Sentence examples for map of volcanic from inspiring English sources

Fig. 10 a Hazard map of volcanic ash load (kg/m2) for Indonesia at 1 km resolution for the 1000 year timeframe; (b) Annual exceedance probability curve versus ash load for a site in Jakarta and (c) Histogram disaggregating the % contribution to ash load hazard of magnitude (VEI) for each source at the site in Jakarta for the 1000 year timeframe.

Fig. 6 Hazard maps of volcanic ash load at 1 km resolution for the 1000 year timeframe for a Indonesia, b Japan, c the Philippines and d Papua New Guinea.

The mapping of volcanic activity such as lava and pyroclastic flows and mudflows on a real-time basis during eruptions is very important for event monitoring and prediction for disaster mitigation.

These factors are dependent on how the reader interprets and understands the hazard map, a facet of volcanic hazard communication that has been relatively unexplored.

The database of results obtained for a grid of sites can be aggregated to generate maps of expected volcanic ash load at different timeframes or disaggregated by event in order to determine the percentage contribution to the hazard by magnitude, distance, source etc.

To make a hazard map for volcanic ballistic projectiles, it is necessary to estimate the travel distance, landing velocity, and landing energy of the ballistic projectiles.

Houlié et al. (2005) suggested the possibility of detecting and mapping the temperature of volcanic plumes using Global Positioning System (GPS) data, based on an analysis of the eruption event at Miyakejima volcano (Japan) on August 18, 2000.

Figure 1 Map of the Auckland Volcanic Field.

Figure 8 Uniform hazard map of the Auckland Volcanic Field.

A map of maximum expected volcanic ash load on a 1-km grid for Papua New Guinea is presented for a 1-in-1000 year event in Fig. 6.

A map of maximum expected volcanic ash load on a 1-km grid for Indonesia is presented here for a 1-in-1000 year event in Fig. 6.