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Inquiry Learning Spaces (ILSs) are personalized learning resources for students, including a lab, apps, and any other type of multimedia material. ILSs follow an inquiry cycle. Inquiry cycles can differ but the basic Go-Lab cycle consists of the phases Orientation, Conceptualisation, Investigation, Conclusion, and Discussion. The aim of an ILS is to provide students with an opportunity to conduct scientific experiments, being guided through the inquiry process and supported at each step.

This page presents ILSs created by teachers or the Go-Lab and/or Next-Lab team (and often in co-creation), on a large set of domains and in many languages. Please note that the Go-Lab Authoring Platform Graasp is no longer maintained. This means that it is not possible to create and publish new Go-Lab ILSs, preview or copy ILSs listed on this page. It is only possible to view the descriptions of ILSs, which were created and published during the lifetime of the Go-Lab projects. This page can be used for your information only. If you are interested in creating and using Inquiry Learning Spaces in your classroom, please visit the new Authoring Platform Graasp.org

If you are looking for Inquiry Learning Spaces created especially for the curricula of Benin, Kenya or Nigeria, please visit our Collections page.

Geography And Earth S...
Structure Of Matter
13-14
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Lód może przybierać różne formy: od płatków śniegu, przez kostki lodu, po lód morski i lód lodowcowy. Uczniowie dowiedzą się, jak bardzo lód morski różni się od lodu lodowcowego i jakie są konsekwencje topnienia lodu.

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Find out, what forms may ice have and check, how melting ice influences the sea level!

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This is the Irish language version of Permafrost from PolarStar.

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This is the Irish Language version of Arctic Amplification.

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Ikirouta on pysyvästi jäässä olevaa maata, jonka lämpötila pysyy  0°C:ssa tai sen alle vähintään kaksi peräkkäistä vuotta. Se pitää sisällään multaa, kiveä ja eloperäistä ainesta, joka ei ole päässyt hajoamaan, koska se on jäässä.

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Dowiesz się, czym jest wieloletnia zmarzlina, gdzie występuje i jak powstaje.

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Este ILS ambiental apresentado foi projetado implementando a abordagem científica. Nesta atividade, os alunos aprendem sobre a ciência por trás do Efeito Estufa e como diferentes moléculas interagem com a radiação eletromagnética.

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Viimeisten vuosikymmenien aikana arktiset alueet ovat lämmenneet kaksi kertaa nopeammin kuin maailma keskimäärin. Merijään häviäminen vahvistaa lämpenemistä, koska meren pinta absorboi enemmän auringon lämpöenergiaa kuin lumen tai jään pinta. Miten tämä vaikuttaa planeettaamme? 

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Το παρόν μάθημα ακολουθεί το μοντέλο ανακαλυπτικής μάθησης. Σε αυτό το μάθημα οι μαθητές μαθαίνουν για το φαινόμενο του θερμοκηπίου και πως τα διάφορα μόρια αλληλεπιδρούν με την ηλεκτρομαγνητική ακτινοβολία.

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La tendencia al calentamiento en el Ártico es dos veces mayor que la media mundial en las últimas décadas. La pérdida de hielo marino amplifica la tendencia al calentamiento porque la superficie del océano absorbe más calor del sol que la superficie de nieve y hielo.