Components
19
Twig Components
32
Render Count
467
ms
Render Time
14.0
MiB
Memory Usage
Components
Render calls
| Store:User | App\Twig\Components\Store\User | 14.0 MiB | 2.32 ms | |
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| Input props | [] |
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| Attributes | [] |
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| Component | App\Twig\Components\Store\User {#3715 -securityService: App\Service\SecurityService {#115 …} -geoService: App\Service\GeoService {#170 …} -institutionUtilsService: App\Service\InstitutionUtilsService {#3716 …} } |
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| Header |
[Anonymous]
|
14.0 MiB | 160.80 ms | |
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| Input props | [ "notSticky" => false ] |
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| Attributes | [ "notSticky" => false ] |
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| Component | Symfony\UX\TwigComponent\AnonymousComponent {#3746 -props: [ "notSticky" => false ] } |
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| Layout:Stack |
[Anonymous]
|
14.0 MiB | 76.71 ms | |
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| Input props | [ "data-compo" => "Header" "tag" => "header" "class" => "js-header transition bg-domain-dark top-0 relative z-10 p-bento -m-bento rounded-b-md" "data-header-sticky" => "yes" ] |
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| Attributes | [ "data-compo" => "Header" "tag" => "header" "class" => "js-header transition bg-domain-dark top-0 relative z-10 p-bento -m-bento rounded-b-md" "data-header-sticky" => "yes" ] |
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| Component | Symfony\UX\TwigComponent\AnonymousComponent {#3772 -props: [ "data-compo" => "Header" "tag" => "header" "class" => "js-header transition bg-domain-dark top-0 relative z-10 p-bento -m-bento rounded-b-md" "data-header-sticky" => "yes" ] } |
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| Header:Anonymous |
[Anonymous]
|
14.0 MiB | 60.89 ms | |
|---|---|---|---|---|
| Input props | [ "minimal" => false ] |
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| Attributes | [ "minimal" => false ] |
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| Component | Symfony\UX\TwigComponent\AnonymousComponent {#3828 -props: [ "minimal" => false ] } |
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| Header:Logo |
[Anonymous]
|
14.0 MiB | 1.05 ms | |
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| Input props | [] |
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| Attributes | [] |
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| Component | Symfony\UX\TwigComponent\AnonymousComponent {#3852 -props: [] } |
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| Header:LocalePicker |
[Anonymous]
|
14.0 MiB | 19.86 ms | |
|---|---|---|---|---|
| Input props | [ "size" => "small" "hoverScheme" => "none" "darkColor" => "domain" ] |
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| Attributes | [ "size" => "small" "hoverScheme" => "none" "darkColor" => "domain" ] |
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| Component | Symfony\UX\TwigComponent\AnonymousComponent {#3869 -props: [ "size" => "small" "hoverScheme" => "none" "darkColor" => "domain" ] } |
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| Button | App\Twig\Components\Button | 14.0 MiB | 2.11 ms | |
|---|---|---|---|---|
| Input props | [ "data-compo" => "Header/LocalePicker" "tag" => "button" "hoverScheme" => "none" "darkColor" => "domain" "class" => "text-center" "afterIcon" => "expand_more" "command" => "show-modal" "commandfor" => "language-picker-dialog" "size" => "small" ] |
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| Attributes | [ "data-compo" => "Header/LocalePicker" "tag" => "button" "class" => "text-center" "afterIcon" => "expand_more" "command" => "show-modal" "commandfor" => "language-picker-dialog" ] |
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| Component | App\Twig\Components\Button {#3894 +size: "small" +darkColor: "domain" +lightColor: "white" +hoverScheme: "none" +hoverTextColor: null +disabled: false +noLabelOnSmallScreen: false +iconClass: null +beforeIconClass: null +afterIconClass: null } |
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| LoginLink |
[Anonymous]
|
14.0 MiB | 17.20 ms | |
|---|---|---|---|---|
| Input props | [ "class" => "grow" "size" => "small" ] |
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| Attributes | [ "class" => "grow" "size" => "small" ] |
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| Component | Symfony\UX\TwigComponent\AnonymousComponent {#3886 -props: [ "class" => "grow" "size" => "small" ] } |
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| Button | App\Twig\Components\Button | 14.0 MiB | 1.48 ms | |
|---|---|---|---|---|
| Input props | [ "data-compo" => "LoginLink" "href" => "/de/login?next=/de/media/674-mittelozeanischer-ruecken" "class" => "grow" "size" => "small" ] |
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| Attributes | [ "data-compo" => "LoginLink" "href" => "/de/login?next=/de/media/674-mittelozeanischer-ruecken" "class" => "grow" ] |
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| Component | App\Twig\Components\Button {#3972 +size: "small" +darkColor: "domain-dark" +lightColor: "white" +hoverScheme: "default" +hoverTextColor: null +disabled: false +noLabelOnSmallScreen: false +iconClass: null +beforeIconClass: null +afterIconClass: null } |
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| Button | App\Twig\Components\Button | 14.0 MiB | 1.52 ms | |
|---|---|---|---|---|
| Input props | [ "class" => "grow" "size" => "small" "darkColor" => "domain" "href" => "/de/subscribe/" ] |
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| Attributes | [ "class" => "grow" "href" => "/de/subscribe/" ] |
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| Component | App\Twig\Components\Button {#3986 +size: "small" +darkColor: "domain" +lightColor: "white" +hoverScheme: "default" +hoverTextColor: null +disabled: false +noLabelOnSmallScreen: false +iconClass: null +beforeIconClass: null +afterIconClass: null } |
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| Dialog:LocalePicker | App\Twig\Components\Dialog\LocalePicker | 14.0 MiB | 62.74 ms | |
|---|---|---|---|---|
| Input props | [] |
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| Attributes | [] |
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| Component | App\Twig\Components\Dialog\LocalePicker {#3810 -localeSwitcherService: App\Service\LocaleSwitcherService {#1494 …} } |
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| Dialog |
[Anonymous]
|
14.0 MiB | 61.22 ms | |
|---|---|---|---|---|
| Input props | [ "data-compo" => "Dialog/LocalePicker" "id" => "language-picker-dialog" ] |
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| Attributes | [ "data-compo" => "Dialog/LocalePicker" "id" => "language-picker-dialog" ] |
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| Component | Symfony\UX\TwigComponent\AnonymousComponent {#4023 -props: [ "data-compo" => "Dialog/LocalePicker" "id" => "language-picker-dialog" ] } |
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| Button | App\Twig\Components\Button | 14.0 MiB | 1.75 ms | |
|---|---|---|---|---|
| Input props | [ "tag" => "button" "size" => "small" "afterIcon" => "close" "class" => "mb-bento" "hoverScheme" => "none" "hoverTextColor" => "domain" "command" => "close" "commandfor" => "language-picker-dialog" ] |
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| Attributes | [ "tag" => "button" "afterIcon" => "close" "class" => "mb-bento" "command" => "close" "commandfor" => "language-picker-dialog" ] |
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| Component | App\Twig\Components\Button {#4057 +size: "small" +darkColor: "domain-dark" +lightColor: "white" +hoverScheme: "none" +hoverTextColor: "domain" +disabled: false +noLabelOnSmallScreen: false +iconClass: null +beforeIconClass: null +afterIconClass: null } |
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| Button | App\Twig\Components\Button | 14.0 MiB | 3.00 ms | |
|---|---|---|---|---|
| Input props | [ "class" => "w-full mb-bento " "href" => "/en/media/674-mid-ocean-ridge" "hoverScheme" => "none" "hoverTextColor" => "domain" "beforeIcon" => null "beforeIconClass" => "text-domain" "data-locale-picker-target" => "en" ] |
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| Attributes | [ "class" => "w-full mb-bento " "href" => "/en/media/674-mid-ocean-ridge" "beforeIcon" => null "data-locale-picker-target" => "en" ] |
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| Component | App\Twig\Components\Button {#4088 +size: null +darkColor: "domain-dark" +lightColor: "white" +hoverScheme: "none" +hoverTextColor: "domain" +disabled: false +noLabelOnSmallScreen: false +iconClass: null +beforeIconClass: "text-domain" +afterIconClass: null } |
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| Button | App\Twig\Components\Button | 14.0 MiB | 2.23 ms | |
|---|---|---|---|---|
| Input props | [ "class" => "w-full mb-bento " "href" => "/fr/media/674-dorsale-oceanique" "hoverScheme" => "none" "hoverTextColor" => "domain" "beforeIcon" => null "beforeIconClass" => "text-domain" "data-locale-picker-target" => "fr" ] |
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| Attributes | [ "class" => "w-full mb-bento " "href" => "/fr/media/674-dorsale-oceanique" "beforeIcon" => null "data-locale-picker-target" => "fr" ] |
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| Component | App\Twig\Components\Button {#4125 +size: null +darkColor: "domain-dark" +lightColor: "white" +hoverScheme: "none" +hoverTextColor: "domain" +disabled: false +noLabelOnSmallScreen: false +iconClass: null +beforeIconClass: "text-domain" +afterIconClass: null } |
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| Button | App\Twig\Components\Button | 14.0 MiB | 17.23 ms | |
|---|---|---|---|---|
| Input props | [ "class" => "w-full mb-bento " "href" => "/es/media/674-dorsal-oceanica" "hoverScheme" => "none" "hoverTextColor" => "domain" "beforeIcon" => null "beforeIconClass" => "text-domain" "data-locale-picker-target" => "es" ] |
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| Attributes | [ "class" => "w-full mb-bento " "href" => "/es/media/674-dorsal-oceanica" "beforeIcon" => null "data-locale-picker-target" => "es" ] |
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| Component | App\Twig\Components\Button {#4144 +size: null +darkColor: "domain-dark" +lightColor: "white" +hoverScheme: "none" +hoverTextColor: "domain" +disabled: false +noLabelOnSmallScreen: false +iconClass: null +beforeIconClass: "text-domain" +afterIconClass: null } |
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| Button | App\Twig\Components\Button | 14.0 MiB | 1.29 ms | |
|---|---|---|---|---|
| Input props | [ "class" => "w-full mb-bento pointer-events-none" "href" => "/de/media/674-mittelozeanischer-ruecken" "hoverScheme" => "none" "hoverTextColor" => "domain" "beforeIcon" => "done" "beforeIconClass" => "text-domain" "data-locale-picker-target" => "de" ] |
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| Attributes | [ "class" => "w-full mb-bento pointer-events-none" "href" => "/de/media/674-mittelozeanischer-ruecken" "beforeIcon" => "done" "data-locale-picker-target" => "de" ] |
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| Component | App\Twig\Components\Button {#4164 +size: null +darkColor: "domain-dark" +lightColor: "white" +hoverScheme: "none" +hoverTextColor: "domain" +disabled: false +noLabelOnSmallScreen: false +iconClass: null +beforeIconClass: "text-domain" +afterIconClass: null } |
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| Banner:UserBanners | App\Twig\Components\Banner\UserBanners | 14.0 MiB | 0.99 ms | |
|---|---|---|---|---|
| Input props | [] |
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| Attributes | [] |
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| Component | App\Twig\Components\Banner\UserBanners {#3763 -purchaseRepository: App\Repository\PurchaseRepository {#118 …} -securityService: App\Service\SecurityService {#115 …} } |
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| MediaField |
[Anonymous]
|
14.0 MiB | 14.22 ms | |
|---|---|---|---|---|
| Input props | [ "title" => "Lernziele" "media" => [ "id" => 674 "title" => "Mittelozeanischer Rücken" "slug" => "mittelozeanischer-ruecken" "mediaType" => "simulation" "thumbnailSizes" => [ "node_pack" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/674-6545f3ff44fdf668331203.webp" "suggestion" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/674-6545f3ff44fdf668331203.webp" "title" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/674-6545f3ff44fdf668331203.webp" ] "thumbnailBackground" => "#00b7ad" "publishedAt" => DateTimeImmutable @1431302400 {#1377 : 2015-05-11 00:00:00.0 UTC (+00:00) } "isExpert" => false "goals" => """ <ul>\r\n \t<li>Darstellen, wie sich der Meeresboden bildet.</li>\r\n \t<li>Definieren, was Divergenzgrenzen und Transformstörungen sind.</li>\r\n \t<li>Diese Animation in den größeren Rahmen der Plattentektonik und der Kontinentaldrift einordnen.</li>\r\n </ul> """ "width" => 550 "height" => 440 "description" => """ <p>Diese Animaton veranschaulicht in <strong>stark vereinfachter</strong> Form das Aufsteigen von Magma an einem mittelozeanischen Rücken und die Ausbildung von ozeanischer Erdkruste. Ein Rücken ist eine Divergenzzone, an der sich zwei Platten voneinander weg bewegen.<br />\r\n Geologen unterscheiden zwei Haupttypen von Divergenz:</p>\r\n \r\n <ul>\r\n \t<li>Schnelle Rücken, bei denen sich die Platten mit einer Geschwindigkeit von 10 cm pro Jahr (zwischen 12 und 17 cm pro Jahr im Pazifik) voneinander entfernen.</li>\r\n \t<li>Langsame Rücken, bei denen sich die Platten um weniger als 5 cm pro Jahr (etwa 2.5 cm im Atlantik) voneinander entfernen.</li>\r\n </ul>\r\n \r\n <p>Die Topographie des Rückens hängt stark von dieser Geschwindigkeit ab.<br />\r\n Anmerkung: Das Modell des „Laufbands” lässt vermuten, dass der Magmaaufstieg im Zentrum für das Auseinanderdriften der Platten verantwortlich ist. Aktuell gültige geologische Modelle zeigen, dass tiefe, im Mantel befindliche Hadley-Zellen, für großräumige Driftbewegungen verantwortlich sind. Ein Rücken ist folgich wie eine plattentektonische Subduktion (oder Unterschiebung) Resultat des Abdriftens der Kontinente.<br />\r\n Hierbei ist festzuhalten, dass die Theorie der Plattentektonik sehr jung ist. Sie wurde 1967 erstmals erwähnt und wir nachwievor weiterentwickelt.</p> """ "suggestions" => [ App\Entity\vo\MediaCardLight {#3471 #id: 929 #title: "Mittelozeanischer Rücken" #mediaType: "simulation" #thumbnailSizes: [ "node_pack" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/929-6545f47d8c2aa650004055.webp" "suggestion" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/929-6545f47d8c2aa650004055.webp" "title" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/929-6545f47d8c2aa650004055.webp" ] #thumbnailBackground: "#f6adcc" #publishedAt: DateTimeImmutable @1567641600 {#3035 : 2019-09-05 00:00:00.0 UTC (+00:00) } #isExpert: false #slug: "mittelozeanischer-ruecken" } App\Entity\vo\MediaCardLight {#3473 #id: 426 #title: "Die 3 Typen seismischer Wellen" #mediaType: "simulation" #thumbnailSizes: [ "node_pack" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/426-6545f35b22453002997606.webp" "suggestion" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/426-6545f35b22453002997606.webp" "title" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/426-6545f35b22453002997606.webp" ] #thumbnailBackground: "#00b7ad" #publishedAt: DateTimeImmutable @1431302400 {#2900 : 2015-05-11 00:00:00.0 UTC (+00:00) } #isExpert: false #slug: "die-3-typen-seismischer-wellen" } App\Entity\vo\MediaCardLight {#3474 #id: 729 #title: "Geologische Faltenbildung" #mediaType: "simulation" #thumbnailSizes: [ "node_pack" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/729-6545f427c501c539590523.webp" "suggestion" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/729-6545f427c501c539590523.webp" "title" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/729-6545f427c501c539590523.webp" ] #thumbnailBackground: "#ec008d" #publishedAt: DateTimeImmutable @1431302400 {#2968 : 2015-05-11 00:00:00.0 UTC (+00:00) } #isExpert: false #slug: "geologische-faltenbildung" } App\Entity\vo\MediaCardLight {#3475 #id: 188 #title: "Seismische Wellen" #mediaType: "simulation" #thumbnailSizes: [ "node_pack" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/188-6545f2d245c0f349929404.webp" "suggestion" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/188-6545f2d245c0f349929404.webp" "title" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/188-6545f2d245c0f349929404.webp" ] #thumbnailBackground: "#f487b9" #publishedAt: DateTimeImmutable @1431302400 {#2863 : 2015-05-11 00:00:00.0 UTC (+00:00) } #isExpert: false #slug: "seismische-wellen" } App\Entity\vo\MediaCardLight {#3476 #id: 483 #title: "Riftzone" #mediaType: "simulation" #thumbnailSizes: [ "node_pack" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/483-6545f37e2fb7a412032620.webp" "suggestion" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/483-6545f37e2fb7a412032620.webp" "title" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/483-6545f37e2fb7a412032620.webp" ] #thumbnailBackground: "#f487b9" #publishedAt: DateTimeImmutable @1431302400 {#2932 : 2015-05-11 00:00:00.0 UTC (+00:00) } #isExpert: false #slug: "riftzone" } ] "tags" => [ "divergenz" "kontinentaldrift" "meeresboden" "ozean" "ozeanische erdkruste" "platte" "rücken" "störung" "tektonik" "transformstörung" "wegener" ] "baseNodeName" => "Geowissenschaften" ] "key" => "goals" ] |
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| Attributes | [ "title" => "Lernziele" "media" => [ "id" => 674 "title" => "Mittelozeanischer Rücken" "slug" => "mittelozeanischer-ruecken" "mediaType" => "simulation" "thumbnailSizes" => [ "node_pack" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/674-6545f3ff44fdf668331203.webp" "suggestion" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/674-6545f3ff44fdf668331203.webp" "title" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/674-6545f3ff44fdf668331203.webp" ] "thumbnailBackground" => "#00b7ad" "publishedAt" => DateTimeImmutable @1431302400 {#1377 : 2015-05-11 00:00:00.0 UTC (+00:00) } "isExpert" => false "goals" => """ <ul>\r\n \t<li>Darstellen, wie sich der Meeresboden bildet.</li>\r\n \t<li>Definieren, was Divergenzgrenzen und Transformstörungen sind.</li>\r\n \t<li>Diese Animation in den größeren Rahmen der Plattentektonik und der Kontinentaldrift einordnen.</li>\r\n </ul> """ "width" => 550 "height" => 440 "description" => """ <p>Diese Animaton veranschaulicht in <strong>stark vereinfachter</strong> Form das Aufsteigen von Magma an einem mittelozeanischen Rücken und die Ausbildung von ozeanischer Erdkruste. Ein Rücken ist eine Divergenzzone, an der sich zwei Platten voneinander weg bewegen.<br />\r\n Geologen unterscheiden zwei Haupttypen von Divergenz:</p>\r\n \r\n <ul>\r\n \t<li>Schnelle Rücken, bei denen sich die Platten mit einer Geschwindigkeit von 10 cm pro Jahr (zwischen 12 und 17 cm pro Jahr im Pazifik) voneinander entfernen.</li>\r\n \t<li>Langsame Rücken, bei denen sich die Platten um weniger als 5 cm pro Jahr (etwa 2.5 cm im Atlantik) voneinander entfernen.</li>\r\n </ul>\r\n \r\n <p>Die Topographie des Rückens hängt stark von dieser Geschwindigkeit ab.<br />\r\n Anmerkung: Das Modell des „Laufbands” lässt vermuten, dass der Magmaaufstieg im Zentrum für das Auseinanderdriften der Platten verantwortlich ist. Aktuell gültige geologische Modelle zeigen, dass tiefe, im Mantel befindliche Hadley-Zellen, für großräumige Driftbewegungen verantwortlich sind. Ein Rücken ist folgich wie eine plattentektonische Subduktion (oder Unterschiebung) Resultat des Abdriftens der Kontinente.<br />\r\n Hierbei ist festzuhalten, dass die Theorie der Plattentektonik sehr jung ist. Sie wurde 1967 erstmals erwähnt und wir nachwievor weiterentwickelt.</p> """ "suggestions" => [ App\Entity\vo\MediaCardLight {#3471 #id: 929 #title: "Mittelozeanischer Rücken" #mediaType: "simulation" #thumbnailSizes: [ "node_pack" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/929-6545f47d8c2aa650004055.webp" "suggestion" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/929-6545f47d8c2aa650004055.webp" "title" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/929-6545f47d8c2aa650004055.webp" ] #thumbnailBackground: "#f6adcc" #publishedAt: DateTimeImmutable @1567641600 {#3035 : 2019-09-05 00:00:00.0 UTC (+00:00) } #isExpert: false #slug: "mittelozeanischer-ruecken" } App\Entity\vo\MediaCardLight {#3473 #id: 426 #title: "Die 3 Typen seismischer Wellen" #mediaType: "simulation" #thumbnailSizes: [ "node_pack" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/426-6545f35b22453002997606.webp" "suggestion" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/426-6545f35b22453002997606.webp" "title" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/426-6545f35b22453002997606.webp" ] #thumbnailBackground: "#00b7ad" #publishedAt: DateTimeImmutable @1431302400 {#2900 : 2015-05-11 00:00:00.0 UTC (+00:00) } #isExpert: false #slug: "die-3-typen-seismischer-wellen" } App\Entity\vo\MediaCardLight {#3474 #id: 729 #title: "Geologische Faltenbildung" #mediaType: "simulation" #thumbnailSizes: [ "node_pack" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/729-6545f427c501c539590523.webp" "suggestion" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/729-6545f427c501c539590523.webp" "title" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/729-6545f427c501c539590523.webp" ] #thumbnailBackground: "#ec008d" #publishedAt: DateTimeImmutable @1431302400 {#2968 : 2015-05-11 00:00:00.0 UTC (+00:00) } #isExpert: false #slug: "geologische-faltenbildung" } App\Entity\vo\MediaCardLight {#3475 #id: 188 #title: "Seismische Wellen" #mediaType: "simulation" #thumbnailSizes: [ "node_pack" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/188-6545f2d245c0f349929404.webp" "suggestion" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/188-6545f2d245c0f349929404.webp" "title" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/188-6545f2d245c0f349929404.webp" ] #thumbnailBackground: "#f487b9" #publishedAt: DateTimeImmutable @1431302400 {#2863 : 2015-05-11 00:00:00.0 UTC (+00:00) } #isExpert: false #slug: "seismische-wellen" } App\Entity\vo\MediaCardLight {#3476 #id: 483 #title: "Riftzone" #mediaType: "simulation" #thumbnailSizes: [ "node_pack" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/483-6545f37e2fb7a412032620.webp" "suggestion" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/483-6545f37e2fb7a412032620.webp" "title" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/483-6545f37e2fb7a412032620.webp" ] #thumbnailBackground: "#f487b9" #publishedAt: DateTimeImmutable @1431302400 {#2932 : 2015-05-11 00:00:00.0 UTC (+00:00) } #isExpert: false #slug: "riftzone" } ] "tags" => [ "divergenz" "kontinentaldrift" "meeresboden" "ozean" "ozeanische erdkruste" "platte" "rücken" "störung" "tektonik" "transformstörung" "wegener" ] "baseNodeName" => "Geowissenschaften" ] "key" => "goals" ] |
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| Component | Symfony\UX\TwigComponent\AnonymousComponent {#4196 -props: [ "title" => "Lernziele" "media" => [ "id" => 674 "title" => "Mittelozeanischer Rücken" "slug" => "mittelozeanischer-ruecken" "mediaType" => "simulation" "thumbnailSizes" => [ "node_pack" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/674-6545f3ff44fdf668331203.webp" "suggestion" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/674-6545f3ff44fdf668331203.webp" "title" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/674-6545f3ff44fdf668331203.webp" ] "thumbnailBackground" => "#00b7ad" "publishedAt" => DateTimeImmutable @1431302400 {#1377 : 2015-05-11 00:00:00.0 UTC (+00:00) } "isExpert" => false "goals" => """ <ul>\r\n \t<li>Darstellen, wie sich der Meeresboden bildet.</li>\r\n \t<li>Definieren, was Divergenzgrenzen und Transformstörungen sind.</li>\r\n \t<li>Diese Animation in den größeren Rahmen der Plattentektonik und der Kontinentaldrift einordnen.</li>\r\n </ul> """ "width" => 550 "height" => 440 "description" => """ <p>Diese Animaton veranschaulicht in <strong>stark vereinfachter</strong> Form das Aufsteigen von Magma an einem mittelozeanischen Rücken und die Ausbildung von ozeanischer Erdkruste. Ein Rücken ist eine Divergenzzone, an der sich zwei Platten voneinander weg bewegen.<br />\r\n Geologen unterscheiden zwei Haupttypen von Divergenz:</p>\r\n \r\n <ul>\r\n \t<li>Schnelle Rücken, bei denen sich die Platten mit einer Geschwindigkeit von 10 cm pro Jahr (zwischen 12 und 17 cm pro Jahr im Pazifik) voneinander entfernen.</li>\r\n \t<li>Langsame Rücken, bei denen sich die Platten um weniger als 5 cm pro Jahr (etwa 2.5 cm im Atlantik) voneinander entfernen.</li>\r\n </ul>\r\n \r\n <p>Die Topographie des Rückens hängt stark von dieser Geschwindigkeit ab.<br />\r\n Anmerkung: Das Modell des „Laufbands” lässt vermuten, dass der Magmaaufstieg im Zentrum für das Auseinanderdriften der Platten verantwortlich ist. Aktuell gültige geologische Modelle zeigen, dass tiefe, im Mantel befindliche Hadley-Zellen, für großräumige Driftbewegungen verantwortlich sind. Ein Rücken ist folgich wie eine plattentektonische Subduktion (oder Unterschiebung) Resultat des Abdriftens der Kontinente.<br />\r\n Hierbei ist festzuhalten, dass die Theorie der Plattentektonik sehr jung ist. Sie wurde 1967 erstmals erwähnt und wir nachwievor weiterentwickelt.</p> """ "suggestions" => [ App\Entity\vo\MediaCardLight {#3471 #id: 929 #title: "Mittelozeanischer Rücken" #mediaType: "simulation" #thumbnailSizes: [ "node_pack" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/929-6545f47d8c2aa650004055.webp" "suggestion" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/929-6545f47d8c2aa650004055.webp" "title" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/929-6545f47d8c2aa650004055.webp" ] #thumbnailBackground: "#f6adcc" #publishedAt: DateTimeImmutable @1567641600 {#3035 : 2019-09-05 00:00:00.0 UTC (+00:00) } #isExpert: false #slug: "mittelozeanischer-ruecken" } App\Entity\vo\MediaCardLight {#3473 #id: 426 #title: "Die 3 Typen seismischer Wellen" #mediaType: "simulation" #thumbnailSizes: [ "node_pack" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/426-6545f35b22453002997606.webp" "suggestion" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/426-6545f35b22453002997606.webp" "title" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/426-6545f35b22453002997606.webp" ] #thumbnailBackground: "#00b7ad" #publishedAt: DateTimeImmutable @1431302400 {#2900 : 2015-05-11 00:00:00.0 UTC (+00:00) } #isExpert: false #slug: "die-3-typen-seismischer-wellen" } App\Entity\vo\MediaCardLight {#3474 #id: 729 #title: "Geologische Faltenbildung" #mediaType: "simulation" #thumbnailSizes: [ "node_pack" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/729-6545f427c501c539590523.webp" "suggestion" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/729-6545f427c501c539590523.webp" "title" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/729-6545f427c501c539590523.webp" ] #thumbnailBackground: "#ec008d" #publishedAt: DateTimeImmutable @1431302400 {#2968 : 2015-05-11 00:00:00.0 UTC (+00:00) } #isExpert: false #slug: "geologische-faltenbildung" } App\Entity\vo\MediaCardLight {#3475 #id: 188 #title: "Seismische Wellen" #mediaType: "simulation" #thumbnailSizes: [ "node_pack" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/188-6545f2d245c0f349929404.webp" "suggestion" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/188-6545f2d245c0f349929404.webp" "title" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/188-6545f2d245c0f349929404.webp" ] #thumbnailBackground: "#f487b9" #publishedAt: DateTimeImmutable @1431302400 {#2863 : 2015-05-11 00:00:00.0 UTC (+00:00) } #isExpert: false #slug: "seismische-wellen" } App\Entity\vo\MediaCardLight {#3476 #id: 483 #title: "Riftzone" #mediaType: "simulation" #thumbnailSizes: [ "node_pack" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/483-6545f37e2fb7a412032620.webp" "suggestion" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/483-6545f37e2fb7a412032620.webp" "title" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/483-6545f37e2fb7a412032620.webp" ] #thumbnailBackground: "#f487b9" #publishedAt: DateTimeImmutable @1431302400 {#2932 : 2015-05-11 00:00:00.0 UTC (+00:00) } #isExpert: false #slug: "riftzone" } ] "tags" => [ "divergenz" "kontinentaldrift" "meeresboden" "ozean" "ozeanische erdkruste" "platte" "rücken" "störung" "tektonik" "transformstörung" "wegener" ] "baseNodeName" => "Geowissenschaften" ] "key" => "goals" ] } |
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| Demo:Video |
[Anonymous]
|
14.0 MiB | 1.09 ms | |
|---|---|---|---|---|
| Input props | [ "width" => "600" "height" => "596" "class" => "max-w-none absolute" ] |
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| Attributes | [ "width" => "600" "height" => "596" "class" => "max-w-none absolute" ] |
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| Component | Symfony\UX\TwigComponent\AnonymousComponent {#4218 -props: [ "width" => "600" "height" => "596" "class" => "max-w-none absolute" ] } |
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| Heading:Large |
[Anonymous]
|
14.0 MiB | 18.29 ms | |
|---|---|---|---|---|
| Input props | [ "tag" => "h2" ] |
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| Attributes | [ "tag" => "h2" ] |
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| Component | Symfony\UX\TwigComponent\AnonymousComponent {#4234 -props: [ "tag" => "h2" ] } |
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| Showcase:RevealPill |
[Anonymous]
|
14.0 MiB | 19.37 ms | |
|---|---|---|---|---|
| Input props | [ "icon" => "source" ] |
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| Attributes | [ "icon" => "source" ] |
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| Component | Symfony\UX\TwigComponent\AnonymousComponent {#4258 -props: [ "icon" => "source" ] } |
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| Showcase:Reveal |
[Anonymous]
|
14.0 MiB | 17.09 ms | |
|---|---|---|---|---|
| Input props | [ "class" => "-mt-1" "text" => Twig\Markup {#4294 -content: "Mehr als 1000 Ressourcen" -charset: "UTF-8" } ] |
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| Attributes | [ "class" => "-mt-1" "text" => "Mehr als 1000 Ressourcen" ] |
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| Component | Symfony\UX\TwigComponent\AnonymousComponent {#4296 -props: [ "class" => "-mt-1" "text" => Twig\Markup {#4294 -content: "Mehr als 1000 Ressourcen" -charset: "UTF-8" } ] } |
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| DemoForm |
[Anonymous]
|
14.0 MiB | 219.24 ms | |
|---|---|---|---|---|
| Input props | [ "isDemoPage" => false "class" => "max-w-prose mx-auto" ] |
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| Attributes | [ "isDemoPage" => false "class" => "max-w-prose mx-auto" ] |
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| Component | Symfony\UX\TwigComponent\AnonymousComponent {#4280 -props: [ "isDemoPage" => false "class" => "max-w-prose mx-auto" ] } |
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| Button | App\Twig\Components\Button | 14.0 MiB | 3.47 ms | |
|---|---|---|---|---|
| Input props | [ "tag" => "button" "type" => "submit" "darkColor" => "domain" "attributeString" => "id="demo_submit" name="demo[submit]" disabled="disabled"" ] |
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| Attributes | [ "tag" => "button" "type" => "submit" "attributeString" => "id="demo_submit" name="demo[submit]" disabled="disabled"" ] |
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| Component | App\Twig\Components\Button {#4540 +size: null +darkColor: "domain" +lightColor: "white" +hoverScheme: "default" +hoverTextColor: null +disabled: false +noLabelOnSmallScreen: false +iconClass: null +beforeIconClass: null +afterIconClass: null } |
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| Heading:Large |
[Anonymous]
|
14.0 MiB | 1.51 ms | |
|---|---|---|---|---|
| Input props | [ "class" => "text-white" "tag" => "h1" ] |
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| Attributes | [ "class" => "text-white" "tag" => "h1" ] |
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| Component | Symfony\UX\TwigComponent\AnonymousComponent {#4325 -props: [ "class" => "text-white" "tag" => "h1" ] } |
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| MediaCard | App\Twig\Components\MediaCard | 14.0 MiB | 1.89 ms | |
|---|---|---|---|---|
| Input props | [ "cardData" => App\Entity\vo\MediaCardLight {#3471 #id: 929 #title: "Mittelozeanischer Rücken" #mediaType: "simulation" #thumbnailSizes: [ "node_pack" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/929-6545f47d8c2aa650004055.webp" "suggestion" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/929-6545f47d8c2aa650004055.webp" "title" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/929-6545f47d8c2aa650004055.webp" ] #thumbnailBackground: "#f6adcc" #publishedAt: DateTimeImmutable @1567641600 {#3035 : 2019-09-05 00:00:00.0 UTC (+00:00) } #isExpert: false #slug: "mittelozeanischer-ruecken" } "context" => "media-teaser" "class" => "w-1/2 " ] |
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| Attributes | [ "class" => "w-1/2 " ] |
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| Component | App\Twig\Components\MediaCard {#4407 -bgColors: [ "bg-magenta" "bg-pink" "bg-bubble-gum" "bg-navy" "bg-turquoise" "bg-green" "bg-red" "bg-orange" "bg-gold" "bg-purple" "bg-prune" ] -redPixel: "data:image/png;base64,iVBORw0KGgoAAAANSUhEUgAAAAEAAAABCAYAAAAfFcSJAAAADUlEQVR42mN8K63/HwAFbAI4DLWlhgAAAABJRU5ErkJggg==" +cardData: App\Entity\vo\MediaCardLight {#3471 #id: 929 #title: "Mittelozeanischer Rücken" #mediaType: "simulation" #thumbnailSizes: [ "node_pack" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/929-6545f47d8c2aa650004055.webp" "suggestion" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/929-6545f47d8c2aa650004055.webp" "title" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/929-6545f47d8c2aa650004055.webp" ] #thumbnailBackground: "#f6adcc" #publishedAt: DateTimeImmutable @1567641600 {#3035 : 2019-09-05 00:00:00.0 UTC (+00:00) } #isExpert: false #slug: "mittelozeanischer-ruecken" } +thumbnailEagerLoading: false +preventTabbableLink: false +context: "media-teaser" } |
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| MediaCard | App\Twig\Components\MediaCard | 14.0 MiB | 0.94 ms | |
|---|---|---|---|---|
| Input props | [ "cardData" => App\Entity\vo\MediaCardLight {#3473 #id: 426 #title: "Die 3 Typen seismischer Wellen" #mediaType: "simulation" #thumbnailSizes: [ "node_pack" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/426-6545f35b22453002997606.webp" "suggestion" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/426-6545f35b22453002997606.webp" "title" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/426-6545f35b22453002997606.webp" ] #thumbnailBackground: "#00b7ad" #publishedAt: DateTimeImmutable @1431302400 {#2900 : 2015-05-11 00:00:00.0 UTC (+00:00) } #isExpert: false #slug: "die-3-typen-seismischer-wellen" } "context" => "media-teaser" "class" => "w-1/2 hidden md:block" ] |
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| Attributes | [ "class" => "w-1/2 hidden md:block" ] |
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| Component | App\Twig\Components\MediaCard {#4620 -bgColors: [ "bg-magenta" "bg-pink" "bg-bubble-gum" "bg-navy" "bg-turquoise" "bg-green" "bg-red" "bg-orange" "bg-gold" "bg-purple" "bg-prune" ] -redPixel: "data:image/png;base64,iVBORw0KGgoAAAANSUhEUgAAAAEAAAABCAYAAAAfFcSJAAAADUlEQVR42mN8K63/HwAFbAI4DLWlhgAAAABJRU5ErkJggg==" +cardData: App\Entity\vo\MediaCardLight {#3473 #id: 426 #title: "Die 3 Typen seismischer Wellen" #mediaType: "simulation" #thumbnailSizes: [ "node_pack" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/426-6545f35b22453002997606.webp" "suggestion" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/426-6545f35b22453002997606.webp" "title" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/426-6545f35b22453002997606.webp" ] #thumbnailBackground: "#00b7ad" #publishedAt: DateTimeImmutable @1431302400 {#2900 : 2015-05-11 00:00:00.0 UTC (+00:00) } #isExpert: false #slug: "die-3-typen-seismischer-wellen" } +thumbnailEagerLoading: false +preventTabbableLink: false +context: "media-teaser" } |
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| MediaCard | App\Twig\Components\MediaCard | 14.0 MiB | 0.62 ms | |
|---|---|---|---|---|
| Input props | [ "cardData" => App\Entity\vo\MediaCardLight {#3474 #id: 729 #title: "Geologische Faltenbildung" #mediaType: "simulation" #thumbnailSizes: [ "node_pack" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/729-6545f427c501c539590523.webp" "suggestion" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/729-6545f427c501c539590523.webp" "title" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/729-6545f427c501c539590523.webp" ] #thumbnailBackground: "#ec008d" #publishedAt: DateTimeImmutable @1431302400 {#2968 : 2015-05-11 00:00:00.0 UTC (+00:00) } #isExpert: false #slug: "geologische-faltenbildung" } "context" => "media-teaser" "class" => "w-1/2 hidden lg:block" ] |
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| Attributes | [ "class" => "w-1/2 hidden lg:block" ] |
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| Component | App\Twig\Components\MediaCard {#4648 -bgColors: [ "bg-magenta" "bg-pink" "bg-bubble-gum" "bg-navy" "bg-turquoise" "bg-green" "bg-red" "bg-orange" "bg-gold" "bg-purple" "bg-prune" ] -redPixel: "data:image/png;base64,iVBORw0KGgoAAAANSUhEUgAAAAEAAAABCAYAAAAfFcSJAAAADUlEQVR42mN8K63/HwAFbAI4DLWlhgAAAABJRU5ErkJggg==" +cardData: App\Entity\vo\MediaCardLight {#3474 #id: 729 #title: "Geologische Faltenbildung" #mediaType: "simulation" #thumbnailSizes: [ "node_pack" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/729-6545f427c501c539590523.webp" "suggestion" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/729-6545f427c501c539590523.webp" "title" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/729-6545f427c501c539590523.webp" ] #thumbnailBackground: "#ec008d" #publishedAt: DateTimeImmutable @1431302400 {#2968 : 2015-05-11 00:00:00.0 UTC (+00:00) } #isExpert: false #slug: "geologische-faltenbildung" } +thumbnailEagerLoading: false +preventTabbableLink: false +context: "media-teaser" } |
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| MediaCard | App\Twig\Components\MediaCard | 14.0 MiB | 2.46 ms | |
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| Input props | [ "cardData" => App\Entity\vo\MediaCardLight {#3475 #id: 188 #title: "Seismische Wellen" #mediaType: "simulation" #thumbnailSizes: [ "node_pack" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/188-6545f2d245c0f349929404.webp" "suggestion" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/188-6545f2d245c0f349929404.webp" "title" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/188-6545f2d245c0f349929404.webp" ] #thumbnailBackground: "#f487b9" #publishedAt: DateTimeImmutable @1431302400 {#2863 : 2015-05-11 00:00:00.0 UTC (+00:00) } #isExpert: false #slug: "seismische-wellen" } "context" => "media-teaser" "class" => "w-1/2 hidden lg:block" ] |
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| Attributes | [ "class" => "w-1/2 hidden lg:block" ] |
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| Component | App\Twig\Components\MediaCard {#4667 -bgColors: [ "bg-magenta" "bg-pink" "bg-bubble-gum" "bg-navy" "bg-turquoise" "bg-green" "bg-red" "bg-orange" "bg-gold" "bg-purple" "bg-prune" ] -redPixel: "data:image/png;base64,iVBORw0KGgoAAAANSUhEUgAAAAEAAAABCAYAAAAfFcSJAAAADUlEQVR42mN8K63/HwAFbAI4DLWlhgAAAABJRU5ErkJggg==" +cardData: App\Entity\vo\MediaCardLight {#3475 #id: 188 #title: "Seismische Wellen" #mediaType: "simulation" #thumbnailSizes: [ "node_pack" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/188-6545f2d245c0f349929404.webp" "suggestion" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/188-6545f2d245c0f349929404.webp" "title" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/188-6545f2d245c0f349929404.webp" ] #thumbnailBackground: "#f487b9" #publishedAt: DateTimeImmutable @1431302400 {#2863 : 2015-05-11 00:00:00.0 UTC (+00:00) } #isExpert: false #slug: "seismische-wellen" } +thumbnailEagerLoading: false +preventTabbableLink: false +context: "media-teaser" } |
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| MediaCard | App\Twig\Components\MediaCard | 14.0 MiB | 1.65 ms | |
|---|---|---|---|---|
| Input props | [ "cardData" => App\Entity\vo\MediaCardLight {#3476 #id: 483 #title: "Riftzone" #mediaType: "simulation" #thumbnailSizes: [ "node_pack" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/483-6545f37e2fb7a412032620.webp" "suggestion" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/483-6545f37e2fb7a412032620.webp" "title" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/483-6545f37e2fb7a412032620.webp" ] #thumbnailBackground: "#f487b9" #publishedAt: DateTimeImmutable @1431302400 {#2932 : 2015-05-11 00:00:00.0 UTC (+00:00) } #isExpert: false #slug: "riftzone" } "context" => "media-teaser" "class" => "w-1/2 hidden lg:block" ] |
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| Attributes | [ "class" => "w-1/2 hidden lg:block" ] |
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| Component | App\Twig\Components\MediaCard {#4686 -bgColors: [ "bg-magenta" "bg-pink" "bg-bubble-gum" "bg-navy" "bg-turquoise" "bg-green" "bg-red" "bg-orange" "bg-gold" "bg-purple" "bg-prune" ] -redPixel: "data:image/png;base64,iVBORw0KGgoAAAANSUhEUgAAAAEAAAABCAYAAAAfFcSJAAAADUlEQVR42mN8K63/HwAFbAI4DLWlhgAAAABJRU5ErkJggg==" +cardData: App\Entity\vo\MediaCardLight {#3476 #id: 483 #title: "Riftzone" #mediaType: "simulation" #thumbnailSizes: [ "node_pack" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_node_pack/uploads/media/thumbnails/483-6545f37e2fb7a412032620.webp" "suggestion" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_suggestion/uploads/media/thumbnails/483-6545f37e2fb7a412032620.webp" "title" => "https://www.preprod-yousg3q-etbsswybjvlic.fr-3.platformsh.site/media-cache/media_thumbnail_title/uploads/media/thumbnails/483-6545f37e2fb7a412032620.webp" ] #thumbnailBackground: "#f487b9" #publishedAt: DateTimeImmutable @1431302400 {#2932 : 2015-05-11 00:00:00.0 UTC (+00:00) } #isExpert: false #slug: "riftzone" } +thumbnailEagerLoading: false +preventTabbableLink: false +context: "media-teaser" } |
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| Footer |
[Anonymous]
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14.0 MiB | 21.38 ms | |
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| Input props | [] |
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| Attributes | [] |
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| Component | Symfony\UX\TwigComponent\AnonymousComponent {#4243 -props: [] } |
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