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"This paper discusses the extent of eruption of Merapi volcano in 1994. It looks at the effects associated with the volcano as it erupted. The damages were inflicted on both the abiotic and biotic environments. The eruption occurred in the southern parts of the volcano. Because of the potential problems the volcano has, this has called for government involvement as an attempt to minimise the casualties. This has been done by intergovernmental cooperation for instance through the establishment of disaster prevention projects like Sobo Technical Centre, Merapi Volcano Project and the office purposely concerned with the investigation on the activities of Merapi. These projects cooperate to establish the hazard maps."

"This article is aimed to find out the behavioural characteristics of people residing in the dangerous zone of Merapi relating to their aspiration and perception on their settlement environment. Three sample areas are located in the volcanic slopes of Merapi being classified as the most dangerous zone whereas the other three are located along the river banks of river flowing down the mount. The result of this research shows that most of the people (65%) do not afraid of the danger, 18% feel afraid of it while the rest 17% are tremendously afraid of the danger. But 94% of the people interview said they are keen to remain living in the village and ony 6% of them are likely to move."

"Daerah penelitian berada di perbatasan antara Dataran Yogyakarta dengan Pegunungan Selatan Yogyakarta bagian barat. Secara morfologi dan litologi yang tersingkap, indikasi gunung api purbayang dibuktikan dengan keterdapatan batuan gunung api seperti lava, breksi, dan tuf. Tujuan daripenelitian ini adalah identifikasi adanya batuan gunung api purba di bawah permuaan sepanjang Berbah-Imogiri berdasarkan data geolistrik. Metode yang digunakan adalah melakukan pengukuran geolistrik di empat lokasi secara mapping dengan konfigurasi dipole-dipole. Panjang bentangan untuksetiap lintasan 500 meter. Hasil pengukuran geolistrik menunjukkan pada lintasan 1 di Sumber KulonKalitirto,Kecamatan Berbah,diinterpretasi adanya batuan gunung api berupa lava basal dan tuf. Lintasan 2 di Pilang-Srimulyo, Kecamatan Piyungan, diinterpretasi berupa breksi skoria. Lintasan 3 di Ngeblak-Bawuran, Kecamatan Pleret, diinterpretasi adanya tuf dan lava. Lintasan4 di Guyangan-Wonolelo, Kecamatan Pleret diinterpretasi berupa tuf dan lava. Batuan gunung api secara umum terbaca mempunyai nilai tahanan jenis yang tinggi, yaitu >300 Ωm. Adanya kandungan air atau mineralisasi cenderung menurunkan nilai tahan jenis batuan gunung api tersebut."

"ABSTRAKHarapan merupakan salah satu faktor yang potensial dalam memprediksi resiliensi. Namun, hasil penelitian-penelitian sebelumnya masih kontradiktif dan terbatas dalam konteks tertentu sehingga hasilnya tidak bisa langsung digeneralisasi. Penelitian ini dilakukan untuk mengetahui pengaruh harapan terhadap resiliensi pada penyintas erupsi Gunung Kelud. Pengukuran harapan menggunakan alat ukur Adult Hope Scale AHS yang disusun oleh Snyder 1991 , sementara pengukuran resiliensi menggunakan alat ukur Connor-Davidson Resilience Scale CD-RISC yang disusun oleh Campbell-Sills dan Stein 2007 . Partisipan penelitian ini berjumlah 115 orang yang menjadi penyintas erupsi Gunung Kelud pada tahun 2014 dengan rentang usia 20-40 tahun. Hasil penelitian menunjukkan adanya pengaruh harapan yang positif dan signifikan terhadap resiliensi pada penyintas erupsi Gunung Kelud F = 51,044, p < 0,01 . Hal ini menunjukkan bahwa semakin tinggi harapan yang dimiliki penyintas, maka semakin tinggi resiliensi penyintas tersebut. Saran untuk menindaklanjuti hasil penelitian ini disertakan.

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ABSTRACTHope is one of potential factors for predicting resilience. However, prior studies show that the relationship between hope and resilience remain inconclusive and limited to certain context, so it can not be generalized to the other context directly. This study was conducted to examine hope as predictor of resilience among Kelud Eruption survivors. Hope was measured using Adult Hope Scale AHS which constructed by Snyder 1991 , while resilience was measured using Connor Davidson Resilience Scale CD RISC by Campbell Sills and Stein 2007 . Participants of this research are 115 survivors mean age 32, range 20 40 of Kelud Eruption on 2014. Result of this research shows that hope positive significantly predicts resilience F 51,044, p 0,01 . That is, the higher hope, the higher resilience among survivors. Recommendations for further research are included."