arcgis pro Search Results


georeferenced in arcgis pro version 3.0.36056  (Esri inc)
90
Esri inc georeferenced in arcgis pro version 3.0.36056
( a ) Plan view and ( b ) vertical cross-section views of the upper part of the reservoir (brown) and the associated seismicity at the beginning of the eruptive earthquake swarm induced by the dike propagation, namely in the morning of 24 February 2021. In ( a ) the location of the 2021 eruption site at the surface is indicated (and its projection down to the reservoir (red broken line, also shown in c), as well as the M4.6 and M5.6 earthquakes (the epicentres) in relation to topography, including the landmark mountain Keilir. In ( b ) the earthquake swarm (and inferred dike) is viewed in a direction perpendicular to the inferred dike (along the normal to the dike-fracture plane). In ( c ) the earthquake swarm is viewed along the strike (direction) of the dike (along the normal to the dike-fracture opening or thickness). The dike-segment initially became arrested at a depth of ~ 2 km. The brownish volume is the high Vp/Vs anomaly (Vp/Vs > = 1.95) from the tomography in Fig. . This anomaly is interpreted as the shallowest part of the magma reservoir. Notice that the Vp/Vs anomaly is not resolved below the depth of 12 km . The 3D images were generated by Voxler, version 4 ( https://support.goldensoftware.com ), the map on the plan view was downloaded from Google Earth Pro version 7.3.6.10201 ( https://earth.google.com ) and georeferenced in <t>ArcGIS</t> Pro version 3.0.36056 ( https://www.esri.com ), and the figure prepared in Inkscape version 1.3.1 ( https://inkscape.org ).
Georeferenced In Arcgis Pro Version 3.0.36056, supplied by Esri inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/product/arcgis+pro/georeferenced+in+arcgis+pro+version+3+0+36056/pmc12069532-123-32-37
Average 90 stars, based on 1 article reviews
georeferenced in arcgis pro version 3.0.36056 - by Bioz Stars, 2026-10
90/100 stars
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arcgis pro 10.0  (Esri inc)
90
Esri inc arcgis pro 10.0
( a ) Plan view and ( b ) vertical cross-section views of the upper part of the reservoir (brown) and the associated seismicity at the beginning of the eruptive earthquake swarm induced by the dike propagation, namely in the morning of 24 February 2021. In ( a ) the location of the 2021 eruption site at the surface is indicated (and its projection down to the reservoir (red broken line, also shown in c), as well as the M4.6 and M5.6 earthquakes (the epicentres) in relation to topography, including the landmark mountain Keilir. In ( b ) the earthquake swarm (and inferred dike) is viewed in a direction perpendicular to the inferred dike (along the normal to the dike-fracture plane). In ( c ) the earthquake swarm is viewed along the strike (direction) of the dike (along the normal to the dike-fracture opening or thickness). The dike-segment initially became arrested at a depth of ~ 2 km. The brownish volume is the high Vp/Vs anomaly (Vp/Vs > = 1.95) from the tomography in Fig. . This anomaly is interpreted as the shallowest part of the magma reservoir. Notice that the Vp/Vs anomaly is not resolved below the depth of 12 km . The 3D images were generated by Voxler, version 4 ( https://support.goldensoftware.com ), the map on the plan view was downloaded from Google Earth Pro version 7.3.6.10201 ( https://earth.google.com ) and georeferenced in <t>ArcGIS</t> Pro version 3.0.36056 ( https://www.esri.com ), and the figure prepared in Inkscape version 1.3.1 ( https://inkscape.org ).
Arcgis Pro 10.0, supplied by Esri inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/product/arcgis+pro/arcgis+pro+10+0/pm34450673-34-18-21
Average 90 stars, based on 1 article reviews
arcgis pro 10.0 - by Bioz Stars, 2026-10
90/100 stars
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arcgis pro  (Esri inc)
90
Esri inc arcgis pro
( a ) Plan view and ( b ) vertical cross-section views of the upper part of the reservoir (brown) and the associated seismicity at the beginning of the eruptive earthquake swarm induced by the dike propagation, namely in the morning of 24 February 2021. In ( a ) the location of the 2021 eruption site at the surface is indicated (and its projection down to the reservoir (red broken line, also shown in c), as well as the M4.6 and M5.6 earthquakes (the epicentres) in relation to topography, including the landmark mountain Keilir. In ( b ) the earthquake swarm (and inferred dike) is viewed in a direction perpendicular to the inferred dike (along the normal to the dike-fracture plane). In ( c ) the earthquake swarm is viewed along the strike (direction) of the dike (along the normal to the dike-fracture opening or thickness). The dike-segment initially became arrested at a depth of ~ 2 km. The brownish volume is the high Vp/Vs anomaly (Vp/Vs > = 1.95) from the tomography in Fig. . This anomaly is interpreted as the shallowest part of the magma reservoir. Notice that the Vp/Vs anomaly is not resolved below the depth of 12 km . The 3D images were generated by Voxler, version 4 ( https://support.goldensoftware.com ), the map on the plan view was downloaded from Google Earth Pro version 7.3.6.10201 ( https://earth.google.com ) and georeferenced in <t>ArcGIS</t> Pro version 3.0.36056 ( https://www.esri.com ), and the figure prepared in Inkscape version 1.3.1 ( https://inkscape.org ).
Arcgis Pro, supplied by Esri inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/product/arcgis+pro/arcgis+pro/pmc09439275-36-5-7
Average 90 stars, based on 1 article reviews
arcgis pro - by Bioz Stars, 2026-10
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arcgis desktop v10.8.1  (Esri inc)
90
Esri inc arcgis desktop v10.8.1
( a ) Plan view and ( b ) vertical cross-section views of the upper part of the reservoir (brown) and the associated seismicity at the beginning of the eruptive earthquake swarm induced by the dike propagation, namely in the morning of 24 February 2021. In ( a ) the location of the 2021 eruption site at the surface is indicated (and its projection down to the reservoir (red broken line, also shown in c), as well as the M4.6 and M5.6 earthquakes (the epicentres) in relation to topography, including the landmark mountain Keilir. In ( b ) the earthquake swarm (and inferred dike) is viewed in a direction perpendicular to the inferred dike (along the normal to the dike-fracture plane). In ( c ) the earthquake swarm is viewed along the strike (direction) of the dike (along the normal to the dike-fracture opening or thickness). The dike-segment initially became arrested at a depth of ~ 2 km. The brownish volume is the high Vp/Vs anomaly (Vp/Vs > = 1.95) from the tomography in Fig. . This anomaly is interpreted as the shallowest part of the magma reservoir. Notice that the Vp/Vs anomaly is not resolved below the depth of 12 km . The 3D images were generated by Voxler, version 4 ( https://support.goldensoftware.com ), the map on the plan view was downloaded from Google Earth Pro version 7.3.6.10201 ( https://earth.google.com ) and georeferenced in <t>ArcGIS</t> Pro version 3.0.36056 ( https://www.esri.com ), and the figure prepared in Inkscape version 1.3.1 ( https://inkscape.org ).
Arcgis Desktop V10.8.1, supplied by Esri inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/product/arcgis+pro/arcgis+pro+2+8/pmc09596447-189-4-7
Average 90 stars, based on 1 article reviews
arcgis desktop v10.8.1 - by Bioz Stars, 2026-10
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arcgis pro 3.1 software  (Esri inc)
90
Esri inc arcgis pro 3.1 software
( a ) Plan view and ( b ) vertical cross-section views of the upper part of the reservoir (brown) and the associated seismicity at the beginning of the eruptive earthquake swarm induced by the dike propagation, namely in the morning of 24 February 2021. In ( a ) the location of the 2021 eruption site at the surface is indicated (and its projection down to the reservoir (red broken line, also shown in c), as well as the M4.6 and M5.6 earthquakes (the epicentres) in relation to topography, including the landmark mountain Keilir. In ( b ) the earthquake swarm (and inferred dike) is viewed in a direction perpendicular to the inferred dike (along the normal to the dike-fracture plane). In ( c ) the earthquake swarm is viewed along the strike (direction) of the dike (along the normal to the dike-fracture opening or thickness). The dike-segment initially became arrested at a depth of ~ 2 km. The brownish volume is the high Vp/Vs anomaly (Vp/Vs > = 1.95) from the tomography in Fig. . This anomaly is interpreted as the shallowest part of the magma reservoir. Notice that the Vp/Vs anomaly is not resolved below the depth of 12 km . The 3D images were generated by Voxler, version 4 ( https://support.goldensoftware.com ), the map on the plan view was downloaded from Google Earth Pro version 7.3.6.10201 ( https://earth.google.com ) and georeferenced in <t>ArcGIS</t> Pro version 3.0.36056 ( https://www.esri.com ), and the figure prepared in Inkscape version 1.3.1 ( https://inkscape.org ).
Arcgis Pro 3.1 Software, supplied by Esri inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/product/arcgis+pro/arcgis+pro+3+0/pmc10560007-100-9-15
Average 90 stars, based on 1 article reviews
arcgis pro 3.1 software - by Bioz Stars, 2026-10
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drone imagery esri arcgis pro v3.0.1  (Esri inc)
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Esri inc drone imagery esri arcgis pro v3.0.1
( a ) Plan view and ( b ) vertical cross-section views of the upper part of the reservoir (brown) and the associated seismicity at the beginning of the eruptive earthquake swarm induced by the dike propagation, namely in the morning of 24 February 2021. In ( a ) the location of the 2021 eruption site at the surface is indicated (and its projection down to the reservoir (red broken line, also shown in c), as well as the M4.6 and M5.6 earthquakes (the epicentres) in relation to topography, including the landmark mountain Keilir. In ( b ) the earthquake swarm (and inferred dike) is viewed in a direction perpendicular to the inferred dike (along the normal to the dike-fracture plane). In ( c ) the earthquake swarm is viewed along the strike (direction) of the dike (along the normal to the dike-fracture opening or thickness). The dike-segment initially became arrested at a depth of ~ 2 km. The brownish volume is the high Vp/Vs anomaly (Vp/Vs > = 1.95) from the tomography in Fig. . This anomaly is interpreted as the shallowest part of the magma reservoir. Notice that the Vp/Vs anomaly is not resolved below the depth of 12 km . The 3D images were generated by Voxler, version 4 ( https://support.goldensoftware.com ), the map on the plan view was downloaded from Google Earth Pro version 7.3.6.10201 ( https://earth.google.com ) and georeferenced in <t>ArcGIS</t> Pro version 3.0.36056 ( https://www.esri.com ), and the figure prepared in Inkscape version 1.3.1 ( https://inkscape.org ).
Drone Imagery Esri Arcgis Pro V3.0.1, supplied by Esri inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/product/arcgis+pro/arcgis+software+esri+arcgis+pro+v3+0+1+x64/10__1002_slash_rse2__401-103-12-14
Average 90 stars, based on 1 article reviews
drone imagery esri arcgis pro v3.0.1 - by Bioz Stars, 2026-10
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arcgis pro software  (Esri inc)
90
Esri inc arcgis pro software
( a ) Plan view and ( b ) vertical cross-section views of the upper part of the reservoir (brown) and the associated seismicity at the beginning of the eruptive earthquake swarm induced by the dike propagation, namely in the morning of 24 February 2021. In ( a ) the location of the 2021 eruption site at the surface is indicated (and its projection down to the reservoir (red broken line, also shown in c), as well as the M4.6 and M5.6 earthquakes (the epicentres) in relation to topography, including the landmark mountain Keilir. In ( b ) the earthquake swarm (and inferred dike) is viewed in a direction perpendicular to the inferred dike (along the normal to the dike-fracture plane). In ( c ) the earthquake swarm is viewed along the strike (direction) of the dike (along the normal to the dike-fracture opening or thickness). The dike-segment initially became arrested at a depth of ~ 2 km. The brownish volume is the high Vp/Vs anomaly (Vp/Vs > = 1.95) from the tomography in Fig. . This anomaly is interpreted as the shallowest part of the magma reservoir. Notice that the Vp/Vs anomaly is not resolved below the depth of 12 km . The 3D images were generated by Voxler, version 4 ( https://support.goldensoftware.com ), the map on the plan view was downloaded from Google Earth Pro version 7.3.6.10201 ( https://earth.google.com ) and georeferenced in <t>ArcGIS</t> Pro version 3.0.36056 ( https://www.esri.com ), and the figure prepared in Inkscape version 1.3.1 ( https://inkscape.org ).
Arcgis Pro Software, supplied by Esri inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/product/arcgis+pro/arcgis+pro+software/pmc11076619-136-11-16
Average 90 stars, based on 1 article reviews
arcgis pro software - by Bioz Stars, 2026-10
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arcgis pro version 3.0 basemap  (Esri inc)
90
Esri inc arcgis pro version 3.0 basemap
( a ) Plan view and ( b ) vertical cross-section views of the upper part of the reservoir (brown) and the associated seismicity at the beginning of the eruptive earthquake swarm induced by the dike propagation, namely in the morning of 24 February 2021. In ( a ) the location of the 2021 eruption site at the surface is indicated (and its projection down to the reservoir (red broken line, also shown in c), as well as the M4.6 and M5.6 earthquakes (the epicentres) in relation to topography, including the landmark mountain Keilir. In ( b ) the earthquake swarm (and inferred dike) is viewed in a direction perpendicular to the inferred dike (along the normal to the dike-fracture plane). In ( c ) the earthquake swarm is viewed along the strike (direction) of the dike (along the normal to the dike-fracture opening or thickness). The dike-segment initially became arrested at a depth of ~ 2 km. The brownish volume is the high Vp/Vs anomaly (Vp/Vs > = 1.95) from the tomography in Fig. . This anomaly is interpreted as the shallowest part of the magma reservoir. Notice that the Vp/Vs anomaly is not resolved below the depth of 12 km . The 3D images were generated by Voxler, version 4 ( https://support.goldensoftware.com ), the map on the plan view was downloaded from Google Earth Pro version 7.3.6.10201 ( https://earth.google.com ) and georeferenced in <t>ArcGIS</t> Pro version 3.0.36056 ( https://www.esri.com ), and the figure prepared in Inkscape version 1.3.1 ( https://inkscape.org ).
Arcgis Pro Version 3.0 Basemap, supplied by Esri inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/product/arcgis+pro/arcgis+pro+version+3+0+basemap/pm40593973-66-9-8
Average 90 stars, based on 1 article reviews
arcgis pro version 3.0 basemap - by Bioz Stars, 2026-10
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arcgis pro 3.4  (Esri inc)
90
Esri inc arcgis pro 3.4
( a ) Plan view and ( b ) vertical cross-section views of the upper part of the reservoir (brown) and the associated seismicity at the beginning of the eruptive earthquake swarm induced by the dike propagation, namely in the morning of 24 February 2021. In ( a ) the location of the 2021 eruption site at the surface is indicated (and its projection down to the reservoir (red broken line, also shown in c), as well as the M4.6 and M5.6 earthquakes (the epicentres) in relation to topography, including the landmark mountain Keilir. In ( b ) the earthquake swarm (and inferred dike) is viewed in a direction perpendicular to the inferred dike (along the normal to the dike-fracture plane). In ( c ) the earthquake swarm is viewed along the strike (direction) of the dike (along the normal to the dike-fracture opening or thickness). The dike-segment initially became arrested at a depth of ~ 2 km. The brownish volume is the high Vp/Vs anomaly (Vp/Vs > = 1.95) from the tomography in Fig. . This anomaly is interpreted as the shallowest part of the magma reservoir. Notice that the Vp/Vs anomaly is not resolved below the depth of 12 km . The 3D images were generated by Voxler, version 4 ( https://support.goldensoftware.com ), the map on the plan view was downloaded from Google Earth Pro version 7.3.6.10201 ( https://earth.google.com ) and georeferenced in <t>ArcGIS</t> Pro version 3.0.36056 ( https://www.esri.com ), and the figure prepared in Inkscape version 1.3.1 ( https://inkscape.org ).
Arcgis Pro 3.4, supplied by Esri inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/product/arcgis+pro/arcgis+pro+version+3+4/pm40393338-69-16-19
Average 90 stars, based on 1 article reviews
arcgis pro 3.4 - by Bioz Stars, 2026-10
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esri arcgis pro  (Esri inc)
90
Esri inc esri arcgis pro
( a ) Plan view and ( b ) vertical cross-section views of the upper part of the reservoir (brown) and the associated seismicity at the beginning of the eruptive earthquake swarm induced by the dike propagation, namely in the morning of 24 February 2021. In ( a ) the location of the 2021 eruption site at the surface is indicated (and its projection down to the reservoir (red broken line, also shown in c), as well as the M4.6 and M5.6 earthquakes (the epicentres) in relation to topography, including the landmark mountain Keilir. In ( b ) the earthquake swarm (and inferred dike) is viewed in a direction perpendicular to the inferred dike (along the normal to the dike-fracture plane). In ( c ) the earthquake swarm is viewed along the strike (direction) of the dike (along the normal to the dike-fracture opening or thickness). The dike-segment initially became arrested at a depth of ~ 2 km. The brownish volume is the high Vp/Vs anomaly (Vp/Vs > = 1.95) from the tomography in Fig. . This anomaly is interpreted as the shallowest part of the magma reservoir. Notice that the Vp/Vs anomaly is not resolved below the depth of 12 km . The 3D images were generated by Voxler, version 4 ( https://support.goldensoftware.com ), the map on the plan view was downloaded from Google Earth Pro version 7.3.6.10201 ( https://earth.google.com ) and georeferenced in <t>ArcGIS</t> Pro version 3.0.36056 ( https://www.esri.com ), and the figure prepared in Inkscape version 1.3.1 ( https://inkscape.org ).
Esri Arcgis Pro, supplied by Esri inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/product/arcgis+pro/esri+arcgis+pro/pm39213853-113-9-9
Average 90 stars, based on 1 article reviews
esri arcgis pro - by Bioz Stars, 2026-10
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program esri arcgis pro v.2.4  (Esri inc)
90
Esri inc program esri arcgis pro v.2.4
Mosquito collection sites in North America ( a ) and Eurasia ( b ). Worldwide distribution of Cx. pipiens and Cx. quinquefasciatus is indicated by blue color and green lines. The overlap between the sheds represents a species hybrid zone indicating that collections in the USA (Chicago, IL and Washington, D.C.) were made within the hybrid zone. The map was created using program <t>ESRI</t> <t>ArcGis</t> Pro v.2.4 ( https://www.esri.com/ ). The species distributions are shown according to previously published data .
Program Esri Arcgis Pro V.2.4, supplied by Esri inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/product/arcgis+pro/program+esri+arcgis+pro+v+2+4/pmc07200692-64-5-6
Average 90 stars, based on 1 article reviews
program esri arcgis pro v.2.4 - by Bioz Stars, 2026-10
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multivariate clustering algorithm in arcgis pro  (Esri inc)
90
Esri inc multivariate clustering algorithm in arcgis pro
Mosquito collection sites in North America ( a ) and Eurasia ( b ). Worldwide distribution of Cx. pipiens and Cx. quinquefasciatus is indicated by blue color and green lines. The overlap between the sheds represents a species hybrid zone indicating that collections in the USA (Chicago, IL and Washington, D.C.) were made within the hybrid zone. The map was created using program <t>ESRI</t> <t>ArcGis</t> Pro v.2.4 ( https://www.esri.com/ ). The species distributions are shown according to previously published data .
Multivariate Clustering Algorithm In Arcgis Pro, supplied by Esri inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
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Image Search Results


( a ) Plan view and ( b ) vertical cross-section views of the upper part of the reservoir (brown) and the associated seismicity at the beginning of the eruptive earthquake swarm induced by the dike propagation, namely in the morning of 24 February 2021. In ( a ) the location of the 2021 eruption site at the surface is indicated (and its projection down to the reservoir (red broken line, also shown in c), as well as the M4.6 and M5.6 earthquakes (the epicentres) in relation to topography, including the landmark mountain Keilir. In ( b ) the earthquake swarm (and inferred dike) is viewed in a direction perpendicular to the inferred dike (along the normal to the dike-fracture plane). In ( c ) the earthquake swarm is viewed along the strike (direction) of the dike (along the normal to the dike-fracture opening or thickness). The dike-segment initially became arrested at a depth of ~ 2 km. The brownish volume is the high Vp/Vs anomaly (Vp/Vs > = 1.95) from the tomography in Fig. . This anomaly is interpreted as the shallowest part of the magma reservoir. Notice that the Vp/Vs anomaly is not resolved below the depth of 12 km . The 3D images were generated by Voxler, version 4 ( https://support.goldensoftware.com ), the map on the plan view was downloaded from Google Earth Pro version 7.3.6.10201 ( https://earth.google.com ) and georeferenced in ArcGIS Pro version 3.0.36056 ( https://www.esri.com ), and the figure prepared in Inkscape version 1.3.1 ( https://inkscape.org ).

Journal: Scientific Reports

Article Title: Tomographic and volcanotectonic control on the 2021–2023 Fagradalsfjall eruptions, Iceland

doi: 10.1038/s41598-025-95169-6

Figure Lengend Snippet: ( a ) Plan view and ( b ) vertical cross-section views of the upper part of the reservoir (brown) and the associated seismicity at the beginning of the eruptive earthquake swarm induced by the dike propagation, namely in the morning of 24 February 2021. In ( a ) the location of the 2021 eruption site at the surface is indicated (and its projection down to the reservoir (red broken line, also shown in c), as well as the M4.6 and M5.6 earthquakes (the epicentres) in relation to topography, including the landmark mountain Keilir. In ( b ) the earthquake swarm (and inferred dike) is viewed in a direction perpendicular to the inferred dike (along the normal to the dike-fracture plane). In ( c ) the earthquake swarm is viewed along the strike (direction) of the dike (along the normal to the dike-fracture opening or thickness). The dike-segment initially became arrested at a depth of ~ 2 km. The brownish volume is the high Vp/Vs anomaly (Vp/Vs > = 1.95) from the tomography in Fig. . This anomaly is interpreted as the shallowest part of the magma reservoir. Notice that the Vp/Vs anomaly is not resolved below the depth of 12 km . The 3D images were generated by Voxler, version 4 ( https://support.goldensoftware.com ), the map on the plan view was downloaded from Google Earth Pro version 7.3.6.10201 ( https://earth.google.com ) and georeferenced in ArcGIS Pro version 3.0.36056 ( https://www.esri.com ), and the figure prepared in Inkscape version 1.3.1 ( https://inkscape.org ).

Article Snippet: The 3D images were generated by Voxler, version 4 ( https://support.goldensoftware.com ), the map on the plan view was downloaded from Google Earth Pro version 7.3.6.10201 ( https://earth.google.com ) and georeferenced in ArcGIS Pro version 3.0.36056 ( https://www.esri.com ), and the figure prepared in Inkscape version 1.3.1 ( https://inkscape.org ).

Techniques: Tomography, Generated

Mosquito collection sites in North America ( a ) and Eurasia ( b ). Worldwide distribution of Cx. pipiens and Cx. quinquefasciatus is indicated by blue color and green lines. The overlap between the sheds represents a species hybrid zone indicating that collections in the USA (Chicago, IL and Washington, D.C.) were made within the hybrid zone. The map was created using program ESRI ArcGis Pro v.2.4 ( https://www.esri.com/ ). The species distributions are shown according to previously published data .

Journal: Scientific Reports

Article Title: Genomic differentiation and intercontinental population structure of mosquito vectors Culex pipiens pipiens and Culex pipiens molestus

doi: 10.1038/s41598-020-63305-z

Figure Lengend Snippet: Mosquito collection sites in North America ( a ) and Eurasia ( b ). Worldwide distribution of Cx. pipiens and Cx. quinquefasciatus is indicated by blue color and green lines. The overlap between the sheds represents a species hybrid zone indicating that collections in the USA (Chicago, IL and Washington, D.C.) were made within the hybrid zone. The map was created using program ESRI ArcGis Pro v.2.4 ( https://www.esri.com/ ). The species distributions are shown according to previously published data .

Article Snippet: The map was created using program ESRI ArcGis Pro v.2.4 ( https://www.esri.com/ ).

Techniques: