Over 1 lakh installations with several prestigous and critical projects executed. New Branches open In Delhi, Chennai, Established PAN India Operations. Operations expand, Factory set up in Pune & Corporate Office in Mumbai. Corporates like SBI, AXIS Bank, ICICI Bank, NCR Corporation added as customers. The growing clientele of the company got a new vertical. Launch of its own brand IGBT based online ups. This opened doors with entry in SBI for supplying UPS systems in West Bengal & Bihar. The company started in Calcutta from a small room with voltage stabilizer as the first product.įirst prestigious project executed for BSNL Orissa. Smart and dynamic, Sourav thinks of inculcating new technologies in the business to spear head AVO’s growth in the next decade. As an aspiring new leader he has built his formative years in the company by front ending business development. Sourav heads the Roof Top Solar segment in Switching AVO. His leadership has led the company to the No. His vision for the company has been unmatched in establishing Switching AVO’s presence at the Pan India Level with 500 people, 21 branches and 150 centres. Rabindra Agarwal is the Managing Director, Switching AVO. in Electrical Engineering from Shivpur University, 1983 and serves as the Director and Head of Procurement, R&D at AVO. He believes in delivering value added services to his customers. Anup Agarwal championed the rise of Switching AVO within two decades of ground breaking solutions in Online UPS and Voltage Stabilizers. The presence of a larger volcanic system in the eastern IFM could influence magmatism and account for the multiple closely spaced volcanic centers in this region.Mr. These observations, combined with observations of vent orientation and morphology and gas flux, suggest the area between Cleveland and Tana represents a zone of complicated volcano-tectonic interaction, similar to calderas elsewhere in the Aleutian arc. These earthquakes have vertically-oriented P-axes and a greater percentage occur in families. VT hypocenters also extend ~7 km northeast of Cleveland's summit at depths of 5 to 10 km BSL, under a group of Holocene-aged vents between Mount Cleveland and Tana. The time-history of VT earthquakes and shallow LP events suggest their occurrence may track the transfer of magma and fluids from the mid-crust to the shallow portions of the conduit system and may provide a means to anticipate future explosions and periods of dome growth. These observations, and a relatively slow one-dimensional seismic velocity model, are consistent with a shallow body of magma that is fed through a deeper conduit system. VT focal mechanisms have horizontal P-axes that align with the regional axis of maximum stress. VT earthquakes beneath Mount Cleveland occur at depths of 2 to 8 km below sea level (BSL) and range in magnitude from −0.2 to 1.8. LP events appear to cluster at shallow depth beneath the active crater of Mount Cleveland and almost all of the explosions occur without identifiable short-term (hours to days) seismic precursors. This analysis reveals the full range of seismic event types expected in a highly active volcanic environment and includes Volcano-Tectonic (VT) earthquakes, Long-Period (LP) events, and explosion signals. We characterize seismicity beneath Chuginadak Island through automated analysis of event waveform frequency content, development of a one-dimensional P-wave velocity model, calculation of earthquake hypocenters, magnitudes, focal mechanisms, and identification of earthquake families. During the study period (July 2014–January 2019), eruptive activity at Cleveland was characterized by small explosions separated by periods of lava effusion that formed small domes in the volcano's summit crater. Collectively, these stations provided the first seismic observations of this frequently active volcano and the surrounding Holocene-aged volcanic vents. The Alaska Volcano Observatory (AVO) installed two permanent broadband seismometers on Chuginadak Island in 2014, and we operated a temporary broadband network focused on the western side of the island in 2015–2016. The persistently active Mount Cleveland volcano, on the western side of Chuginadak Island, is surrounded by several closely spaced Quaternary volcanic centers including Carlisle, Herbert, Kagamil, Tana, and Uliaga, and numerous small satellite vents on Chiginadak between Cleveland and Tana. Cleveland and Tana are remote volcanoes located in the central Aleutian volcanic arc on the eastern end of the Islands of Four Mountains (IFM).
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