{"@context":"http://iiif.io/api/presentation/3/context.json","id":"https://makingscience.royalsociety.org/items/rr_16_299/referees-report-by-charles-chree-on-a-paper-the-vertical-temperature-gradient-on-the-west-coast-of-scotland-and-at-oxshott-surrey-by-william-henry-dines/manifest.json","type":"Manifest","label":{"en":["Referee's report by Charles Chree, on a paper 'The vertical temperature gradient on the west coast of Scotland and at Oxshott, Surrey' by William Henry Dines"]},"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/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_001.jpeg","type":"Image","format":"image/jpeg"}],"metadata":[{"label":{"en":["Format"]},"value":{"en":["Manuscript"]}},{"label":{"en":["Reference Number"]},"value":{"en":["RR/16/299"]}},{"label":{"en":["Physical description"]},"value":{"en":["Standardised form (type A) and notes on paper"]}},{"label":{"en":["Creator"]},"value":{"en":["Charles Chree"]}}],"items":[{"id":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_001.ptif/canvas","type":"Canvas","label":{"en":["Referee's report by Charles Chree, on a paper 'The vertical temperature gradient on the west coast of Scotland and at Oxshott, Surrey' by William Henry Dines - 1"]},"height":5299,"width":8225,"thumbnail":[{"id":"https://royalsociety-image-public.s3.eu-west-2.amazonaws.com/w128/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_001.jpeg","type":"Image","format":"image/jpeg","width":128,"height":128}],"items":[{"id":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_001.ptif/annotation_page","type":"AnnotationPage","items":[{"id":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_001.ptif/annotation","type":"Annotation","motivation":"Painting","body":{"id":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_001.ptif/info.json","type":"Image","service":[{"id":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_001.ptif","type":"ImageService2","profile":"http://iiif.io/api/image/2/level2.json"}],"height":8225,"width":5299},"target":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_001.ptif/canvas"}]}]},{"id":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_002.ptif/canvas","type":"Canvas","label":{"en":["Referee's report by Charles Chree, on a paper 'The vertical temperature gradient on the west coast of Scotland and at Oxshott, Surrey' by William Henry Dines - 2"]},"height":8178,"width":5296,"thumbnail":[{"id":"https://royalsociety-image-public.s3.eu-west-2.amazonaws.com/w128/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_002.jpeg","type":"Image","format":"image/jpeg","width":128,"height":128}],"items":[{"id":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_002.ptif/annotation_page","type":"AnnotationPage","items":[{"id":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_002.ptif/annotation","type":"Annotation","motivation":"Painting","body":{"id":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_002.ptif/info.json","type":"Image","service":[{"id":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_002.ptif","type":"ImageService2","profile":"http://iiif.io/api/image/2/level2.json"}],"height":5296,"width":8178},"target":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_002.ptif/canvas"}]}]},{"id":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_003.ptif/canvas","type":"Canvas","label":{"en":["Referee's report by Charles Chree, on a paper 'The vertical temperature gradient on the west coast of Scotland and at Oxshott, Surrey' by William Henry Dines - 3"]},"height":5148,"width":8088,"thumbnail":[{"id":"https://royalsociety-image-public.s3.eu-west-2.amazonaws.com/w128/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_003.jpeg","type":"Image","format":"image/jpeg","width":128,"height":128}],"items":[{"id":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_003.ptif/annotation_page","type":"AnnotationPage","items":[{"id":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_003.ptif/annotation","type":"Annotation","motivation":"Painting","body":{"id":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_003.ptif/info.json","type":"Image","service":[{"id":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_003.ptif","type":"ImageService2","profile":"http://iiif.io/api/image/2/level2.json"}],"height":8088,"width":5148},"target":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_003.ptif/canvas"}]}]},{"id":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_004.ptif/canvas","type":"Canvas","label":{"en":["Referee's report by Charles Chree, on a paper 'The vertical temperature gradient on the west coast of Scotland and at Oxshott, Surrey' by William Henry Dines - 4"]},"height":5135,"width":8104,"thumbnail":[{"id":"https://royalsociety-image-public.s3.eu-west-2.amazonaws.com/w128/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_004.jpeg","type":"Image","format":"image/jpeg","width":128,"height":128}],"items":[{"id":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_004.ptif/annotation_page","type":"AnnotationPage","items":[{"id":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_004.ptif/annotation","type":"Annotation","motivation":"Painting","body":{"id":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_004.ptif/info.json","type":"Image","service":[{"id":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_004.ptif","type":"ImageService2","profile":"http://iiif.io/api/image/2/level2.json"}],"height":8104,"width":5135},"target":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_004.ptif/canvas"}]}]},{"id":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_005.ptif/canvas","type":"Canvas","label":{"en":["Referee's report by Charles Chree, on a paper 'The vertical temperature gradient on the west coast of Scotland and at Oxshott, Surrey' by William Henry Dines - 5"]},"height":5117,"width":6105,"thumbnail":[{"id":"https://royalsociety-image-public.s3.eu-west-2.amazonaws.com/w128/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_005.jpeg","type":"Image","format":"image/jpeg","width":128,"height":128}],"items":[{"id":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_005.ptif/annotation_page","type":"AnnotationPage","items":[{"id":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_005.ptif/annotation","type":"Annotation","motivation":"Painting","body":{"id":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_005.ptif/info.json","type":"Image","service":[{"id":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_005.ptif","type":"ImageService2","profile":"http://iiif.io/api/image/2/level2.json"}],"height":6105,"width":5117},"target":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_005.ptif/canvas"}]}]},{"id":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_006.ptif/canvas","type":"Canvas","label":{"en":["Referee's report by Charles Chree, on a paper 'The vertical temperature gradient on the west coast of Scotland and at Oxshott, Surrey' by William Henry Dines - 6"]},"height":5116,"width":6076,"thumbnail":[{"id":"https://royalsociety-image-public.s3.eu-west-2.amazonaws.com/w128/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_006.jpeg","type":"Image","format":"image/jpeg","width":128,"height":128}],"items":[{"id":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_006.ptif/annotation_page","type":"AnnotationPage","items":[{"id":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_006.ptif/annotation","type":"Annotation","motivation":"Painting","body":{"id":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_006.ptif/info.json","type":"Image","service":[{"id":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_006.ptif","type":"ImageService2","profile":"http://iiif.io/api/image/2/level2.json"}],"height":6076,"width":5116},"target":"https://images-rs-sitm.fly.dev/iiif/3/RR%2FRR_16_211-418%2FTIF%2FRR_16_299%2FRR_16_299_006.ptif/canvas"}]}]}]}