By Francisco Gutiérrez, Mateo Gutiérrez
This is a hugely illustrated e-book with each one landform being defined with the subsequent constitution: (1) major features, together with geometric, morphometric and sedimentological positive factors. (2) Genetic techniques and controlling elements. (3) assorted typologies if appropriate. (4) extra reviews relating to numerous proper facets such us environmental implications or geographical distribution. picture visualization of landforms is key for studying geomorphology and stimulating the curiosity during this field-based topic; an image is worthy 1000 phrases. for this reason, the publication constitutes a important academic source for each collage scholar enrolled in classes comparable with earth floor approaches and landforms (e.g. Geomorphology, actual Geography, Geology, Geohazards, Environmental Sciences.). The e-book can also be appealing to visitors and folks partial to nature who need to know concerning the terminology and starting place of the landforms they stumble upon of their journeys. in lots of instances, the geomorphological positive factors represent the most asset of firstclass secure components (e.g., UNESCO global background websites, nationwide Parks).
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Extra resources for Landforms of the Earth: An Illustrated Guide
Sample text
Each embayment corresponds to the headscar of a landslide 50–150 km3 in volume, whose deposits have been identified in the adjacent seafloor. The major axis of the island is around 29 km (Image from © Google Earth) Fig. 8B Partial view of the 16 km long arcuate escarpment of Las Cañadas (Tenerife, Spain), which corresponds to the headscar of a multi-episodic flank collapse, occurred around 200 kyr ago. The erosional depression generated by this ca. 750 km3 mega-landslide has been partially filled by the Teide Volcano.
All Rights Reserved) 32 3 Tectonic Landforms Fig. 6D Pressure ridge (foreground) in a local zone of compression associated with the right-lateral Boconó fault in the Mucubají Lake area, Venezuela. The trace of the fault runs along the foot of the ridge. Faulted Pleistocene moraine in the background (Published with permission of © Franck Audemard 2015. 7 with scarps, troughs and benches parallel to the strike of the underlying beds. For instance, in slopes underlain by steeply dipping beds, outward toppling of the strata produces uphillfacing scarps (antislope scarps) and small half-graben depressions of their upslope side, which may disrupt drainages and act as sediment traps (Figs.
6 Landforms of Strike-Slip Faults 31 Fig. 6B Laterally offset transverse drainages on the right-lateral San Andreas Fault, Carrizo National Monument, California. The bayonet-like sharp bend of the channels indicates that the block on the upper right side of the fault moves towards the reader (Image from © Bing Maps) Fig. 6C Shutter ridge and offset-deflected drainage associated with a left-lateral oblique fault. The block on the downslope side moves up and to the left. The upslope-facing scarp of the shutter ridge has partially blocked a drainage, which is offset and deflected to the right.