{ "opencollection": "1.0.0", "info": { "name": "USGS Water Data OGC APIs agency-codes aquifer-types API", "version": "0.56.0" }, "items": [ { "info": { "name": "aquifer-types", "type": "folder" }, "items": [ { "info": { "name": "Get Aquifer types metadata", "type": "http" }, "http": { "method": "GET", "url": "https://api.waterdata.usgs.gov/ogcapi/v0/collections/aquifer-types", "params": [ { "name": "f", "value": "", "type": "query", "description": "The optional f parameter indicates the output format which the server shall provide as part of the response document. The default format is GeoJSON. CSV is also available." }, { "name": "lang", "value": "", "type": "query", "description": "The optional lang parameter instructs the server return a response in a certain language, if supported. If the language is not among the available values, the Accept-Language header language will be used if it is supported. If the header is missing, the default server language is used. Note that providers may only support a single language (or often no language at all), that can be different from the server language. Language strings can be written in a complex (e.g. \"fr-CA,fr;q=0.9,en-US;q=0.8,en;q=0.7\"), simple (e.g. \"de\") or locale-like (e.g. \"de-CH\" or \"fr_BE\") fashion." } ] }, "docs": "Groundwater occurs in aquifers under two different conditions. Where water only partly fills an aquifer, the upper surface is free to rise and decline. These aquifers are referred to as unconfined (or water-table) aquifers. Where water completely fills an aquifer that is overlain by a confining bed, the aquifer is referred to as a confined (or artesian) aquifer. When a confined aquifer is penetrated by a well, the water level in the well will rise above the top of the aquifer (but not necessaril" }, { "info": { "name": "Get Aquifer types items", "type": "http" }, "http": { "method": "GET", "url": "https://api.waterdata.usgs.gov/ogcapi/v0/collections/aquifer-types/items", "params": [ { "name": "f", "value": "", "type": "query", "description": "The optional f parameter indicates the output format which the server shall provide as part of the response document. The default format is GeoJSON." }, { "name": "lang", "value": "", "type": "query", "description": "The optional lang parameter instructs the server return a response in a certain language, if supported. If the language is not among the available values, the Accept-Language header language will be used if it is supported. If the header is missing, the default server language is used. Note that providers may only support a single language (or often no language at all), that can be different from the server language. Language strings can be written in a complex (e.g. \"fr-CA,fr;q=0.9,en-US;q=0.8,en;q=0.7\"), simple (e.g. \"de\") or locale-like (e.g. \"de-CH\" or \"fr_BE\") fashion." }, { "name": "bbox", "value": "", "type": "query", "description": "Only features that have a geometry that intersects the bounding box are selected.The bounding box is provided as four or six numbers, depending on whether the coordinate reference system includes a vertical axis (height or depth)." }, { "name": "limit", "value": "", "type": "query", "description": "The optional limit parameter limits the number of items that are presented in the response document (maximum=50000, default=10000)." }, { "name": "crs", "value": "", "type": "query", "description": "Indicates the coordinate reference system for the results." }, { "name": "bbox-crs", "value": "", "type": "query", "description": "Indicates the coordinate reference system for the given bbox coordinates." }, { "name": "properties", "value": "", "type": "query", "description": "The properties that should be included. The parameter value is a comma-separated list of property names." }, { "name": "skipGeometry", "value": "", "type": "query", "description": "This option can be used to skip response geometries for each feature." }, { "name": "offset", "value": "", "type": "query", "description": "The optional offset parameter indicates the index within the result set from which the server shall begin presenting results in the response document. The first element has an index of 0 (default)." }, { "name": "id", "value": "", "type": "query", "description": "The single-character code identifying the type of aquifer" }, { "name": "aquifer_type_description", "value": "", "type": "query", "description": "Longer description of the aquifer type." }, { "name": "filter", "value": "", "type": "query", "description": "CQL Text filter expression. CQL JSON cannot be used here, only in the body. \nSee also: https://docs.pygeoapi.io/en/latest/cql.html \n\nExample: time_series_id IN ('64ee32f5350a4ec4967435dcd2e364ea', '3e55d9c2d8a54bec9ca5e292b07d5a96')" } ], "auth": { "type": "apikey", "key": "api_key", "value": "{{api_key}}", "placement": "query" } }, "docs": "Groundwater occurs in aquifers under two different conditions. Where water only partly fills an aquifer, the upper surface is free to rise and decline. These aquifers are referred to as unconfined (or water-table) aquifers. Where water completely fills an aquifer that is overlain by a confining bed, the aquifer is referred to as a confined (or artesian) aquifer. When a confined aquifer is penetrated by a well, the water level in the well will rise above the top of the aquifer (but not necessaril" }, { "info": { "name": "Get Aquifer types items with CQL2", "type": "http" }, "http": { "method": "POST", "url": "https://api.waterdata.usgs.gov/ogcapi/v0/collections/aquifer-types/items", "body": { "type": "json", "data": "{}" }, "auth": { "type": "apikey", "key": "api_key", "value": "{{api_key}}", "placement": "query" } }, "docs": "Groundwater occurs in aquifers under two different conditions. Where water only partly fills an aquifer, the upper surface is free to rise and decline. These aquifers are referred to as unconfined (or water-table) aquifers. Where water completely fills an aquifer that is overlain by a confining bed, the aquifer is referred to as a confined (or artesian) aquifer. When a confined aquifer is penetrated by a well, the water level in the well will rise above the top of the aquifer (but not necessaril" }, { "info": { "name": "Options for Aquifer types items", "type": "http" }, "http": { "method": "OPTIONS", "url": "https://api.waterdata.usgs.gov/ogcapi/v0/collections/aquifer-types/items", "auth": { "type": "apikey", "key": "api_key", "value": "{{api_key}}", "placement": "query" } }, "docs": "Groundwater occurs in aquifers under two different conditions. Where water only partly fills an aquifer, the upper surface is free to rise and decline. These aquifers are referred to as unconfined (or water-table) aquifers. Where water completely fills an aquifer that is overlain by a confining bed, the aquifer is referred to as a confined (or artesian) aquifer. When a confined aquifer is penetrated by a well, the water level in the well will rise above the top of the aquifer (but not necessaril" }, { "info": { "name": "Get Aquifer types item by id", "type": "http" }, "http": { "method": "GET", "url": "https://api.waterdata.usgs.gov/ogcapi/v0/collections/aquifer-types/items/:featureId", "params": [ { "name": "crs", "value": "", "type": "query", "description": "Indicates the coordinate reference system for the results." }, { "name": "f", "value": "", "type": "query", "description": "The optional f parameter indicates the output format which the server shall provide as part of the response document. The default format is GeoJSON. CSV is also available." }, { "name": "lang", "value": "", "type": "query", "description": "The optional lang parameter instructs the server return a response in a certain language, if supported. If the language is not among the available values, the Accept-Language header language will be used if it is supported. If the header is missing, the default server language is used. Note that providers may only support a single language (or often no language at all), that can be different from the server language. Language strings can be written in a complex (e.g. \"fr-CA,fr;q=0.9,en-US;q=0.8,en;q=0.7\"), simple (e.g. \"de\") or locale-like (e.g. \"de-CH\" or \"fr_BE\") fashion." } ], "auth": { "type": "apikey", "key": "api_key", "value": "{{api_key}}", "placement": "query" } }, "docs": "Groundwater occurs in aquifers under two different conditions. Where water only partly fills an aquifer, the upper surface is free to rise and decline. These aquifers are referred to as unconfined (or water-table) aquifers. Where water completely fills an aquifer that is overlain by a confining bed, the aquifer is referred to as a confined (or artesian) aquifer. When a confined aquifer is penetrated by a well, the water level in the well will rise above the top of the aquifer (but not necessaril" }, { "info": { "name": "Options for Aquifer types item by id", "type": "http" }, "http": { "method": "OPTIONS", "url": "https://api.waterdata.usgs.gov/ogcapi/v0/collections/aquifer-types/items/:featureId", "auth": { "type": "apikey", "key": "api_key", "value": "{{api_key}}", "placement": "query" } }, "docs": "Groundwater occurs in aquifers under two different conditions. Where water only partly fills an aquifer, the upper surface is free to rise and decline. These aquifers are referred to as unconfined (or water-table) aquifers. Where water completely fills an aquifer that is overlain by a confining bed, the aquifer is referred to as a confined (or artesian) aquifer. When a confined aquifer is penetrated by a well, the water level in the well will rise above the top of the aquifer (but not necessaril" }, { "info": { "name": "Get Aquifer types queryables", "type": "http" }, "http": { "method": "GET", "url": "https://api.waterdata.usgs.gov/ogcapi/v0/collections/aquifer-types/queryables", "params": [ { "name": "properties", "value": "", "type": "query", "description": "The properties that should be included. The parameter value is a comma-separated list of property names." }, { "name": "f", "value": "", "type": "query", "description": "The optional f parameter indicates the output format which the server shall provide as part of the response document. The default format is GeoJSON. CSV is also available." }, { "name": "profile", "value": "", "type": "query", "description": "The profile to be applied to a given request" }, { "name": "lang", "value": "", "type": "query", "description": "The optional lang parameter instructs the server return a response in a certain language, if supported. If the language is not among the available values, the Accept-Language header language will be used if it is supported. If the header is missing, the default server language is used. Note that providers may only support a single language (or often no language at all), that can be different from the server language. Language strings can be written in a complex (e.g. \"fr-CA,fr;q=0.9,en-US;q=0.8,en;q=0.7\"), simple (e.g. \"de\") or locale-like (e.g. \"de-CH\" or \"fr_BE\") fashion." } ], "auth": { "type": "apikey", "key": "api_key", "value": "{{api_key}}", "placement": "query" } }, "docs": "Groundwater occurs in aquifers under two different conditions. Where water only partly fills an aquifer, the upper surface is free to rise and decline. These aquifers are referred to as unconfined (or water-table) aquifers. Where water completely fills an aquifer that is overlain by a confining bed, the aquifer is referred to as a confined (or artesian) aquifer. When a confined aquifer is penetrated by a well, the water level in the well will rise above the top of the aquifer (but not necessaril" }, { "info": { "name": "Get Aquifer types schema", "type": "http" }, "http": { "method": "GET", "url": "https://api.waterdata.usgs.gov/ogcapi/v0/collections/aquifer-types/schema", "params": [ { "name": "f", "value": "", "type": "query", "description": "The optional f parameter indicates the output format which the server shall provide as part of the response document. The default format is GeoJSON. CSV is also available." }, { "name": "lang", "value": "", "type": "query", "description": "The optional lang parameter instructs the server return a response in a certain language, if supported. If the language is not among the available values, the Accept-Language header language will be used if it is supported. If the header is missing, the default server language is used. Note that providers may only support a single language (or often no language at all), that can be different from the server language. Language strings can be written in a complex (e.g. \"fr-CA,fr;q=0.9,en-US;q=0.8,en;q=0.7\"), simple (e.g. \"de\") or locale-like (e.g. \"de-CH\" or \"fr_BE\") fashion." } ], "auth": { "type": "apikey", "key": "api_key", "value": "{{api_key}}", "placement": "query" } }, "docs": "Groundwater occurs in aquifers under two different conditions. Where water only partly fills an aquifer, the upper surface is free to rise and decline. These aquifers are referred to as unconfined (or water-table) aquifers. Where water completely fills an aquifer that is overlain by a confining bed, the aquifer is referred to as a confined (or artesian) aquifer. When a confined aquifer is penetrated by a well, the water level in the well will rise above the top of the aquifer (but not necessaril" } ] } ], "bundled": true }