northeast-southwest trending. Movement vector from thrust fault be affected from change of compression that relative rotation to pattern of pacul pandan mount strike slip fault and be affected from the pattern of sysnthetic fault from pacul pandan mount strike slip fault. The distributing compression so have relative rotation clockwise trending and have 19,5 o movement of rotation axis. The Geometry from thrust fault in kendeng zone showed imbrication trailing type system. Moreover tectonic of kendeng zone the main in central kendeng can not be separated from the influence of pacul strike slip fault that similar formed to starts of kendeng fold and thrust fault form, with the compression trend north-south that begin in Plio-Pleistocene.

We successfully revealed the refined seismicity near Mt. Pandan which occurred on February 2016 adopting waveform cross-correlation technique. Mt. Pandan seismic sequence is very interested since there were some earthquakes occurred in June 2015 and also seismic swarm in February 2016. Cross-correlation values are necessary to be used in double-difference relocation due to providing more reliable travel time differential data. About 65 events is relocated using 27 channels came from 9 seismic stations of BMKG. We provided more precisely hypocenters because the P and S phases are manually hand-picked. Seismicity pattern more precisely shows lineation which is elongated and deeper in west-east direction (10-20 km) and has no correlation with thrusting fault on the north side Mt.pandan otherwise strongly expected was related to strike-slip fault in the northeast Klangon, near Mt. Pandan.

Development Area Unit IV East Java Province is one of the provinces on the island of Java which consists of three regencies, namely Jember Regency, Bondowoso Regency and Situbondo Regency. The area has great potential for ecotourism such as marine tourism, nature tourism, cultural tourism and handicrafts spread across several sub-districts. which is visited every day. Therefore, in an effort to take advantage of the potential of the region and maintain the sustainability of the area, this research is needed. The purpose of this study was to identify and inventory the potential of ecotourism resources in the Regional Development Unit IV of East Java Province. The analytical method used in this study is an analysis of ecotourism potential, a qualitative descriptive analysis technique used as an analysis of ecotourism potential. The results of the study show that there is a lot of potential in the Regional Development Unit IV of East Java Province to be developed. Broadly speaking, the ecotourism potential can be directly accessed through: https://pariwisata.situbondokab.go.id and https://disparpora.bondowosokab.go.id and https://jembertourism.com.

This paper studied the influence of asset sustainable livelihood either direct or indirect due to development ofagriculture city. Location of study was at Batu city as one of central agriculture city, East Java Province of Indonesia. Batu was well known either as tourism city or center agriculture city. As center agriculture city was supported by the natural and environmental condition, and public social condition mainly by functioning agricultural area. The methodology consisted of interview, documentation, observation and field survey, collecting secondary data, and then analysis data. Results used as the consideration in the effort of developing center agriculture based on livelihood sustainable approach Otherwise, agricultural business men could develop their business wisely by using the facilities like: the input was agricultural structure; agricultural plantation was on farm, and producing agricultural results as agroindustry.&lt;br&gt;

Financial inclusion is an effort intended to eliminate price and non-price barriers toward public access to formal financial institutions. The aim of that is income equalization of the societies affecting increasing economic growth, poverty alleviation, and financial system stability. East Java is one of the provinces in Indonesia with the most number of Islamic Rural Banks (BPRS). This study wants to find out how the role of BPRS in realizing the acceleration of Islamic financial inclusion in East Java. Then, this research is conducted in the period January 2014 – May 2018 in which data sourced from the Islamic Banking Statistics (SPS), Financial Services Authority (FSA). An Autoregressive Integrated Moving Average (ARIMA) is applied as research method to predict the level of Islamic financial inclusion in East Java through BPRS by using three from four financial inclusion indicators released by Bank Indonesia in 2014 namely access with number of BPRS as its proxy, usage with amount of third party funds and amount of financing as its proxies, and quality with total assets and NonPerforming Financing (NPF) as its proxies. The results show that based on forecasting values until December 2020, the number of BPRS predicted will decrease with the last number as many as 27 banks, DPK will increase with the last number 1,680,558.79 million Rupiah, the amount of financing will increase with the last number as many as 1,822,810.80 million Rupiah, asset will increase with the last number 2,299,250.44 million Rupiah, and NPF will increase with the last number 12.48 percent.

We successfully revealed the refined seismicity near Mt. Pandan which occurred on February 2016 adopting waveform cross-correlation technique. Mt. Pandan seismic sequence is very interested since there were some earthquakes occurred in June 2015 and also seismic swarm in February 2016. Cross-correlation values are necessary to be used in double-difference relocation due to providing more reliable travel time differential data. About 65 events is relocated using 27 channels came from 9 seismic stations of BMKG. We provided more precisely hypocenters because the P and S phases are manually hand-picked. Seismicity pattern more precisely shows lineation which is elongated and deeper in west-east direction (10-20 km) and has no correlation with thrusting fault on the north side Mt.pandan otherwise strongly expected was related to strike-slip fault in the northeast Klangon, near Mt. Pandan.