Announcement for the 11th IAG International Conference on Geomorphology (2-6 February 2026, Christchurch, New Zealand)

The IAG is delighted to announce its 11th International Conference on Geomorphology! It will take place in Christchurch, New Zealand (Ōtautahi, Aotearoa) on 2-6 February 2026!

The Conference will include scientific sessions, workshops and field trips. All details are available on the web page of the event: https://www.geomorph.org/11th-iag-international-conference-on-geomorphology-2-6-february-2026-christchurch-new-zealand/.

You can also visit the website of the event: https://www.confer.co.nz/icg2026/call-for-abstracts/
and express your interest by subscribing to the mailing list: https://confer.eventsair.com/icg2026/eoi/Site/Register.

All key dates for the event can be found below – or in pdf here.

8th Badlands Working Group Workshop (online, 16 July 2024)

The IAG Badlands Working Group organises its 8th Workshop on July 16th (14:00-16:00 CET)!

This Workshop will take the form of a webinar. Four speakers will present various aspects of badlands research, such as land use, structural control or soil erosion, in various badlands regions (e.g. Türkiye, Spain, India). The seminars will be followed by the Badlands Working Group Meeting.

Find the detailed programme here. The meeting will be held online- the link will be shared soon.

IAG Photo Contest – winner May 2024

The winner of the IAG Photo Contest in May 2024 is Furkan Karabacak (Türkiye)! Find below his photo and descriptive text.

If you want to participate in the contest, find the rules, guidelines and details on the procedure here.


Badlands – a fascinating landscape formed by multi-processes

by Furkan Karabacak, Türkiye

The Nallihan badlands area is a landscape that makes you feel like you are on another planet. It is located in an extremely arid area in the interior of the Anatolian Orogenic Plateau, Türkiye. The badlands is composed of a Paleocene-aged conglomerate, marl, clay and sandstone terrestrial series, and its morphology is characterised by steep slopes, a thin regolith layer, and high drainage density. With its fascinating forms caused by differential erosion and colors reflecting various paleo-environmental conditions, this area is also a favorite spot for geomorphology enthusiasts.