By R. M. Teeuw
Read or Download Mapping Hazardous Terrain using Remote Sensing (Geological Society Special Publication No. 283) PDF
Similar geology books
For complicated undergraduate and starting graduate scholars in atmospheric, oceanic, and weather technological know-how, surroundings, Ocean and weather Dynamics is an introductory textbook at the circulations of the ambience and ocean and their interplay, with an emphasis on worldwide scales. it is going to provide scholars a great take hold of of what the ambience and oceans appear like at the large-scale and why they appear that manner.
Extraordinary detailed booklet discussing the earthquake that modified a few preconceived concepts concerning intracontinental mountain construction. good written and comprises the entire diagram inserts and maps. ebook in first-class form.
This publication describes porous media and the way their actual, petrophysical, mechanical, electrical and superficial houses are decided. the various measuring tools and the corresponding gear are defined. middle research (conventional or exact) required for any reservoir engineering operation or for utilizing mathematical versions is defined.
- Advances in Jurassic Research 2000. Proceedings of the Fifth International Symposium on the Jurassic System. R.L. Hall and P.L. Smith (Eds.), GeoResearch Forum 6
- Geology For Dummies
- Groundwater contamination inventory
- Evaporite basins
- Precambrian of the Northern Hemisphere
- Tectonic Geomorphology (2nd Edition)
Extra resources for Mapping Hazardous Terrain using Remote Sensing (Geological Society Special Publication No. 283)
International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, 35(B1), 445–452. , G UILLANDE , R. & H UAMAN , D. 1997. Mapping of lava flows through SPOT images—an example of the Sabancaya volcano (Peru). International Journal of Remote Sensing, 18, 3111– 3133. LPDAAC 2005. Land Processes Distributed Active Archive Center, Datapool @ LPDAAC. asp. , P ATRICK , M. & T RAUTWEIN , C. 2003. Estimating lava volume by precision combination of multiple baseline spaceborne and airborne interferometric synthetic aperture radar: the 1997 eruption of Okmok volcano.
Bjo¨rnsson (1998) described the caldera as being 6–10 km diameter, bordered by the mountain ridge Grı´msfjall to the south and subglacial mountains to the north and east (Fig. 1c). The Grı´msvo¨tn caldera is divided into three smaller calderas: the main (or south), north and east calderas (Guðmundsson & Milsom 1997). The subglacial lake covers the main caldera and extends into the northern depression at high water levels. The lake covers the areas of highest geothermal activity, and the eruptions in 1922, 1934, 1983, 1998 and 2004 all took place at its southern margin, where geothermal activity is also most intense (Guðmundsson & Bjo¨rnsson 1991).
B JO¨ RNSSON , H. & E INARSSON , P. 1990. Volcanoes beneath Vatnajo¨kull, Iceland: evidence from radio echo-sounding, earthquakes and jo¨kulhlaups. Jo¨kull, 40, 147–168. ¨ TN TEMPERATURE COMPARISONS, GRIMSVO B JO¨ RNSSON , H. & G UÐMUNDSSON , M. T. 1993. Variations in the thermal output of the subglacial Grı´msvo¨tn Caldera, Iceland. Geophysical Research Letters, 20, 2127–2130. , D AUTEUIL , O. & V AN V LEIT -L ANO¨ E , B. 1998. Pleistocene subglacial volcanism in Iceland: tectonic implications.