{"@context":"http://iiif.io/api/presentation/3/context.json","id":"https://makingscience.royalsociety.org/items/pt_40_7/paper-on-the-meteorology-of-the-lake-district-of-cumberland-and-westmoreland-westmorland-including-the-results-of-experiments-on-the-fall-of-rain-at-various-heights-up-to-3166-feet-above-the-sea-level-by-john-fletcher-miller/manifest.json","type":"Manifest","label":{"en":["Paper, 'On the meteorology of the Lake District of Cumberland and Westmoreland [Westmorland], including the results of experiments on the fall of rain at various heights, up to 3166 feet above the sea level' by John Fletcher Miller"]},"requiredStatement":{"label":{"en":["Attribution"]},"value":{"en":["The Royal Society"]}},"rights":"http://creativecommons.org/licenses/by/4.0/legalcode","provider":[{"id":"https://royalsociety.org/","type":"Agent","label":{"en":["The Royal Society"]},"homepage":[{"id":"https://makingscience.royalsociety.org","type":"Text","label":{"en":["The Royal Society - Science in the Making"]},"format":"text/html"}]}],"thumbnail":[{"id":"https://royalsociety-image-public.s3.eu-west-2.amazonaws.com/w400/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0001.jpeg","type":"Image","format":"image/jpeg"}],"metadata":[{"label":{"en":["Format"]},"value":{"en":["Manuscript"]}},{"label":{"en":["Reference Number"]},"value":{"en":["PT/40/7"]}},{"label":{"en":["Physical description"]},"value":{"en":["Ink on paper"]}},{"label":{"en":["Creator"]},"value":{"en":["John Fletcher Miller"]}}],"items":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0001.ptif/canvas","type":"Canvas","label":{"en":["Paper, 'On the meteorology of the Lake District of Cumberland and Westmoreland [Westmorland], including the results of experiments on the fall of rain at various heights, up to 3166 feet above the sea level' by John Fletcher Miller - 1"]},"height":4816,"width":7589,"thumbnail":[{"id":"https://royalsociety-image-public.s3.eu-west-2.amazonaws.com/w128/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0001.jpeg","type":"Image","format":"image/jpeg","width":128,"height":128}],"items":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0001.ptif/annotation_page","type":"AnnotationPage","items":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0001.ptif/annotation","type":"Annotation","motivation":"Painting","body":{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0001.ptif/info.json","type":"Image","service":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0001.ptif","type":"ImageService2","profile":"http://iiif.io/api/image/2/level2.json"}],"height":7589,"width":4816},"target":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0001.ptif/canvas"}]}]},{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0002.ptif/canvas","type":"Canvas","label":{"en":["Paper, 'On the meteorology of the Lake District of Cumberland and Westmoreland [Westmorland], including the results of experiments on the fall of rain at various heights, up to 3166 feet above the sea level' by John Fletcher Miller - 2"]},"height":4860,"width":7607,"thumbnail":[{"id":"https://royalsociety-image-public.s3.eu-west-2.amazonaws.com/w128/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0002.jpeg","type":"Image","format":"image/jpeg","width":128,"height":128}],"items":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0002.ptif/annotation_page","type":"AnnotationPage","items":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0002.ptif/annotation","type":"Annotation","motivation":"Painting","body":{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0002.ptif/info.json","type":"Image","service":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0002.ptif","type":"ImageService2","profile":"http://iiif.io/api/image/2/level2.json"}],"height":7607,"width":4860},"target":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0002.ptif/canvas"}]}]},{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0003.ptif/canvas","type":"Canvas","label":{"en":["Paper, 'On the meteorology of the Lake District of Cumberland and Westmoreland [Westmorland], including the results of experiments on the fall of rain at various heights, up to 3166 feet above the sea level' by John Fletcher Miller - 3"]},"height":4921,"width":7647,"thumbnail":[{"id":"https://royalsociety-image-public.s3.eu-west-2.amazonaws.com/w128/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0003.jpeg","type":"Image","format":"image/jpeg","width":128,"height":128}],"items":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0003.ptif/annotation_page","type":"AnnotationPage","items":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0003.ptif/annotation","type":"Annotation","motivation":"Painting","body":{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0003.ptif/info.json","type":"Image","service":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0003.ptif","type":"ImageService2","profile":"http://iiif.io/api/image/2/level2.json"}],"height":7647,"width":4921},"target":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0003.ptif/canvas"}]}]},{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0004.ptif/canvas","type":"Canvas","label":{"en":["Paper, 'On the meteorology of the Lake District of Cumberland and Westmoreland [Westmorland], including the results of experiments on the fall of rain at various heights, up to 3166 feet above the sea level' by John Fletcher Miller - 4"]},"height":4885,"width":7647,"thumbnail":[{"id":"https://royalsociety-image-public.s3.eu-west-2.amazonaws.com/w128/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0004.jpeg","type":"Image","format":"image/jpeg","width":128,"height":128}],"items":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0004.ptif/annotation_page","type":"AnnotationPage","items":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0004.ptif/annotation","type":"Annotation","motivation":"Painting","body":{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0004.ptif/info.json","type":"Image","service":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0004.ptif","type":"ImageService2","profile":"http://iiif.io/api/image/2/level2.json"}],"height":7647,"width":4885},"target":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0004.ptif/canvas"}]}]},{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0005.ptif/canvas","type":"Canvas","label":{"en":["Paper, 'On the meteorology of the Lake District of Cumberland and Westmoreland [Westmorland], including the results of experiments on the fall of rain at various heights, up to 3166 feet above the sea level' by John Fletcher Miller - 5"]},"height":2382,"width":3613,"thumbnail":[{"id":"https://royalsociety-image-public.s3.eu-west-2.amazonaws.com/w128/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0005.jpeg","type":"Image","format":"image/jpeg","width":128,"height":128}],"items":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0005.ptif/annotation_page","type":"AnnotationPage","items":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0005.ptif/annotation","type":"Annotation","motivation":"Painting","body":{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0005.ptif/info.json","type":"Image","service":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0005.ptif","type":"ImageService2","profile":"http://iiif.io/api/image/2/level2.json"}],"height":3613,"width":2382},"target":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0005.ptif/canvas"}]}]},{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0006.ptif/canvas","type":"Canvas","label":{"en":["Paper, 'On the meteorology of the Lake District of Cumberland and Westmoreland [Westmorland], including the results of experiments on the fall of rain at various heights, up to 3166 feet above the sea level' by John Fletcher Miller - 6"]},"height":4862,"width":7438,"thumbnail":[{"id":"https://royalsociety-image-public.s3.eu-west-2.amazonaws.com/w128/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0006.jpeg","type":"Image","format":"image/jpeg","width":128,"height":128}],"items":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0006.ptif/annotation_page","type":"AnnotationPage","items":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0006.ptif/annotation","type":"Annotation","motivation":"Painting","body":{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0006.ptif/info.json","type":"Image","service":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0006.ptif","type":"ImageService2","profile":"http://iiif.io/api/image/2/level2.json"}],"height":7438,"width":4862},"target":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0006.ptif/canvas"}]}]},{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0007.ptif/canvas","type":"Canvas","label":{"en":["Paper, 'On the meteorology of the Lake District of Cumberland and Westmoreland [Westmorland], including the results of experiments on the fall of rain at various heights, up to 3166 feet above the sea level' by John Fletcher Miller - 7"]},"height":4743,"width":7478,"thumbnail":[{"id":"https://royalsociety-image-public.s3.eu-west-2.amazonaws.com/w128/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0007.jpeg","type":"Image","format":"image/jpeg","width":128,"height":128}],"items":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0007.ptif/annotation_page","type":"AnnotationPage","items":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0007.ptif/annotation","type":"Annotation","motivation":"Painting","body":{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0007.ptif/info.json","type":"Image","service":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0007.ptif","type":"ImageService2","profile":"http://iiif.io/api/image/2/level2.json"}],"height":7478,"width":4743},"target":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0007.ptif/canvas"}]}]},{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0008.ptif/canvas","type":"Canvas","label":{"en":["Paper, 'On the meteorology of the Lake District of Cumberland and Westmoreland [Westmorland], including the results of experiments on the fall of rain at various heights, up to 3166 feet above the sea level' by John Fletcher Miller - 8"]},"height":4807,"width":7435,"thumbnail":[{"id":"https://royalsociety-image-public.s3.eu-west-2.amazonaws.com/w128/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0008.jpeg","type":"Image","format":"image/jpeg","width":128,"height":128}],"items":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0008.ptif/annotation_page","type":"AnnotationPage","items":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0008.ptif/annotation","type":"Annotation","motivation":"Painting","body":{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0008.ptif/info.json","type":"Image","service":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0008.ptif","type":"ImageService2","profile":"http://iiif.io/api/image/2/level2.json"}],"height":7435,"width":4807},"target":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0008.ptif/canvas"}]}]},{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0009.ptif/canvas","type":"Canvas","label":{"en":["Paper, 'On the meteorology of the Lake District of Cumberland and Westmoreland [Westmorland], including the results of experiments on the fall of rain at various heights, up to 3166 feet above the sea level' by John Fletcher Miller - 9"]},"height":4756,"width":7475,"thumbnail":[{"id":"https://royalsociety-image-public.s3.eu-west-2.amazonaws.com/w128/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0009.jpeg","type":"Image","format":"image/jpeg","width":128,"height":128}],"items":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0009.ptif/annotation_page","type":"AnnotationPage","items":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0009.ptif/annotation","type":"Annotation","motivation":"Painting","body":{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0009.ptif/info.json","type":"Image","service":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0009.ptif","type":"ImageService2","profile":"http://iiif.io/api/image/2/level2.json"}],"height":7475,"width":4756},"target":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0009.ptif/canvas"}]}]},{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0010.ptif/canvas","type":"Canvas","label":{"en":["Paper, 'On the meteorology of the Lake District of Cumberland and Westmoreland [Westmorland], including the results of experiments on the fall of rain at various heights, up to 3166 feet above the sea level' by John Fletcher Miller - 10"]},"height":4821,"width":7470,"thumbnail":[{"id":"https://royalsociety-image-public.s3.eu-west-2.amazonaws.com/w128/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0010.jpeg","type":"Image","format":"image/jpeg","width":128,"height":128}],"items":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0010.ptif/annotation_page","type":"AnnotationPage","items":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0010.ptif/annotation","type":"Annotation","motivation":"Painting","body":{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0010.ptif/info.json","type":"Image","service":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0010.ptif","type":"ImageService2","profile":"http://iiif.io/api/image/2/level2.json"}],"height":7470,"width":4821},"target":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0010.ptif/canvas"}]}]},{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0011.ptif/canvas","type":"Canvas","label":{"en":["Paper, 'On the meteorology of the Lake District of Cumberland and Westmoreland [Westmorland], including the results of experiments on the fall of rain at various heights, up to 3166 feet above the sea level' by John Fletcher Miller - 11"]},"height":4807,"width":7466,"thumbnail":[{"id":"https://royalsociety-image-public.s3.eu-west-2.amazonaws.com/w128/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0011.jpeg","type":"Image","format":"image/jpeg","width":128,"height":128}],"items":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0011.ptif/annotation_page","type":"AnnotationPage","items":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0011.ptif/annotation","type":"Annotation","motivation":"Painting","body":{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0011.ptif/info.json","type":"Image","service":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0011.ptif","type":"ImageService2","profile":"http://iiif.io/api/image/2/level2.json"}],"height":7466,"width":4807},"target":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0011.ptif/canvas"}]}]},{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0012.ptif/canvas","type":"Canvas","label":{"en":["Paper, 'On the meteorology of the Lake District of Cumberland and Westmoreland [Westmorland], including the results of experiments on the fall of rain at various heights, up to 3166 feet above the sea level' by John Fletcher Miller - 12"]},"height":4882,"width":7466,"thumbnail":[{"id":"https://royalsociety-image-public.s3.eu-west-2.amazonaws.com/w128/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0012.jpeg","type":"Image","format":"image/jpeg","width":128,"height":128}],"items":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0012.ptif/annotation_page","type":"AnnotationPage","items":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0012.ptif/annotation","type":"Annotation","motivation":"Painting","body":{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0012.ptif/info.json","type":"Image","service":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0012.ptif","type":"ImageService2","profile":"http://iiif.io/api/image/2/level2.json"}],"height":7466,"width":4882},"target":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0012.ptif/canvas"}]}]},{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0013.ptif/canvas","type":"Canvas","label":{"en":["Paper, 'On the meteorology of the Lake District of Cumberland and Westmoreland [Westmorland], including the results of experiments on the fall of rain at various heights, up to 3166 feet above the sea level' by John Fletcher Miller - 13"]},"height":4764,"width":7487,"thumbnail":[{"id":"https://royalsociety-image-public.s3.eu-west-2.amazonaws.com/w128/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0013.jpeg","type":"Image","format":"image/jpeg","width":128,"height":128}],"items":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0013.ptif/annotation_page","type":"AnnotationPage","items":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0013.ptif/annotation","type":"Annotation","motivation":"Painting","body":{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0013.ptif/info.json","type":"Image","service":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0013.ptif","type":"ImageService2","profile":"http://iiif.io/api/image/2/level2.json"}],"height":7487,"width":4764},"target":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0013.ptif/canvas"}]}]},{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0014.ptif/canvas","type":"Canvas","label":{"en":["Paper, 'On the meteorology of the Lake District of Cumberland and Westmoreland [Westmorland], including the results of experiments on the fall of rain at various heights, up to 3166 feet above the sea level' by John Fletcher Miller - 14"]},"height":4835,"width":7389,"thumbnail":[{"id":"https://royalsociety-image-public.s3.eu-west-2.amazonaws.com/w128/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0014.jpeg","type":"Image","format":"image/jpeg","width":128,"height":128}],"items":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0014.ptif/annotation_page","type":"AnnotationPage","items":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0014.ptif/annotation","type":"Annotation","motivation":"Painting","body":{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0014.ptif/info.json","type":"Image","service":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0014.ptif","type":"ImageService2","profile":"http://iiif.io/api/image/2/level2.json"}],"height":7389,"width":4835},"target":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0014.ptif/canvas"}]}]},{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0015.ptif/canvas","type":"Canvas","label":{"en":["Paper, 'On the meteorology of the Lake District of Cumberland and Westmoreland [Westmorland], including the results of experiments on the fall of rain at various heights, up to 3166 feet above the sea level' by John Fletcher Miller - 15"]},"height":4763,"width":7428,"thumbnail":[{"id":"https://royalsociety-image-public.s3.eu-west-2.amazonaws.com/w128/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0015.jpeg","type":"Image","format":"image/jpeg","width":128,"height":128}],"items":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0015.ptif/annotation_page","type":"AnnotationPage","items":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0015.ptif/annotation","type":"Annotation","motivation":"Painting","body":{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0015.ptif/info.json","type":"Image","service":[{"id":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0015.ptif","type":"ImageService2","profile":"http://iiif.io/api/image/2/level2.json"}],"height":7428,"width":4763},"target":"https://rs-images.cogapp.cloud/iiif/3/PT%2FPT_40%2FPT_40_7%2Ftif%2FPT_40_7_0015.ptif/canvas"}]}]}]}