Commands
10
Queries
4.94 ms
Query time
0
Failed Queries
| # | Time | Connection | Command |
|---|---|---|---|
| 1 | 0.71 ms | cache | CONNECT redis.internal 6379 5 <null> 5 5 |
| 2 | 0.42 ms | cache | SELECT 0 |
| 3 | 0.31 ms | cache | MGET wJo3GJ9dRH:data > anonymous-media > id=4969,locale=en,domain=junior |
| 4 | 0.74 ms | cache | INFO Memory |
| 5 | 0.04 ms | cache | MULTI 2 |
| 6 | 0.13 ms | cache | SETEX wJo3GJ9dRH:data > anonymous-media > id=4969,locale=en,domain=junior 2678399 �(�A N_ Oa:2:{i:0;s:13:"cache-service";i:1;s:36:"cache-service-data > anonymous-media";}a:15:{s:2:"id";i:638;s:5:"title";s:25:"Different types of faults";s:4:"slug";s:25:"different-types-of-faults";s:9:"mediaType";s:10:"simulation";s:14:"thumbnailSizes";a:3:{s:9:"node_pack";s:160:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/638-6545f3e705948949390576.webp";s:10:"suggestion";s:161:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/638-6545f3e705948949390576.webp";s:5:"title";s:156:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/638-6545f3e705948949390576.webp";}s:19:"thumbnailBackground";s:7:"#f487b9";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:67:"<ul> <li>To illustrate the different types of faults.</li> </ul>";s:5:"width";i:550;s:6:"height";i:440;s:11:"description";s:163:"<p>Three types of fault movements (normal, reverse and strike-slip faults) are illustrated, along with their locations on a lithospheric plates boundaries map.</p>";s:11:"suggestions";a:6:{i:0;a:9:{s:2:"id";i:39;s:5:"title";s:24:"December 26 2004 Tsunami";s:4:"slug";s:24:"december-26-2004-tsunami";s:9:"mediaType";s:10:"simulation";s:14:"thumbnailSizes";a:3:{s:9:"node_pack";s:159:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/39-6545f3462f88a785335328.webp";s:10:"suggestion";s:160:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/39-6545f3462f88a785335328.webp";s:5:"title";s:155:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/39-6545f3462f88a785335328.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:86:"<ul> <li>To observe the tsunami’s progression in the Indian Ocean.</li> </ul>";}i:1;a:9:{s:2:"id";i:426;s:5:"title";s:28:"The 3 types of seismic waves";s:4:"slug";s:28:"the-3-types-of-seismic-waves";s:9:"mediaType";s:10:"simulation";s:14:"thumbnailSizes";a:3:{s:9:"node_pack";s:160:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/426-6545f35b22453002997606.webp";s:10:"suggestion";s:161:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/426-6545f35b22453002997606.webp";s:5:"title";s:156:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/426-6545f35b22453002997606.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:65:"<ul> <li>To study the propagation of seismic waves.</li> </ul>";}i:2;a:9:{s:2:"id";i:210;s:5:"title";s:7:"Tsunami";s:4:"slug";s:7:"tsunami";s:9:"mediaType";s:10:"simulation";s:14:"thumbnailSizes";a:3:{s:9:"node_pack";s:160:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/210-6545f2df90bc8496958036.webp";s:10:"suggestion";s:161:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/210-6545f2df90bc8496958036.webp";s:5:"title";s:156:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/210-6545f2df90bc8496958036.webp";}s:19:"thumbnailBackground";s:7:"#462f92";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:80:"<ul> <li>To understand the successive events leading to a tsunami.</li> </ul>";}i:3;a:9:{s:2:"id";i:398;s:5:"title";s:13:"Day and night";s:4:"slug";s:13:"day-and-night";s:9:"mediaType";s:10:"simulation";s:14:"thumbnailSizes";a:3:{s:9:"node_pack";s:160:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/398-6545f34b104cd302421004.webp";s:10:"suggestion";s:161:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/398-6545f34b104cd302421004.webp";s:5:"title";s:156:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/398-6545f34b104cd302421004.webp";}s:19:"thumbnailBackground";s:7:"#f6adcc";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:63:"<ul> <li>To understand the night & day cycle.</li> </ul>";}i:4;a:9:{s:2:"id";i:454;s:5:"title";s:16:"Earth's interior";s:4:"slug";s:16:"earth-s-interior";s:9:"mediaType";s:10:"simulation";s:14:"thumbnailSizes";a:3:{s:9:"node_pack";s:160:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/454-6545f36b51ed2437647496.webp";s:10:"suggestion";s:161:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/454-6545f36b51ed2437647496.webp";s:5:"title";s:156:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/454-6545f36b51ed2437647496.webp";}s:19:"thumbnailBackground";s:7:"#ee1b2e";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:176:"<ul> <li>To develop understanding of the structure of the Earth’s interior.</li> <li>To illustrate the importance of proportions and the concept of scale.</li> </ul>";}i:5;a:9:{s:2:"id";i:585;s:5:"title";s:19:"Lithospheric plates";s:4:"slug";s:19:"lithospheric-plates";s:9:"mediaType";s:10:"simulation";s:14:"thumbnailSizes";a:3:{s:9:"node_pack";s:160:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/585-6545f3c11d274678813393.webp";s:10:"suggestion";s:161:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/585-6545f3c11d274678813393.webp";s:5:"title";s:156:"https://junior.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/585-6545f3c11d274678813393.webp";}s:19:"thumbnailBackground";s:7:"#462f92";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:263:"<ul> <li>To observe the arrangement of the lithospheric plates and their respective movements.</li> <li>To make the connection between the ocean floor’s topography, seismic and volcanic activity, the age of ocean floors and geothermic waves.</li> </ul>";}}s:4:"tags";a:11:{i:0;s:9:"collision";i:1;s:11:"convergence";i:2;s:10:"divergence";i:3;s:10:"earthquake";i:4;s:5:"fault";i:5;s:18:"lithospheric plate";i:6;s:13:"oceanic ridge";i:7;s:4:"rift";i:8;s:6:"seisms";i:9;s:6:"strike";i:10;s:10:"subduction";}s:12:"baseNodeName";s:27:"Earth science and astronomy";} |
| 7 | 0.06 ms | cache | SADD wJo3GJ9dRH:tagscache-service wJo3GJ9dRH:data > anonymous-media > id=4969,locale=en,domain=junior |
| 8 | 0.04 ms | cache | SADD wJo3GJ9dRH:tagscache-service-data > anonymous-media wJo3GJ9dRH:data > anonymous-media > id=4969,locale=en,domain=junior |
| 9 | 0.66 ms | cache | EXEC |
| 10 | 1.83 ms | cache | MGET wJo3GJ9dRH:data > locale-page-groups > locale=en |