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Dziak, R. West Mata is a m deep submarine volcano where explosive boninite eruptions were directly observed in May Here we present long-term acoustic and tephra records of West Mata explosion activity from three deployments of hydrophone and particle sensor moorings beginning on 8 January These records provide insights into the character of explosive magma degassing occurring at the volcano 's summit vent until the decline and eventual cessation of the eruption during late and early The detailed acoustic records show three types of volcanic signals, 1 discrete explosions, 2 diffuse explosions, and 3 volcanic tremor.

Discrete explosions are short duration, high amplitude broad-band signals caused by rapid gas bubble release. Diffuse signals are likely a result of 'trap-door' explosions where a quench cap of cooled lava forms over the magmatic vent but gas pressure builds underneath the cap. This pressure eventually causes the cap to breach and gas is explosively released until pressure reduces and the cap once again forms. Volcanic tremor is typified by narrow-band, long-duration signals with overtones, as well as narrow-band tones that vary frequency over time between Hz.

The harmonic tremor is thought to be caused by modulation of rapid, short duration gas explosion pulses and not a magma resonance phenomenon. The variable frequency tones may be caused by focused degassing or hydrothermal fluid flow from a narrow volcanic vent or conduit.

Acoustic data suggest that eruption velocities for a single explosion range from m s-1, although synchronous arrival of explosion signals has complicated our efforts to estimate long-term gas flux. Directory of Open Access Journals Sweden. Pemanfaatan mata air sangat beragam, antara lain penggunaan untuk keperluan air minum, irigasi, perikanan, untuk obyek wisata. Mata air mempunyai debit terbatas, namun kualitasnya baik, penggunaannya beragam, hal tersebut sering terjadi konflik pemanfaatan.

Di saat musim kemarau, beberapa mata air merupakan sumber air satu-satunya di suatu tempat, sehingga pengelolaannya harus dilakukan secara baik. Penelitian ini bertujuan untuk mempelajari pengelolaan mata air berbasis teknologi tepat guna dalam penyediaan air rumahtangga di lereng selatan Gunungapi Merapi.

Penelitian dilakukan dengan survei dan observasi di lapangan terhadap mata air yang digunakan untuk penyediaan air rumahtangga. Sejumlah responden pengguna mata air dan tokoh masyarakat setempat diwawancarai secara bebas dan terstruktur untuk memperoleh data pengelolaan mata air.

Hasil penelitian menunjukkan bahwa kondisi lingkungan dan karakteristik mata air, pengetahuan masyarakat dan budaya lokal yang beragam akan berpengaruh terhadap pengelolaanmata air. Perkembangan teknologi tidak dapat diabaikan dalam pengelolaan sumberdaya air.

Hal ini dapat dipadukan dengan budaya masyarakat setempat dalam pengelolaan mata air, sehingga dapat diperoleh manfaat yang optimal dan kesinambungan fungsi dan manfaat mata air tersebut. The use of water from springs is very diverse, varying from water for drinking, irrigation, fisheries, even for tourism.

The springs usually have a limited discharge but the water quality from springs is good, therefore they are often facing some conflicts in utilization. In the dry season, in fact the springs are the only source of water supply; therefore the management of the spring should be done properly. This research aims to study the spring management based on appropriate technology in relation to household water supply in the. This paper summarize the preliminary data about a geological mapping on the scale The recognized units comprise the Mata Surrao granite, which is within the typical Archean Granite-Greenstone Terrain of Rio Maria, and has mainly a monzogranitic composition.

Its foliation is restricted to the north and east borders. The mapped host rocks are represented by Tonalitic Ortho gneisses, Gneisses with Pegmatites, Migmatite Gneisses, both latter show different deformation rates. Such age can be interpreted either as the crystallization age of this granitic body, or a renewed one caused by the thermo tectonic event that affected the region at the end of Archean time.

It can be deduced from the initial ratio that an important crustal contribution controlled the Mata Surrao granite genesis. An eruption can also cause earthquakes, mudflows and flash floods, rock falls and landslides, acid rain, fires, and even tsunamis. Volcanic gas Baker, E. These boundaries create multiple zones of extension and thus provide abundant opportunities for magma to invade the crust. In we discovered hydrothermal venting on the largest and most southerly of these volcanoes , W and E Mata.

We also revisited W and E Mata. Over each volcano we conducted CTD tows to map plumes and collect water samples. Based on the CTD results, camera tows searched for seafloor sources on three volcanoes. The N Mata volcanoes , extending from Mata Taha 1 in the south to Mata Fitu 7 in the north, lie within a prominent gap in the shallow bathymetry along the southern border of the Tonga trench.

Northward from E Mata the Mata volcanoes degrade from large symmetrical cones to smaller and blocky volcanic edifices. Summit depths range from m W Mata to m Mata Nima 5. The most active volcano in the chain is the erupting W Mata , with an intense plume that extended m above the summit.

The surveys now show that 6 of the 7 N Mata volcanoes are also hydrothermally active. Sulfur dioxide emissions from la soufriere volcano , st. Vincent, west indies. This value is similar to the sulfur dioxide emissions of other Central American volcanoes but less than those measured at Mount Etna, an exceptionally strong volcanic source of sulfur dioxide.

Cristobalite in volcanic ash of the soufriere hills volcano , montserrat, british west indies. Crystalline silica mostly cristobalite was produced by vapor-phase crystallization and devitrification in the andesite lava dome of the Soufriere Hills volcano , Montserrat.

The submicrometer fraction of ash generated by pyroclastic flows formed by lava dome collapse contains 10 to 24 weight percent crystalline silica, an enrichment of 2 to 5 relative to the magma caused by selective crushing of the groundmass.

The submicrometer fraction of ash generated by explosive eruptions has much lower contents 3 to 6 percent of crystalline silica. High levels of cristobalite in respirable ash raise concerns about adverse health effects of long-term human exposure to ash from lava dome eruptions.

Magma flow instability and cyclic activity at soufriere hills volcano , montserrat, british west indies. Dome growth at the Soufriere Hills volcano to was frequently accompanied by repetitive cycles of earthquakes, ground deformation, degassing, and explosive eruptions. The cycles reflected unsteady conduit flow of volatile-charged magma resulting from gas exsolution, rheological stiffening, and pressurization. The cycles, over hours to days, initiated when degassed stiff magma retarded flow in the upper conduit.

Conduit pressure built with gas exsolution, causing shallow seismicity and edifice inflation. Magma and gas were then expelled and the edifice deflated. The repeat time-scale is controlled by magma ascent rates, degassing, and microlite crystallization kinetics. Cyclic behavior allows short-term forecasting of timing, and of eruption style related to explosivity potential. Gede Volcano West Java is part of an andesitic stratovolcano complex consisting of Pangrango in the north- west and Gede in the south-east.

The last recorded eruptive activity was a phreatic subvolcanian ash eruption in Hot springs occur in the saddle between the Gede and Pangrango edifice, as well as on the NE flank base. The most recent eruptive events produced pyroclastic material, their flow deposits concentrate toward the NE.

To support the monitoring instrumentation upgrades under way, surveys of soil CO2 degassing have been performed on the flanks of Gede, in circular and radial traverses. The goal was to establish a spatial distribution of flank CO2 fluxes, and to allow smart siting for continuous gas monitoring stations. Crater fluxes were not surveyed, as its low-temperature hydrothermal system is likely prone to large hydraulic changes in this tropical environment, resulting in variable permeability effects that might mask signals from deeper reservoir or conduit degassing.

The high precipitation intensity in the mountains of tropical Java pose challenges to this method, since soil gas permeability is largely controlled by soil moisture content. Simultaneous soil moisture measurements were undertaken. This instrument has a very precise and highly stable sensor and an atmospheric pressure equilibrator, making it highly sensitive to low fluxes. It is the far superior choice for higher precision low. Full Text Available Kasus kehilangan mata pada pasien dapat menimbulkan masalah fungsi dan estetik.

Salah satu cara yang dapat dilakukan untuk memperbaiki masalah estetik adalah dengan membuatkan protesa mata kepada pasien tersebut. Tujuan pembuatan obturator mata pada pasien yang kehilangan mata adalah untuk membantu pasien dalam memperbaiki estetik.

Pemeriksaan wajah menunjukkan muka asimetris. Pada mata kanan tampak adanya cheloid yang timbul setelah operasi pengangkatan bola mata. Perawatan dilakukan dengan pembuatan protesa mata non fabricated dengan tahap-tahap: pencetakan mata dengan sendok cetak mata perorangan dan pengisian hasil cetakan terdiri dari dua bagian, yang pertama diisi dengan gips keras sampai bagian terlebar dari cetakan dasar soket dan dibuat tiga retensi sebagai kunci, kedua sampai menutupi seluruh hasil cetakan.

Pembuatan model malam sklera, mencoba pola malam sklera dan packing model malam sklera. Kontrol setelah 2 minggu menunjukkan hasil yang baik, tidak ada keluhan rasa sakit, tidak ada peradangan, volume dan frekuensi air mata menjadi berkurang jumlah dan frekuensinya. This regional structure acts as conduits for the hydrothermal fluids to ascend from a deeper system toward the surface and, in the end, mix with groundwater. In this research, water geochemistry, gas chemistry and isotopes 2H, 18O and 13C were used to explore the subsurface fluid characteristics and mixing mechanisms of the hydrothermal fluids with groundwater.

In addition to those geochemical methods, soil-gas and dissolved Rn observations were performed to understand the geological control of fluid chemistry.

Based on the analytical results, the hydrothermal system of Tampomas is only developed at the northeastern flank of the volcano , which is mainly controlled by NE-SW structures as deep fluid conduits, while the Cimalaka Caldera Rim around Sekarwangi act as the boundary flow of the system. Soil-gas and dissolved Rn confirm that these permeable zones are effective conduits for the ascending thermal fluids. It is found that NE faults carry higher trace elements from the deeper system, while the circular feature of the Caldera Rim acts as the boundary of the hydrothermal system.

Hydrothermal system of the Papandayan Volcano , West Java, Indonesia and its geochemistry evolution of thermal water after the November eruption. After the last magmatic eruptionin , only few phreatic explosions have been occurring. At the present time, the activity is centeredin the northeast crater manifested by the presence of fumaroles and hot springs.

In November an explosive eruption occurred and ejected ash and altered rocks. Study of the altered rocks revealedthat an advanced argillic alteration took place in the hydrothermal system by an interaction betweenacid fl uids and rocks.

Four zones of alteration have been formed as a limited extension along faults oracross permeable structures at different levels beneath the active crater of the volcano. Two types of acid fl uids are distinguished in the crater of the Papandayan Volcano : 1 acidsulphate-chloride water with pH values between 1.

This evolution is likely explained by an increase in the neutralization of acidfl uids which tends to show that water-rock interactions were more signifi cant after the eruption.

Thechanges in chemistry observed in were the consequence of the opening of new fractures whereunaltered or less altered volcanic rocks were in contact with the ascending acid water. Full Text Available Diagnosis merupakan penentuan jenis-jenis penyakit berdasarkan penelitian sesuai dengan gejala-gejala yang dialami. Gejala gangguan penglihatan yang sering dialami adalah rabun. Rabun dapat berupa rabun melihat benda jauh, rabun melihat benda pada jarak dekat dan lain-lain. Semua jenis rabun mata pada intinya merupakan gangguan memfokuskan bayangan benda yang dilihat atau kelainan refraksi Ametropia.

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