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Twitterhttps://pacific-data.sprep.org/resource/private-data-license-agreement-0https://pacific-data.sprep.org/resource/private-data-license-agreement-0
The report from the GIS conference that the SPREP GIS team participated in from 25 to 29 November
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TwitterIncludes links to various GIS events and conferences
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TwitterThese are the results of the survey "GIS Support on Campus", which was announced via email on May 13, 2014 to Gis4lib, HIGHERED-L, and MAPS-L. I have received requests to view the survey results; however, there was no statement about redistribution in the original survey, other than a presentation at the Esri Education GIS Conference 2014. To ensure confidentiality for survey respondents, these results have been anonimized or aggregated where needed. The PDF of my presentation slides from the 2014 Esri Education GIS Conference can be accessed at http://proceedings.esri.com/library/userconf/educ14/index.html. Search for "Bringing It All Together: Rethinking GIS Support on Campus". If you have specific questions, feel free to email me at megan.slemons@emory.edu.
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TwitterProjects, data and layers required to complete workshops at the 2024 ODF GIS Conference. Download the zip file and extract the files to a location on your workstation.
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TwitterAn ArcGIS Hub site used by the general public to discover outdoor recreation opportunities.
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TwitterOur conference is the UK's largest GIS (Geographical Information Systems) event. GIS is a digital technology your student uses as part of their A Level studies. Y12 have already used GIS to take part in a day of action for the National Education Nature Park on their school site. On the 14th May, their findings will be presented to the attendees of conference, around 3000 professional geographers and GIS users. They will also have the opportunity to attend sessions that enhance their GIS skills and showcase the rewarding and engaging careers GIS can unlock.
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TwitterGIS Team Conference 2021July 20-22, 2021This storymap outlines the agenda/topics that will be covered by the various TEAMS "meetings" throughout the 3-day conference. All are welcome, however TEAMS meetings are capped at 1,000 attendees (wishful thinking, but hey? It could go viral...) So tell your co-workers, program managers, division directors, secretaries, and your cats that this will be helpful for all to understand the investment that we have in our GIT. Inspiration for your programs to begin conceptualizing solutions that leverage our existing GIS platforms that do not require any additional licensing.
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TwitterDo you have data and maps that you think others would benefit from using? Are you uncertain of the best ways to share this information with individuals, groups or even the public? What about updating the data? In this session, we will show you tips and tricks in ArcGIS Pro, ArcGIS Online and ArcGIS Enterprise that will help you unleash your data and maps to your desired audience.Details on the Esri Canada User Conferences can be found here.
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TwitterThe dataset is made publicly available as a GIS at nominal 1:5 000 000 scale, and shows the time-space-event distribution of mafic-ultramafic magmatism in Australia from the early Archean to the present day. Development of this GIS has been a multi-year project and earlier released extracts (in viewable pdf form with accompanying Geoscience Australia Records) included compilations for the Archean magmatic record, the Proterozoic magmatic record, and the Australian Large Igneous Provinces (LIPs). Publication of the GIS completes the series with addition of the Phanerozoic magmatic record, and formalisation of the complete record of Archean-Phanerozoic magmatic events as a single series. The chronology of Australian mafic-ultramafic magmatism resolves into 74 magmatic events within, predominately, resolvable bands of ±10 million years. Each event is identified by geological units grouped by similar age - this coeval magmatism may or may not be genetically related and may be in response to different geodynamic environments. These magmatic events range in age from the Eoarchean ~3730 Ma ME 1 - Manfred Event, confined within a small remnant domain within the Yilgarn Craton, to the widespread record of Cenozoic magmatism in eastern Australia (ME 72 to ME 74). The magmatic events range in magnitude from the giant volumes of magma in Large Igneous Provinces, to events whose only known occurrence is an isolated record of dated mafic igneous rock in a single drillhole. The GIS makes it possible to focus on the location of any one of these magmatic events, or groups of magmatic events that may be of interest, and overlay context from any other information that users may have available. The delineation of magmatic events for this study is based on several hundred published ages of mafic and ultramafic igneous rocks from different isotopic systems and minerals. In addition to their ages and extents, primary recorded aspects of each magmatic event include the presence or absence of ultramafic components. Further to this, the presence or correlation of known magmatic-related mineralisation is highlighted in Time-Space-Event Charts of Australia (Appendix D, figures D1 and D2). The basis for mapping has been regional solid geology, interpreted basement geology and surface geology base maps made available by the State and Northern Territory geological surveys, providing insight into the total areal extent of the magmatic systems under cover. Also available to complement the Event GIS are the domains and element boundaries from the Australian Crustal Elements map. These boundaries which are which are based on geophysical extrapolation of crustal elements under the cover of continental basins, provide a framework of the shallow crustal structure of the continent, and are used in this guide. The Crustal Elements digital dataset is available for download from the Geoscience Australia website. Insight into the geodynamic development of the continent is provided by the magmatic event structure through time. The compilation draws attention to concentrations of mafic-ultramafic magmatism in the Archean from ~2820-2665 Ma, in the Proterozoic from ~1870-1590 Ma, and in the late Neoproterozoic-Phanerozoic from ~530-225 Ma. These three time spans contain 39 of the 74 magmatic events, 53% of the entire mafic-ultramafic magmatic event record of the continent. The periods in between have mafic-ultramafic magmatic records that are more dispersed in time. Other features of interest include the shared geographic and crustal element locations of Large Igneous Provinces and numerous events with smaller magma volumes. Read the rest of the Executive Summary in the document.
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TwitterGIS in Education Award Nomination Form for Delmarva GIS Conference 2026 - FINAL
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TwitterInformation about events (for example: war, famine, mass migration) that have shaped a population, and the recognition of event significance within and beyond that population. Includes, for example, information about: historical events of influence (for example: those which have resulted in significant shifts in population characteristics, or which endure in traditions and ceremonies); and recent events that are 'newsworthy' and influence population attitudes and the policies of social groups. Natural disasters, such as tsunamis, earthquakes, and hurricanes/cyclones can be included.
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TwitterEvents are symbolized by their Seismic Magnitude regardless of age.
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TwitterFor the latter part of the 20th century, Northern Ireland, officially part of the United Kingdom but sharing an island with the Republic of Ireland, saw violence between the nationalists (mostly Roman Catholic background) and unionists (mostly Protestant background). The Good Friday Agreement of 1998 sought to end this conflict, by establishing peace between these two communities and guiding how Northern Ireland should be governed. But even 20 years on, Northern Ireland remains divided. Yet, hope is on the horizon. Young students in Lurgan—a town of 25,000 south of Belfast—are using Survey123 for ArcGIS to record data across sectarian lines. After analyzing the data collected, the students from conflicting backgrounds find that they aren't that different after all. This is how change begins. Join the students of Lurgan to learn how youth are using GIS to make a difference in their community.
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TwitterWildland fire event polygons for 2004-2017 reconciled in SmartFire 2 for the EPA Air Quality Times Series (EQUATES) modeling project (https://doi.org/10.1016/j.dib.2023.109022). These event polygons represent a combination of properties from a collection of remotely sensed and ground-based fire activity datasets. The primary underlying fire activity datasets for the fire event polygons are the Hazard Mapping System (HMS) remote sense fire product (https://www.ospo.noaa.gov/Products/land/hms.html), SIT-ICS/209 Incident Reports (https://www.wildfire.gov/application/sit209), GeoMAC Fire Event polygons (https://data-nifc.opendata.arcgis.com/datasets/nifc::historic-perimeters-combined-2000-2018-geomac/about), and the Monitoring Trends in Burn Severity (MTBS) burn scar event perimeters (https://www.mtbs.gov/direct-download). This dataset includes events identified as over wildland and does not contain biomass burning events over agricultural areas, such as crop residue field burns. Additionally, certain grass fires, such as the annual prescribed fires in the Flint Hills region, have been removed for inclusion in a separate processing stream. Some minor updates have been made to the dataset since the publishing of the EQUATES emission inventories including removal of known errors related to issues in the underlying activity. This dataset is associated with the following publication: Beidler, J., G. Pouliot, and K. Foley. 2004-2017 Geospatial Dataset of Wild and Prescribed Fire Activity Over the Conterminous United States. Data in Brief. Elsevier B.V., Amsterdam, NETHERLANDS, 56: 110856, (2024).
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TwitterFeature service generated by Hub for public Hub events. DO NOT DELETE THIS SERVICE. It stores the public Hub events for your organization.
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TwitterThis downloadable zip file also contains a map package of emergency management layers that Kittitas County uses during a forest fire event,
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TwitterLocations of Vision Zero community engagement events. This data includes date, location name, address, type, and description of the event.
Contact: Department of Environmental Services
Data Accessibility: Internal Use Only
Update Frequency: As Needed
Last Revision Date: 2/2/2024
Creation Date: 2/2/2024
Feature Dataset Name: DES_TEO
Layer Name: VisionZero_Community_Events
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TwitterAttribution 4.0 (CC BY 4.0)https://creativecommons.org/licenses/by/4.0/
License information was derived automatically
This document provides supporting information to assist in the use of the Australian Mafic-Ultramafic Magmatic Events GIS Dataset. The dataset is made publicly available as a GIS at nominal 1:5 000 …Show full descriptionThis document provides supporting information to assist in the use of the Australian Mafic-Ultramafic Magmatic Events GIS Dataset. The dataset is made publicly available as a GIS at nominal 1:5 000 000 scale, and shows the time-space-event distribution of mafic-ultramafic magmatism in Australia from the early Archean to the present day. Development of this GIS has been a multi-year project and earlier released extracts (in viewable pdf form with accompanying Geoscience Australia Records) included compilations for the Archean magmatic record, the Proterozoic magmatic record, and the Australian Large Igneous Provinces (LIPs). Publication of the GIS completes the series with addition of the Phanerozoic magmatic record, and formalisation of the complete record of Archean-Phanerozoic magmatic events as a single series. The chronology of Australian mafic-ultramafic magmatism resolves into 74 magmatic events within, predominately, resolvable bands of ±10 million years. Each event is identified by geological units grouped by similar age - this coeval magmatism may or may not be genetically related and may be in response to different geodynamic environments. These magmatic events range in age from the Eoarchean ~3730 Ma ME 1 - Manfred Event, confined within a small remnant domain within the Yilgarn Craton, to the widespread record of Cenozoic magmatism in eastern Australia (ME 72 to ME 74). The magmatic events range in magnitude from the giant volumes of magma in Large Igneous Provinces, to events whose only known occurrence is an isolated record of dated mafic igneous rock in a single drillhole. The GIS makes it possible to focus on the location of any one of these magmatic events, or groups of magmatic events that may be of interest, and overlay context from any other information that users may have available. The delineation of magmatic events for this study is based on several hundred published ages of mafic and ultramafic igneous rocks from different isotopic systems and minerals. In addition to their ages and extents, primary recorded aspects of each magmatic event include the presence or absence of ultramafic components. Further to this, the presence or correlation of known magmatic-related mineralisation is highlighted in Time-Space-Event Charts of Australia (Appendix D, figures D1 and D2). The basis for mapping has been regional solid geology, interpreted basement geology and surface geology base maps made available by the State and Northern Territory geological surveys, providing insight into the total areal extent of the magmatic systems under cover. Also available to complement the Event GIS are the domains and element boundaries from the Australian Crustal Elements map. These boundaries which are which are based on geophysical extrapolation of crustal elements under the cover of continental basins, provide a framework of the shallow crustal structure of the continent, and are used in this guide. The Crustal Elements digital dataset is available for download from the Geoscience Australia website. Insight into the geodynamic development of the continent is provided by the magmatic event structure through time. The compilation draws attention to concentrations of mafic-ultramafic magmatism in the Archean from ~2820-2665 Ma, in the Proterozoic from ~1870-1590 Ma, and in the late Neoproterozoic-Phanerozoic from ~530-225 Ma. These three time spans contain 39 of the 74 magmatic events, 53% of the entire mafic-ultramafic magmatic event record of the continent. The periods in between have mafic-ultramafic magmatic records that are more dispersed in time. Other features of interest include the shared geographic and crustal element locations of Large Igneous Provinces and numerous events with smaller magma volumes. Read the rest of the Executive Summary in the document.
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TwitterThe annual New Zealand Esri User Conference (NZEUC) is your opportunity to engage directly with key people from the geospatial industry whose decisions are critical when deploying the right solutions within their organisation.NZEUC (15-17 September, Te Pae Convention Centre, Christchurch) is the largest geospatial event of the calendar year, attended by senior GIS professionals and decision-makers across Government, Local Government, Conservation, Public Safety and Defense, Utilities, Infrastructure, Agri-Business, and more.At the NZEUC, Eagle Technology and Esri together deliver much anticipated technology updates and trends from Esri User Conference San Diego to the New Zealand and South Pacific audience.Organisations that are exhibiting at NZEUC 2025 can find important dates and other information such as pack in and pack out times detailed in this document.
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TwitterI'm Hannah, and I started my career in GIS from a B2B consulting side, and now as a customer in a global energy company. I love bringing together data and democratising location intelligence through cloud technology and collaboration. I've been fortunate to speak on this at a number of international industry conferences, and look forward to seeing where both GIS and myself can go in the future.
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Twitterhttps://pacific-data.sprep.org/resource/private-data-license-agreement-0https://pacific-data.sprep.org/resource/private-data-license-agreement-0
The report from the GIS conference that the SPREP GIS team participated in from 25 to 29 November