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Revert "Include calcite font resource in UWP project (#1545)"
This reverts commit 59723ec. Revert "Update link in readme to .NET API reference." This reverts commit c5b3329. Revert "Update link in readme to .NET API reference." This reverts commit 628f2dd. Revert "Update src/MAUI/Maui.Samples/Samples/Geometry/Buffer/readme.md" This reverts commit e119d4e. Revert "Adding new lines to EOF" This reverts commit 3bfea1d. Revert "Update readme with geodesic buffer details and link" This reverts commit 25fdc73. Revert "Update link in readme to .NET API reference." This reverts commit 7e3fcbf.
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Diff for: src/MAUI/Maui.Samples/Samples/Geometry/Buffer/readme.md

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@@ -12,7 +12,7 @@ Creating buffers is a core concept in GIS proximity analysis that allows you to
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1. Tap on the map.
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2. A planar and a geodesic buffer will be created at the tap location using the distance (miles) specified in the text box.
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3. Continue tapping to create additional buffers. Notice that buffers closer to the equator appear similar in size. As you move north or south from the equator, however, the geodesic polygons become much larger. Geodesic polygons are in fact a better representation of the true shape and size of the buffer. Geodesic buffers will not be generated for points placed beyond +/-90 degrees latitude.
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3. Continue tapping to create additional buffers. Notice that buffers closer to the equator appear similar in size. As you move north or south from the equator, however, the geodesic polygons become much larger. Geodesic polygons are in fact a better representation of the true shape and size of the buffer.
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4. Tap `Clear` to remove all buffers and start again.
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## How it works
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Buffers can be generated as either `planar` (flat - coordinate space of the map's spatial reference) or `geodesic` (technique that considers the curved shape of the Earth's surface, which is generally a more accurate representation). In general, distortion in the map increases as you move away from the standard parallels of the spatial reference's projection. This map is in Web Mercator so areas near the equator are the most accurate. As you move the buffer location north or south from that line, you'll see a greater difference in the polygon size and shape. Planar operations are generally faster, but performance improvement may only be noticeable for large operations (buffering a great number or complex geometry).
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Geodesic buffers in the far northern and southern regions of the map will extend beyond the map's limits. The visible extent of the basemap in this sample is limited to between approximately +/-85 degrees latitude while geodesic buffers are calculated to extend all the way to the poles (+/-90 degrees). Also, since map view wraparound is active, geodesic buffers that cross the international date line (180 degrees longitude) will be [normalized](https://developers.arcgis.com/net/api-reference/api/net/Esri.ArcGISRuntime/Esri.ArcGISRuntime.Geometry.GeometryEngine.NormalizeCentralMeridian.html), resulting in a multipart geometry. This results in a vertical line in the buffer graphic at the dateline.
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For more information about using buffer analysis, see the topic [How Buffer (Analysis) works](https://pro.arcgis.com/en/pro-app/tool-reference/analysis/how-buffer-analysis-works.htm) in the *ArcGIS Pro* documentation.
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## Tags
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analysis, buffer, euclidean, geodesic, geometry, planar
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analysis, buffer, euclidean, geodesic, geometry, planar

Diff for: src/UWP/ArcGIS.UWP.Viewer/ArcGIS.UWP.Viewer.csproj

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<CopyToOutputDirectory>PreserveNewest</CopyToOutputDirectory>
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</Content>
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</ItemGroup>
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<ItemGroup>
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<Content Include="Resources\Fonts\calcite-ui-icons-24new.ttf" />
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</ItemGroup>
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<!-- Imports -->
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<Import Project="..\..\Samples.Shared\ArcGIS.Samples.Shared.projitems" Label="Shared" />
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<PropertyGroup Condition=" '$(VisualStudioVersion)' == '' or '$(VisualStudioVersion)' &lt; '14.0' ">
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Diff for: src/WPF/WPF.Viewer/Samples/Geometry/Buffer/readme.md

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Original file line numberDiff line numberDiff line change
@@ -12,7 +12,7 @@ Creating buffers is a core concept in GIS proximity analysis that allows you to
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1. Tap on the map.
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2. A planar and a geodesic buffer will be created at the tap location using the distance (miles) specified in the text box.
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3. Continue tapping to create additional buffers. Notice that buffers closer to the equator appear similar in size. As you move north or south from the equator, however, the geodesic polygons become much larger. Geodesic polygons are in fact a better representation of the true shape and size of the buffer. Geodesic buffers will not be generated for points placed beyond +/-90 degrees latitude.
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3. Continue tapping to create additional buffers. Notice that buffers closer to the equator appear similar in size. As you move north or south from the equator, however, the geodesic polygons become much larger. Geodesic polygons are in fact a better representation of the true shape and size of the buffer.
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4. Click `Clear` to remove all buffers and start again.
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## How it works
@@ -32,10 +32,8 @@ Creating buffers is a core concept in GIS proximity analysis that allows you to
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Buffers can be generated as either `planar` (flat - coordinate space of the map's spatial reference) or `geodesic` (technique that considers the curved shape of the Earth's surface, which is generally a more accurate representation). In general, distortion in the map increases as you move away from the standard parallels of the spatial reference's projection. This map is in Web Mercator so areas near the equator are the most accurate. As you move the buffer location north or south from that line, you'll see a greater difference in the polygon size and shape. Planar operations are generally faster, but performance improvement may only be noticeable for large operations (buffering a great number or complex geometry).
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Geodesic buffers in the far northern and southern regions of the map will extend beyond the map's limits. The visible extent of the basemap in this sample is limited to between approximately +/-85 degrees latitude while geodesic buffers are calculated to extend all the way to the poles (+/-90 degrees). Also, since map view wraparound is active, geodesic buffers that cross the international date line (180 degrees longitude) will be [normalized](https://developers.arcgis.com/net/api-reference/api/net/Esri.ArcGISRuntime/Esri.ArcGISRuntime.Geometry.GeometryEngine.NormalizeCentralMeridian.html), resulting in a multipart geometry. This results in a vertical line in the buffer graphic at the dateline.
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For more information about using buffer analysis, see the topic [How Buffer (Analysis) works](https://pro.arcgis.com/en/pro-app/tool-reference/analysis/how-buffer-analysis-works.htm) in the *ArcGIS Pro* documentation.
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## Tags
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analysis, buffer, euclidean, geodesic, geometry, planar
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analysis, buffer, euclidean, geodesic, geometry, planar

Diff for: src/WinUI/ArcGIS.WinUI.Viewer/Samples/Geometry/Buffer/readme.md

+2-4
Original file line numberDiff line numberDiff line change
@@ -12,7 +12,7 @@ Creating buffers is a core concept in GIS proximity analysis that allows you to
1212

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1. Tap on the map.
1414
2. A planar and a geodesic buffer will be created at the tap location using the distance (miles) specified in the text box.
15-
3. Continue tapping to create additional buffers. Notice that buffers closer to the equator appear similar in size. As you move north or south from the equator, however, the geodesic polygons become much larger. Geodesic polygons are in fact a better representation of the true shape and size of the buffer. Geodesic buffers will not be generated for points placed beyond +/-90 degrees latitude.
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3. Continue tapping to create additional buffers. Notice that buffers closer to the equator appear similar in size. As you move north or south from the equator, however, the geodesic polygons become much larger. Geodesic polygons are in fact a better representation of the true shape and size of the buffer.
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4. Click `Clear` to remove all buffers and start again.
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## How it works
@@ -32,10 +32,8 @@ Creating buffers is a core concept in GIS proximity analysis that allows you to
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Buffers can be generated as either `planar` (flat - coordinate space of the map's spatial reference) or `geodesic` (technique that considers the curved shape of the Earth's surface, which is generally a more accurate representation). In general, distortion in the map increases as you move away from the standard parallels of the spatial reference's projection. This map is in Web Mercator so areas near the equator are the most accurate. As you move the buffer location north or south from that line, you'll see a greater difference in the polygon size and shape. Planar operations are generally faster, but performance improvement may only be noticeable for large operations (buffering a great number or complex geometry).
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Geodesic buffers in the far northern and southern regions of the map will extend beyond the map's limits. The visible extent of the basemap in this sample is limited to between approximately +/-85 degrees latitude while geodesic buffers are calculated to extend all the way to the poles (+/-90 degrees). Also, since map view wraparound is active, geodesic buffers that cross the international date line (180 degrees longitude) will be [normalized](https://developers.arcgis.com/net/api-reference/api/net/Esri.ArcGISRuntime/Esri.ArcGISRuntime.Geometry.GeometryEngine.NormalizeCentralMeridian.html), resulting in a multipart geometry. This results in a vertical line in the buffer graphic at the dateline.
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For more information about using buffer analysis, see the topic [How Buffer (Analysis) works](https://pro.arcgis.com/en/pro-app/tool-reference/analysis/how-buffer-analysis-works.htm) in the *ArcGIS Pro* documentation.
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## Tags
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analysis, buffer, euclidean, geodesic, geometry, planar
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analysis, buffer, euclidean, geodesic, geometry, planar

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