| snippet:
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Epithermal gold-silver deposits in Northland and the Hauraki Goldfield (Great Barrier Island and Coromandel Peninsula) were formed in ancient geothermal systems associated with volcanism that was active during the Miocene-Pliocene. Gold is being deposited in modern epithermal deposits today in active geothermal systems of the Rotorua-Taupō area, associated with Quaternary volcanism. |
| summary:
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Epithermal gold-silver deposits in Northland and the Hauraki Goldfield (Great Barrier Island and Coromandel Peninsula) were formed in ancient geothermal systems associated with volcanism that was active during the Miocene-Pliocene. Gold is being deposited in modern epithermal deposits today in active geothermal systems of the Rotorua-Taupō area, associated with Quaternary volcanism. |
| extent:
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[[166.158931564922,-48.2329843974233],[179.436023526899,-34.0078155417841]] |
| accessInformation:
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| thumbnail:
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thumbnail/thumbnail.png |
| maxScale:
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1.7976931348623157E308 |
| typeKeywords:
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["ArcGIS","ArcGIS Server","Data","Map Service","Service"] |
| description:
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| licenseInfo:
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| catalogPath:
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| title:
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Epithermal Gold |
| type:
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Map Service |
| url:
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| tags:
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["Geology","New Zealand","Gold","Epithermal","Minerals","Critical Minerals"] |
| culture:
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en-NZ |
| portalUrl:
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| name:
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Critical_Minerals_Epithermal_Gold |
| guid:
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3FB3E8F4-DA04-4863-870E-DB9A029F0214 |
| minScale:
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0 |
| spatialReference:
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NZGD_2000_New_Zealand_Transverse_Mercator |