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Failed Queries
| # | Time | Connection | Command |
|---|---|---|---|
| 1 | 0.53 ms | cache | CONNECT redis.internal 6379 5 <null> 5 5 |
| 2 | 0.27 ms | cache | SELECT 0 |
| 3 | 0.20 ms | cache | MGET wJo3GJ9dRH:data > anonymous-media > id=5312,locale=en,domain=www |
| 4 | 0.76 ms | cache | INFO Memory |
| 5 | 0.02 ms | cache | MULTI 2 |
| 6 | 0.10 ms | cache | SETEX wJo3GJ9dRH:data > anonymous-media > id=5312,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:674;s:5:"title";s:15:"Mid-ocean ridge";s:4:"slug";s:15:"mid-ocean-ridge";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/674-6545f3ff44fdf668331203.webp";s:10:"suggestion";s:158:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/674-6545f3ff44fdf668331203.webp";s:5:"title";s:153:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/674-6545f3ff44fdf668331203.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:225:"<ul> <li>Illustrate how the ocean floor forms.</li> <li>Define transformation fault and a diverging frontier</li> <li>Replace this animation in a more general setting of plate tectonics and continental drift</li> </ul>";s:5:"width";i:550;s:6:"height";i:440;s:11:"description";s:1190:"<p>This animation illustrates in a <strong>very simplified</strong> manner, the rising of magma at the mid-oceanic ridge level and the creation of oceanic crust. A ridge is a zone of divergence where two plates separate from each other.</p> <p>Geologists distinguish two types of divergence:</p> <ul> <li>Fast ridges which separate more than 10 cm per year (between 12 and 17 cm per year for the Pacific Ocean ridges).</li> <li>Slow ridges which separate less than 5 cm per year (about 2.5 cm per year for the Atlantic ridge).</li> </ul> <p>The topography of the ridge strongly depends on this speed.</p> <p><em>Note:</em> The rolling carpet model presented in this animation can lead you to believe that the rising of magma in the centre is the cause of the separation of plates. This is not the case. Geological models actually show that the deep convection currents, situated in the mantle would be the cause of a drifting movement of plates on a large scale. The ridge, like subduction, would therefore be a consequence of continental drift.</p> <p>Note that the plate tectonic theory is a young theory, announced in 1967, and is always evolving.</p>";s:11:"suggestions";a:6:{i:0;a:9:{s:2:"id";i:929;s:5:"title";s:15:"Mid-ocean ridge";s:4:"slug";s:15:"mid-ocean-ridge";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/929-6545f47d8c2aa650004055.webp";s:10:"suggestion";s:158:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/929-6545f47d8c2aa650004055.webp";s:5:"title";s:153:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/929-6545f47d8c2aa650004055.webp";}s:19:"thumbnailBackground";s:7:"#f6adcc";s:11:"publishedAt";O:17:"DateTimeImmutable":3:{s:4:"date";s:26:"2019-05-21 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:313:"<ul> <li>To understand the functioning of an oceanic ridge and the magmatism of oceanic ridges.</li> <li>To illustrate how the oceanic crust forms and how it evolves.</li> <li>To describe the geological properties of the rocks that make up the oceanic lithosphere: peridotite, basalt and gabbro.</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:157:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/426-6545f35b22453002997606.webp";s:10:"suggestion";s:158:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/426-6545f35b22453002997606.webp";s:5:"title";s:153:"https://www.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:729;s:5:"title";s:16:"Geological folds";s:4:"slug";s:16:"geological-folds";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/729-6545f427c501c539590523.webp";s:10:"suggestion";s:158:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/729-6545f427c501c539590523.webp";s:5:"title";s:153:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/729-6545f427c501c539590523.webp";}s:19:"thumbnailBackground";s:7:"#ec008d";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:224:"<ul> <li>To define the principal forms of geological folds.</li> <li>To define the hinge of a fold and its axial plane.</li> <li>To illustrate the relation between the form of a fold and pressure intensity.</li> </ul>";}i:3;a:9:{s:2:"id";i:188;s:5:"title";s:13:"Seismic waves";s:4:"slug";s:13:"seismic-waves";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/188-6545f2d245c0f349929404.webp";s:10:"suggestion";s:158:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/188-6545f2d245c0f349929404.webp";s:5:"title";s:153:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/188-6545f2d245c0f349929404.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:93:"<ul> <li>To illustrate seismic waves propagation and their corresponding speed.</li> </ul>";}i:4;a:9:{s:2:"id";i:483;s:5:"title";s:11:"Rift Valley";s:4:"slug";s:11:"rift-valley";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/483-6545f37e2fb7a412032620.webp";s:10:"suggestion";s:158:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/483-6545f37e2fb7a412032620.webp";s:5:"title";s:153:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/483-6545f37e2fb7a412032620.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:208:"<ul> <li>To observe the effects of pressure during expansion.</li> <li>To introduce the rift and the oceanic ridge.</li> <li>To make the connection between similar phenomena (graben, horst).</li> </ul>";}i:5;a:9:{s:2:"id";i:738;s:5:"title";s:22:"Speed of seismic waves";s:4:"slug";s:22:"speed-of-seismic-waves";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/738-6545f42c56409336792605.webp";s:10:"suggestion";s:158:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/738-6545f42c56409336792605.webp";s:5:"title";s:153:"https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/738-6545f42c56409336792605.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:94:"<ul> <li>To illustrate propagation of seismic waves and their respective speeds.</li> </ul>";}}s:4:"tags";a:11:{i:0;s:17:"continental drift";i:1;s:10:"divergence";i:2;s:5:"fault";i:3;s:5:"ocean";i:4;s:11:"ocean floor";i:5;s:13:"oceanic crust";i:6;s:5:"plate";i:7;s:5:"ridge";i:8;s:9:"tectonics";i:9;s:20:"transformation fault";i:10;s:7:"wegener";}s:12:"baseNodeName";s:13:"Earth science";} |
| 7 | 0.05 ms | cache | SADD wJo3GJ9dRH:tagscache-service wJo3GJ9dRH:data > anonymous-media > id=5312,locale=en,domain=www |
| 8 | 0.06 ms | cache | SADD wJo3GJ9dRH:tagscache-service-data > anonymous-media wJo3GJ9dRH:data > anonymous-media > id=5312,locale=en,domain=www |
| 9 | 0.84 ms | cache | EXEC |
| 10 | 1.88 ms | cache | MGET wJo3GJ9dRH:data > locale-page-groups > locale=en |