Projects
Find out more about our projects

The EXCESS project will collect unprecedented data covering parts of the world susceptible to landslides. The project, led by the University of Plymouth, started in February 2024 and will run for three years. It is being funded through a grant of £778,812 from the Natural Environment Research Council.
The Quake4D project is funded by UK Research and Innovation as part of their Future Leaders Fellowship funding which has been awarded to Dr Zoë Mildon.
Quake4D is a four year project worth £1.1 million, that will unite geology, physics and computer modelling to develop new approaches to understanding and calculating earthquake hazard.
SENSUM proposes a novel integrated approach for the management of hydrogeological hazards, leveraging advances in Wireless Sensor Net-works (WSNs) and Internet of Things (IoT) technologies, microelectronics and machine learning to provide warnings of hazardous events and im-prove numerical models of their dynamics.
SENSUM is a £1.2 million project funded by the Natural Environment Research Council (NERC) under its Constructing a Digital Environment programme.
This NERC-funded project aims to discover how magma is transported during the construction of oceanic crust during seafloor spreading.
The project will combine magnetic fabric, paleomagnetic and geochemical methods and will develop a comprehensive model for the anatomy of the magma systems responsible for forming two-thirds of the Earth's surface, using the rock record to test and challenge current paradigms for seafloor spreading processes.
Tsunamis generated by large mass flows, like large landslides and pyroclastic density currents (PDCs), constitute a lethal hazard in volcanic areas. This project aims to collect field data about recent events in Stromboli to accurately assess the process that triggered the tsunamis. By means of numerical simulations key parameters will be characterised that will help improve the early warning system and reduce the risk related to these unpredictable but extremely dangerous phenomena.
The project is funded by the UK Natural Environment Research Council.
The NERC-funded ‘Equable Earth’ project is trying to determine what temperatures were like across North America during the Cretaceous-Palaeogene boundary.Learn more about the project
The present project involves a multidisciplinary, international and diverse team who is working closely with local authorities and communities to incorporate digital field datasets and citizen science to enhance the knowledge of citizens about natural hazards, risk perception and post-disaster long term recovery and resilience patterns.
NET is funded by the Royal Academy of Engineering with the Frontiers of Development Seed funding Programme under the Global Challenges Research Fund (GCRF).
Understanding how tectonics and climate interact to shape landscape change is a key challenge for geomorphologists.
Study examines causes of earthquakes originating deep below earth’s surface.
The project aims to answer scientific questions about the formation and modification of the oceanic crust and shallow mantle using drill core from the Oman ophiolite.
Investigating the interactions between active tectonics and landscape evolution.
This project is funded by NERC facilities grant and the Geological Society of London.
Learn more about the projectA collaborative research effort aiming to understand the formation and development of the Moroccan Central High Atlas Mountains.
Project MAREST (MARine Ecosystem Stability and Turnover) aims to investigate the long-term response of shallow-water marine communities to past sea-level and climate changes. By integrating sequence stratigraphy and palaeoecology (stratigraphic palaeobiology) with geochemical analytical methods, the faunal and environmental changes of the Jurassic Sundance Seaway (western United States) can be reconstructed.
Examines the Sahara Desert climate-related erosion of volcanic island landscapes using alluvial fan and river terrace landforms.
Despite the intensive study of Cretaceous marine temperatures using a variety of techniques, an equator–to-pole temperature profile for the Cretaceous greenhouse world remains poorly constrained.