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79 Cards in this Set
- Front
- Back
Types of vector data analysis
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buffering, overlay, distance measurement, network analysis
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Most common analysis of spatial data is what:
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buffer and overlay
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buffereing is:
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creating a proximity area around a selected point line, or polygon
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what is a buffer zone
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the newly created area within a specified distance from the selected features
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A buffere is a:
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polygon created at a specified distance from a point line or polygon
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a buffer around a point is:
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circular zones
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a buffer around a line is
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elongated polygons following the line feature, the polygong doenst' have to be on both sides of the line
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a buffer around a polygon is
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a zone extending outward from the polygon boundaries
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Buffer issues:
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1- you never want to forget the untits youw ant to use,
2- dissolving vs. not dissolving 3- use of different buffer distances 4-variation of buffere distances 5-multiple buffer zones 6-inclusions zones vx. exclusion zones |
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What is dissolving:
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removing intersects of buffer zones so it is one seamless polygon feature
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what is overlay:
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MOST POWERFUL feature of modern GIS.
It is the ablitly to place the cartographic representation of a thematic information of a selected theme over that of another |
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what is site suitablitly?
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examines social, economic, physical, biological and other criteria to locate potential sited for some purpose (part of overlay)
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what do overlay opperations combine:
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geometry and attributes of two feature maps to create an output
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Overlay procedure requires:
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an input map layre and an overlay map layer
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what can an output layer be in overlay:
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point, line, or polygon layer
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what must the overlay map layer and input map layer have in common:
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the same coordinate system
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The input layer can be what:
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a point, line or polygon
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The overlay layer must be a what:
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a polygon ***
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type of overlay polygong operations:
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1- point-in-polygon
2- line-in-polygon 3- polygon-in-polygon |
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What are the common overlay methods:
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union, intersect, and identity
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Union overlay method is what:
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-OR
-both input/overlay =polygon layers -combines the area extent from both maps |
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Intersect overlay method is what:
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= AND
-preserves only features that are within common area -output feature have attribute data from both layers -input layer can be a layer of point, line or polygon |
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Identity overlay method is what:
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= OR and AND [(Input layer) AND (overlay layer)] OR (input layer)
-preserves features that are within common area and features from input layer -input layer can be a layer of point, line or polygon |
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Buffers can be combined with what to analyze spaitail information:
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polygon overlayes
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What is vector line length:
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length of straight line calculated by pythagorean theorem using beginning and ending point locations
-length of curvillinear line calcultaed by adding lenghts of individual line segments -uses coordinate system to figure out measurements |
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To calculate area of vector polygon you:
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break complex polygon into simpler geometric shapes such as right triangles and rectangels whose area can be calculated
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Map manipulation is what:
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no attribute data combination, just about the geometry
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Examples of map manipulation are what:
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dissolve, clip, merge
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Map minipulation clipping is:
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cutting out a section of city (cookie cutting) ex. you could get jsut the roads of the city
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Map minipulation merging is what:
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seamless layer, erase
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Raster data analysis is based on what:
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based on cells and grids
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Raster data analysis can be performed on what:
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-individual cells
-a group of celss -an entire grid -a set of grids |
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Common Raster data anaylsis operations:
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-local operations
-neighborhood operations -zonal operations -distance measurements |
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What do you have to do before starting a raster data analysis:
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set up the environment covered by the analysis
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TO set up the env. covered by the analysis you can:
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-difine the extent of the environment (area extent-ArcView) (set window- ArcInfo)
-Define the size of the output grid cells (the size of the input grid cells) (set cell (ArcInfo)) |
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What is a mask grid in raster data anaylsis:
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-a grid (or set of grids) used as a way to difine the area extent of the analysis
-in that case the extent of the analysis is defined by the cells of the mask grid that do not have a value of "no data" ("no data" is different from the '0' value) |
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Raster data anaylsis common operation: LOCAL OPERATION
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-core raster data anaylsis
-consists of cell-by-cell operations based on preset or made up functions |
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Local operation: types of functions include:
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-arithmetic
-logartithmic -trigonometric -power *applied by one cell at a time *can be applied on single grid or with multiple grids |
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Local operations with a single grid:
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each cell value in the output grid is the result of the mathematical operation using the corresponding (overlapping) cell value in the input grid
ex. -floating point grid to integer grid -slope in percent to slope in degrees -universal soil loss equation |
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Local operations with several grids;
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-similar to vector overlay anaylsis
-allows more possiblities for local operations ex. the combine operation (several grids) |
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Raster data anaylsis common operation: NEIGHBORHOOD OPERATIONS
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-involves a focus cell and a set of cells in its vicinity (neighborhood)
-the value of the focus cell is computed with the values of the selected neighbor (surrounding) cells -the selection of surrounding cells is based on the distance &/or the directional relationships to the focus cells -the operation may or may not use the focus cell value |
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Some neighborhood operations:
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-* x-by-x window = (ex. 3x3) the focus cell is always in the middle (most commonly used)
-circle neighborhood= figure out radius of circle & figures out the cell values inside circle -Annulus = (doughnut shaped) cells that fall into the doughnut are used for computaion -wedge neighborhood= cells insde the wedge are used. ex. data simplification and terrain analysis |
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Raster data anaylsis common operation: ZONAL OPERATIONS
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*operation used to describe the geometry of zones (in a single grid) or to summarize the cells values by zone.
zones, disconnected zone, continuous zone |
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a zone is:
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connected (continous zone/1 region) or disconnected groups (2 regions)of cells with same values
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Characterisitcs of zonal operations:
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zonal operations are performed either on a -single grid (discription of zone geometry) or on two grids (summary of cell values by zones)
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Description of zone geometry (on single grid)
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area is the sum of cells times cell area
ex. cell size = 2m => Cell area = 4msquared |
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Zonal operations perimeter:
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it is the sum of the lengths of the boundary of each region of the zone
ex. cell size =2m Zone B : perimeter = 2x10=20m (you get 10 by counting the sides of the cells you want to caluculate) |
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Zonal operations thichness:
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radius (in cell length) of the largest circle that can be drawn within each zone
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Zonal operations centroid:
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consists of the parameters of the ellipse that best approximate each zone: centroid, major axis, minor axis
(major axis is the longest one, centroid is point in middle, minor axis is the smallest) |
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Using operation syntax to summarize cell values by zones (on two grids) you:
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used input, zonal operator, and zonal grid to get an output grid
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Raster data analysis common operation: DISTANCE MEASURE OPERATIONS
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-extended neighborhood operation or global operation
-it consists of calculated distances away from source cells in a single grid |
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Princle of distance computation:
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it is based on the node-link relationship
*node is VERY import. for computation - there are diagonal link, and lateral link , reference cell and direct neighbor cells |
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Princle of distance compuation:
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-its node represents its center
-its links are the segments connecting its node to the nodes of the adjacent celss -direct neighbor is a cell connected on the side (lateral link) -diagonal neighbor is a cell connected by its angle (diagonal link) |
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Line Length (raster)
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from node to node (not side to side)
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Physical distance measure of application of distance measurment operations:
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-straight-line distances away from source cells (similar to a buffer or source cells with continuous distance ex. buffer around stream network)
-reclassification=> discrete/homogeneous zone -slice operation => equal-area/equal-interval zones) -Allocation (allocaion grid, watershed) |
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Raster Anaylsis tools: overlays
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called Map Algebra (you can +, - , / ) can make use of more than 2 layers
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another name for terrain:
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land surface
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Land surfaces are:
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-undulated, continuous, and 3D
-they are measured and anylays generaged from elevation data |
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elevation data of land surfaces include:
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-slope(rate of change in elevation0
-apect (orientation of slope) -watershed -stream network -flow accumulation |
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The Z value in terrains:
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-represent the elevation data in GIS
-they are not stored as part of the coordinate system, but as attribute data (vector data z value sotred in numerical field of attribute tabel, in raster data z is stored as cell values in grid) |
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Common data for terrain analysis
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DEM and TIN
DEM- most common input data for terrain anayl. -its quality determines the accuracy of the anaylsis -needs to be converted to specific software format (grid for ArcView/ArcGIS/ArcInfo) |
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Terrain Maping includes:
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contouring, vertical profiling, hill shading, hypsometric tinting, and 3D View
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Terrain Maping CONTOURING:
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ISOLINE-line connecting points of equal value in a thematic map
CONTOUR LINE: line connecting points of euql elevation-it is the isoline for a topographic map CONTOUR INTERVAL- verticle distance between two consecutive contour lines |
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Goal of contouring:
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gerated contour line or isoline to show the distribution of continous phenomenon
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Caseof elevation in contouring:
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-close contour line=>steep terrain
-'V' indicate stream direction (pointing upstream) -traditionally helps calculate slope |
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Terrain Maping: VERTICAL PROFILING:
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construction of diagram showing the change in elevation along a line on a map
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Goal of Vertical Profiling:
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vizualize the changes in elevation along a linear feature of the map, or along a user difined line
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Terain Mapping: HILL SHADING:
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it is the simulation of the image of a terrain under the sun light
-slope facing incoming light are bright while slopes opposite to the sun are dark |
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Goal of Hill shading:
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display the shape of lang features
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Hill shading is also called:
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shaded relief and shading
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Terrain Maping: HYPSOMETRIC TINTING
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consists of displaying the elevation zones in different colors
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Goal of hypsometric tinting:
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to visualize the progression in elevation
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Another name for hypsometric tinting
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layer tinting
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Terain mapping:PERSPECTIVE VIEW (3D)
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it is the thre dimensional view of the terrain
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Perspective View is controlled by 4 parameters:
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1) The viewing azimuth- angle between north and the line defined by the target (on the surface) and the point of observation=> 0`-360`
2)the viewing angle- angle between the surface (horizontal) and the line defined by the target (on the surface) and the point of observation=> 0`-90` (@90` no longer view it as 3D but as 2D) 3) the view distance- distance b/w the ovbservation point and the target 4) the z-scale or verticle exaggeration factor- ratio b/w the verticle and horizonal scales |
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Terrain Mappaing: 3D DRAPING-
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superimposition of thematic layers with a perspective view
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Terrain anaylsis- SLOPE:
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it is the rate of change in elevation
-percent slope= (verticle distance/horizontal distance)x100 -degree slope= arctan (verticle distance/horiz. distance) |
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Terrain anaylsis- ASPECT:
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it is the orientation of slope (you can use 0`- 360` or cardinal orientation
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Terrain anaylsis- VIEWSHED ANALYSIS:
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*consists of using elevation grids to generate topography related hydrology features such as: watershed and sub-watershed, stream network, flwo accumulation (depth)
-watershed=catchment=basin -DEM=> field elevation=> flow direction grid=> flwo accumulation grid |