Symfony Profiler

• Request / Response
• Performance
• Validator
• Forms
• Exception
• Logs 12
• Events
• Routing
• Cache
• Translation 250
• Security
• Twig
• Twig Components
• HTTP Client
• Doctrine
• Debug
• Messages
• Emails
• Notifications
• Serializer
• EasyAdmin
• VichUploader
• Doctrine MongoDB 0
• Redis
• Vite
• Configuration

Commands

#	Time	Connection	Command
1	0.63 ms	cache	CONNECT redis.internal 6379 5 <null> 5 5
2	0.33 ms	cache	SELECT 0
3	0.19 ms	cache	MGET wJo3GJ9dRH:data > anonymous-media > id=2668,locale=es,domain=junior
4	0.40 ms	cache	INFO Memory
5	0.02 ms	cache	MULTI 2
6	0.06 ms	cache	SETEX wJo3GJ9dRH:data > anonymous-media > id=2668,locale=es,domain=junior 2678399 ��CB�_Oa:2:{i:0;s:13:"cache-service";i:1;s:36:"cache-service-data > anonymous-media";}a:15:{s:2:"id";i:39;s:5:"title";s:20:"Tsunami del 26-12-04";s:4:"slug";s:20:"tsunami-del-26-12-04";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:107:"<ul> <li>Observar la propagaci&oacute;n del tsunami del 26-12-2004 en el Oc&eacute;ano Indio.</li> </ul>";s:5:"width";i:550;s:6:"height";i:440;s:11:"description";s:180:"<p>Ilustraci&oacute;n de la progresi&oacute;n del tsunami del 26 de diciembre del 2004, a partir del epicentro del se&iacute;smo, sobre el mapa del Oc&eacute;ano &Iacute;ndico.</p>";s:11:"suggestions";a:6:{i:0;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:96:"<ul> <li>Comprender la sucesi&oacute;n de acontecimientos que llevan a un tsunami.</li> </ul>";}i:1;a:9:{s:2:"id";i:638;s:5:"title";s:26:"Diferentes tipos de fallas";s:4:"slug";s:26:"diferentes-tipos-de-fallas";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:65:"<ul> <li>Estudio de los diferentes tipos de fallas.</li> </ul>";}i:2;a:9:{s:2:"id";i:454;s:5:"title";s:21:"Interior de la Tierra";s:4:"slug";s:21:"interior-de-la-tierra";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:104:"<ul> <li>Disponer de una visi&oacute;n hecha a escala de las capas sucesivas de la Tierra.</li> </ul>";}i:3;a:9:{s:2:"id";i:426;s:5:"title";s:33:"Los tres tipos de ondas sísmicas";s:4:"slug";s:32:"los-tres-tipos-de-ondas-sismicas";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:83:"<ul> <li>Estudiar la propagaci&oacute;n de las ondas s&iacute;smicas.</li> </ul>";}i:4;a:9:{s:2:"id";i:585;s:5:"title";s:34:"Placas litosféricas (tectónicas)";s:4:"slug";s:30:"placas-litosfericas-tectonicas";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:286:"<ul> <li>Observar la repartici&oacute;n de las placas litosf&eacute;ricas y sus movimientos.</li> <li>Relacionar la topograf&iacute;a de los fondos oce&aacute;nicos, la actividad s&iacute;smica y el volcanismo, la edad de los fondos marinos y el flujo geot&eacute;rmico.</li> </ul>";}i:5;a:9:{s:2:"id";i:398;s:5:"title";s:12:"Día y noche";s:4:"slug";s:11:"dia-y-noche";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:73:"<ul> <li>Comprender la alternaci&oacute;n d&iacute;a/noche.</li> </ul>";}}s:4:"tags";a:6:{i:0;s:9:"epicentro";i:1;s:8:"maremoto";i:2;s:4:"onda";i:3;s:7:"seísmo";i:4;s:10:"tectónica";i:5;s:7:"tsunami";}s:12:"baseNodeName";s:20:"El cielo y la Tierra";}
7	0.02 ms	cache	SADD wJo3GJ9dRH: tags cache-service wJo3GJ9dRH:data > anonymous-media > id=2668,locale=es,domain=junior
8	0.02 ms	cache	SADD wJo3GJ9dRH: tags cache-service-data > anonymous-media wJo3GJ9dRH:data > anonymous-media > id=2668,locale=es,domain=junior
9	0.38 ms	cache	EXEC
10	2.71 ms	cache	MGET wJo3GJ9dRH:data > locale-page-groups > locale=es