Two rubbersheeting options are supported.
Rubber sheeting arcgis 10 1.
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Spatial adjustment rubbersheeting makes small geometric adjustments in your data usually to align features with more accurate information.
Arcgis help 10 1 about spatial adjustment rubbersheeting about spatial adjustment rubbersheeting geometric distortions commonly occur in source maps.
See about spatial adjustment rubbersheeting for more details.
For the tension spline method the weight parameter defines the weight of tension.
Rubbersheeting is typically used to align two or more layers.
Linear this method creates a quick tin surface but does not really take into account the neighborhood.
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Types of geometric transformations include rubber sheeting usually used for georeferencing projection using the projection information to transform the data from one projection to another translation shifting all the coordinates equally rotation rotating all the coordinates by some angle and changing the cell size of the dataset.
The z value is the amount of change between the from end and to end of a link.
Natural neighbor and linear.
This process moves the features of a layer using a piecewise transformation that preserves straight lines.
Before performing spatial adjustment rubbersheeting you need to choose an adjustment method.
The typical values are 0 1 5 and 10.
The higher the weight the coarser the output surface.
For example if the change in x for a link is 10 map units the z value of the tin node at the from end of that link will be 10.
Arcgis tutorial data for desktop data path.
Rubber sheeting spatial adjustment of a feature class in arcgis.
The values entered must be equal to or greater than zero.
The z value of each node is used to interpolate the amount of x y adjustment applied to each feature coordinate.
The typical values that may be used are 0 0 001 0 01 0 1 and 0 5.
It is slightly faster and produces good results when you have many rubbersheet links spread uniformly over the data.