Commands
10
Queries
17.56 ms
Query time
0
Failed Queries
| # | Time | Connection | Command |
|---|---|---|---|
| 1 | 0.69 ms | cache | CONNECT redis.internal 6379 5 <null> 5 5 |
| 2 | 0.40 ms | cache | SELECT 0 |
| 3 | 0.30 ms | cache | MGET wJo3GJ9dRH:data > anonymous-media > id=6644,locale=en,domain=www |
| 4 | 0.68 ms | cache | INFO Memory |
| 5 | 0.03 ms | cache | MULTI 2 |
| 6 | 0.12 ms | cache | SETEX wJo3GJ9dRH:data > anonymous-media > id=6644,locale=en,domain=www 2678399 ���A _ Oa:2:{i:0;s:13:"cache-service";i:1;s:36:"cache-service-data > anonymous-media";}a:15:{s:2:"id";i:889;s:5:"title";s:30:"Interactive Earth: Geodynamics";s:4:"slug";s:29:"interactive-earth-geodynamics";s:9:"mediaType";s:10:"simulation";s:14:"thumbnailSizes";a:3:{s:9:"node_pack";s:157:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/889-6545f4656ece5688743390.webp";s:10:"suggestion";s:158:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/889-6545f4656ece5688743390.webp";s:5:"title";s:153:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/889-6545f4656ece5688743390.webp";}s:19:"thumbnailBackground";s:7:"#004387";s:11:"publishedAt";O:17:"DateTimeImmutable":3:{s:4:"date";s:26:"2017-04-11 00:00:00.000000";s:13:"timezone_type";i:3;s:8:"timezone";s:3:"UTC";}s:8:"isExpert";b:0;s:5:"goals";s:225:"<ul> <li>To develop a model to describe the theory of plate tectonics and the flow of energy that drives this process.</li> <li>To describe how earthquakes, volcanism, oceanic ridges and mountains are related.</li> </ul>";s:5:"width";i:550;s:6:"height";i:440;s:11:"description";s:434:"<p>What did Earth look like 200 million years ago? Are Volcanoes and Earthquakes Related?<br /> This simulation let you and your students explore plate tectonics, volcanoes, earthquakes, faults. The distribution of earthquakes and volcanoes provides information on the dynamic structure of the Earth.</p> <p>This simulation is part of the <a href="/en/search?q=interactive+earth" target="_blank">Interactive Earth project</a>.</p>";s:11:"suggestions";a:6:{i:0;a:9:{s:2:"id";i:976;s:5:"title";s:9:"Watershed";s:4:"slug";s:9:"watershed";s:9:"mediaType";s:10:"simulation";s:14:"thumbnailSizes";a:3:{s:9:"node_pack";s:157:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/976-6545f492985be646618409.webp";s:10:"suggestion";s:158:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/976-6545f492985be646618409.webp";s:5:"title";s:153:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/976-6545f492985be646618409.webp";}s:19:"thumbnailBackground";s:7:"#ec008d";s:11:"publishedAt";O:17:"DateTimeImmutable":3:{s:4:"date";s:26:"2023-03-20 00:00:00.000000";s:13:"timezone_type";i:3;s:8:"timezone";s:3:"UTC";}s:8:"isExpert";b:0;s:5:"goals";s:249:"<ul> <li>To define what a watershed and a water divide line are.</li> <li>To explain the time lag between precipitation, flooding, and recession.</li> <li>To explain how land-use planning can limit or exacerbate the risk of floods.</li> </ul>";}i:1;a:9:{s:2:"id";i:946;s:5:"title";s:11:"Ozone layer";s:4:"slug";s:11:"ozone-layer";s:9:"mediaType";s:10:"simulation";s:14:"thumbnailSizes";a:3:{s:9:"node_pack";s:157:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/946-6545f485966fa165967576.webp";s:10:"suggestion";s:158:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/946-6545f485966fa165967576.webp";s:5:"title";s:153:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/946-6545f485966fa165967576.webp";}s:19:"thumbnailBackground";s:7:"#ec008d";s:11:"publishedAt";O:17:"DateTimeImmutable":3:{s:4:"date";s:26:"2020-03-09 00:00:00.000000";s:13:"timezone_type";i:3;s:8:"timezone";s:3:"UTC";}s:8:"isExpert";b:0;s:5:"goals";s:240:"<ul> <li>To illustrate the ozone production / destruction cycle that operates in the stratosphere.</li> <li>To observe why the CFC molecules disrupt the ozone-oxygen cycle and explain the "hole in the ozone layer".</li> </ul>";}i:2;a:9:{s:2:"id";i:303;s:5:"title";s:17:"Continental drift";s:4:"slug";s:17:"continental-drift";s:9:"mediaType";s:10:"simulation";s:14:"thumbnailSizes";a:3:{s:9:"node_pack";s:157:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/303-6545f3126eee5679417238.webp";s:10:"suggestion";s:158:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/303-6545f3126eee5679417238.webp";s:5:"title";s:153:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/303-6545f3126eee5679417238.webp";}s:19:"thumbnailBackground";s:7:"#00b7ad";s:11:"publishedAt";O:17:"DateTimeImmutable":3:{s:4:"date";s:26:"2015-05-11 00:00:00.000000";s:13:"timezone_type";i:3;s:8:"timezone";s:3:"UTC";}s:8:"isExpert";b:0;s:5:"goals";s:307:"<ul> <li>To illustrate the arrangement and movements of the lithospheric plates on the Geological Time Scale.</li> <li>To study of the evolution of lithospheric plates’ positions, from Pangea to the present, as well as an extrapolation of their positions in the distant future (30 MY).</li> </ul>";}i:3;a:9:{s:2:"id";i:57;s:5:"title";s:25:"Erosion and deforestation";s:4:"slug";s:25:"erosion-and-deforestation";s:9:"mediaType";s:10:"simulation";s:14:"thumbnailSizes";a:3:{s:9:"node_pack";s:156:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/57-6545f3b6c6ce2672721279.webp";s:10:"suggestion";s:157:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/57-6545f3b6c6ce2672721279.webp";s:5:"title";s:152:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/57-6545f3b6c6ce2672721279.webp";}s:19:"thumbnailBackground";s:7:"#f6951d";s:11:"publishedAt";O:17:"DateTimeImmutable":3:{s:4:"date";s:26:"2015-05-11 00:00:00.000000";s:13:"timezone_type";i:3;s:8:"timezone";s:3:"UTC";}s:8:"isExpert";b:0;s:5:"goals";s:214:"<ul> <li>To illustrate the link between deforestation and the erosion of soils.</li> <li>To understand the impact of deforestation on the environment (ecosystem, climate, landslides…..)</li> </ul>";}i:4;a:9:{s:2:"id";i:947;s:5:"title";s:18:"Rhizobial symbiont";s:4:"slug";s:18:"rhizobial-symbiont";s:9:"mediaType";s:10:"simulation";s:14:"thumbnailSizes";a:3:{s:9:"node_pack";s:157:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/947-6545f4860cfeb756362832.webp";s:10:"suggestion";s:158:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/947-6545f4860cfeb756362832.webp";s:5:"title";s:153:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/947-6545f4860cfeb756362832.webp";}s:19:"thumbnailBackground";s:7:"#462f92";s:11:"publishedAt";O:17:"DateTimeImmutable":3:{s:4:"date";s:26:"2020-03-19 00:00:00.000000";s:13:"timezone_type";i:3;s:8:"timezone";s:3:"UTC";}s:8:"isExpert";b:1;s:5:"goals";s:183:"<ul> <li>To illustrate a symbiosis (endosymbiosis type).</li> <li>To identify the nutrients exchanged between the two partners.</li> <li>To study the nitrogen cycle.</li> </ul>";}i:5;a:9:{s:2:"id";i:693;s:5:"title";s:7:"Wegener";s:4:"slug";s:7:"wegener";s:9:"mediaType";s:10:"simulation";s:14:"thumbnailSizes";a:3:{s:9:"node_pack";s:157:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/693-6545f40da0cca660329221.webp";s:10:"suggestion";s:158:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/693-6545f40da0cca660329221.webp";s:5:"title";s:153:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/693-6545f40da0cca660329221.webp";}s:19:"thumbnailBackground";s:7:"#b51d8e";s:11:"publishedAt";O:17:"DateTimeImmutable":3:{s:4:"date";s:26:"2015-05-11 00:00:00.000000";s:13:"timezone_type";i:3;s:8:"timezone";s:3:"UTC";}s:8:"isExpert";b:0;s:5:"goals";s:399:"<ul> <li>To discover the clues that enabled Alfred Wegener to announce his theory of continental drift.</li> <li>To compare Wegener’s hypotheses and those of his detractors of the time (fixism, catastrophism).</li> <li>To complete Wegener’s hypotheses in the light of more recent discoveries (topography of the ocean bottoms, geomagnetism, thermal sources, earthquakes)</li> </ul>";}}s:4:"tags";a:12:{i:0;s:17:"continental drift";i:1;s:10:"continents";i:2;s:5:"earth";i:3;s:10:"earthquake";i:4;s:6:"faults";i:5;s:17:"interactive earth";i:6;s:13:"oceanic ridge";i:7;s:4:"rift";i:8;s:6:"seisms";i:9;s:9:"tectonics";i:10;s:9:"volcanoes";i:11;s:7:"wegener";}s:12:"baseNodeName";s:33:"Environmental science and Ecology";} |
| 7 | 0.05 ms | cache | SADD wJo3GJ9dRH:tagscache-service wJo3GJ9dRH:data > anonymous-media > id=6644,locale=en,domain=www |
| 8 | 0.04 ms | cache | SADD wJo3GJ9dRH:tagscache-service-data > anonymous-media wJo3GJ9dRH:data > anonymous-media > id=6644,locale=en,domain=www |
| 9 | 0.65 ms | cache | EXEC |
| 10 | 14.59 ms | cache | MGET wJo3GJ9dRH:data > locale-page-groups > locale=en |