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We present two methods of spectral analysis that utilize LiDAR-derived digital elevation models of the Puget Sound lowlands, Washington, and the Tualatin Mountains, Oregon, to quantify and automatically map the topographic signatures of deep-seated landslides.
To map the topographic organization of azimuth preference, we plotted azimuth preference maps in which the preferred azimuth of each vertex was color coded and projected on the cortical surface.
To map the representation of the acoustic azimuth in human auditory cortex, we used a phase-encoding stimulation paradigm similar to the phase-encoding paradigms used to map the topographic organization of visual space in visual cortex (e.g., Engel et al. 1997) and the cochleotopic organization of auditory cortex (Striem-Amit et al. 2011).
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Figures 2, 3, 4, 5, and 6 show maps of the topographic correlation between both devices.
Contour and drainage lines were digitized from the topographic map and the geological map at hard copy was scanned and digitized.
Now, let's look at Map 3. Describe in as much detail as possible the topographic map and the terrain it represents.
First, let's look at Map 2. Describe in as much detail as possible the topographic map and the terrain it represents.
In that study, component definition relied on the magnitude of spatial correlation between the measured scalp potential field (i.e. the topographic map) at single time points and reference topographic maps for EP-components derived from a control group.
Indeed, the topographic map of Tutankhamun's chamber has already led an Egyptologist to a radical theory.
The topographic map of Paddington indicates exactly where to glimpse the terrace and gingerbread houses the neighborhood is famous for.
The pore-fluid pressure fields are superposed on the topographic map in (a, c).
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CEO of Professional Science Editing for Scientists @ prosciediting.com