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Soil and Landscape Grid National Soil Attribute Maps - Rock outcrop occurrence (3" resolution) - Release 1 

Ver: 1
Status of Data: completed
Update Frequency: notPlanned
Security Classification: unclassified
Record Last Modified: 2025-12-02
Viewed 58 times
Accessed 27 times
Dataset Created: 2019-09-01
Dataset Published: 2023-12-04
Data can be accessed from the following links:
HTTPPoint-of-truth metadata URLHTTPCloud Optimised GeoTIFF - Rock Outcrop Occurrence, Release 1WMSDES_rockoutcrop_N_P_AU_NAT_C_20190901HTTPLandscape Data Visualiser - Rock Outcrop Occurrence, Release 1HTTPro-crate-metadata.jsonHTTPFile Naming Conventions
How to cite this collection:
Malone, B. & Searle, R. (2023). Soil and Landscape Grid National Soil Attribute Maps - Rock outcrop occurrence (3" resolution) - Release 1. Version 1. Terrestrial Ecosystem Research Network. Dataset. https://dx.doi.org/10.25919/82gq-pf38 
The map gives a modelled estimate (probability) of the spatial distribution of rock outcroppings across Australia.

This product was produced in the development of the updated soil thickness map of Australia, details of which are published in Malone and Searle (2020; https://doi.org/10.1016/j.geoderma.2020.114579). This product is the output from Model 1 of aforementioned paper and uses the Rock Properties database provided by Geoscience Australia which gives the locations of sampled rock outcrops across Australia (http://www.ga.gov.au/scientific-topics/disciplines/geophysics/rock-properties). Filtering this dataset resulted in 14616 rock outcrop locations within areas where relief >300 m. A machine learning model was used to find relationships between observed data and associated environmental covariate data to inform the mapping of rock outcrop occurrence across Australia.

Detailed information about the Soil and Landscape Grid of Australia can be found at - SLGA

  • Attribute Definition: Probability of rock outcrops;
  • Units: 0-1;
  • Period (temporal coverage; approximately): 1950-2021;
  • Spatial resolution: 3 arc seconds (approx 90m);
  • Total number of gridded maps for this attribute: 1;
  • Number of pixels with coverage per layer: 2007M (49200 * 40800);
  • Data license : Creative Commons Attribution 4.0 (CC BY);
  • Target data standard: GlobalSoilMap specifications;
  • Format: Cloud Optimised GeoTIFF;
 
Credit
We at TERN acknowledge the Traditional Owners and Custodians throughout Australia, New Zealand and all nations. We honour their profound connections to land, water, biodiversity and culture and pay our respects to their Elders past, present and emerging. This work was jointly funded by CSIRO, Terrestrial Ecosystem Research Network (TERN) and the Australian Government through the National Collaborative Research Infrastructure Strategy (NCRIS).
We are grateful to the custodians of the soil site data in each state and territory for providing access to the soil site data, and all of the organisations listed as collaborating agencies for their significant contributions to the project and its outcomes. 
Purpose
The map gives a modelled estimate (probability) of the spatial distribution of rock outcroppings across Australia.
The aim is to operate an open national capability that provides access to verified, science-quality land surface dynamics data and soils information layers, plus high-end data analytics tools that integrated with other TERN observations can meet the needs of ecosystem researchers and actionable information for policy makers and natural resource managers. 
Lineage
The modelling and mapping of rock outcrop occurrence was performed as part of efforts to update and improve modelling of soil thickness across the Australia. Following is the description of method and further details of this work.

Rather than fitting a single model of soil thicknesses we went for a nuanced approach which entailed three separate models for:

Model 1. Predicting the occurrence of rock outcrops.
Model 2. Predicting the thickness of soils within the 0-2 m range
Model 3. Predicting the occurrence of deep soils (soils greater than 2 m thick).
Models 1 and 3 used the categorical model variant of the Ranger RF which was preceded by distinguishing; for Model 1, the observations that were deemed as rock outcrops from soils. And for Model 3, distinguishing soils that were less than 2 m thick (and not rock outcrops) from soils greater than 2 m thick. Ultimately both Models 1 and 3 were binary categorical models. 50 repeats of 5-fold CV (cross-validation) iterations of the Ranger RF model were run for each Model variant.

Model 2 used the regression form of the random forest model. After removing from the total data set the observations that were regarded as rock outcrops and soil greater than 2 m, there were 111,302 observations available. Of these, 67,698 had explicitly defined soil thickness values. The remaining 43,604 were right-censored data and were treated as follows. For each repeated 5-fold iteration, prior to splitting the data in calibration and validation datasets, values from a beta function were drawn at random of length 43,604. This value (between 0 and 1) was multiplied by the censored value soil thickness and then added to this same value, creating a simulated pseudo-soil thickness. Once the simulated data were combined with actual soil thickness data, the values were square-root transformed to approximate a normal distribution. Ranger RF modelling proceeded after optimising the Hyperparameter settings as described above for the categorical modelling. Like the categorical modelling, 50 repeated 5-fold CV iterations were computed.

All three model approaches were integrated via a simple ‘if-then’ pixel-based procedure. At each pixel, if Model 1 indicated the presence of rock outcrops 45 times or more out of 50 (90% of resampling iterations), the estimated soil thickness was estimated as rock outcrop, or effectively 0 cm. Similarly, for Model 3 which was the model based on prediction of deep soils (soils >2 m deep). In no situations did we encounter both Models 1 and 3 predict in the positive on 90% or more occasions simultaneously. If Model 1 or 3 did not predict in the positive in 90% of iterations, the prediction outputs of Model 2 were used.

After model integration, we derived a set of soil thickness exceedance probability mapping outputs. These were derived simply by assessing the empirical probabilities (at each pixel) and then tallying the number of occasions the estimated soil depth exceeded given threshold depths of 10 cm, 50 cm, 100 cm, and 150 cm. This tallied number was divided by 50 to give an exceedance probability for each threshold depth.

All processing for the generation of these products was undertaken using the R programming language (R Core Team, 2020).
  • Code - https://github.com/AusSoilsDSM/SLGA
  • Observation data - https://esoil.io/TERNLandscapes/Public/Pages/SoilDataFederator/SoilDataFederator.html
  • Covariate rasters - https://esoil.io/TERNLandscapes/Public/Pages/SLGA/GetData-COGSDataStore.html
 
Method DocumentationMethods Summary - Soil ThicknessR: A language and environment for statistical computing. R Foundation for Statistical Computing, Vienna, Austria.
Procedure StepsData not provided.
Australia
Temporal Coverage
From 1950-01-01 to 2020-01-01 
Spatial Resolution

Distance of 90 Meters

Vertical Extent

Data not provided.

ANZSRC - FOR
Agricultural land management
Agricultural spatial analysis and modelling
Pedology and pedometrics
Soil sciences
GCMD Sciences
LAND SURFACE - SOILS
SOLID EARTH - ROCKS/MINERALS/CRYSTALS
Horizontal Resolution
30 meters - < 100 meters
Parameters
rock outcrop
Temporal Resolution
Decadal
Topic
environment
geoscientificInformation
User Defined
3-dimensional soil mapping
Continental DSM
Digital Soil Mapping
Geology
Global Soil Map
Machine learning
Raster
Rock
SLGA
Soil Maps
Soil Thickness
Spatial modelling
TERN_Soils
TERN_Soils_DSM
Author
Malone, Brendan
Searle, Ross
Collaborator
Department of Environment, Water and Natural Resources (2012-2018), South Australian Government
Department of Land Resource Management (2012-2016), Northern Territory Government
Department of Primary Industries, Parks, Water and Environment, Tasmanian Government
Office of Environment and Heritage (2011-2019), New South Wales
University of Sydney
Geoscience Australia
Department of Science, Information Technology, Innovation and the Arts (2012-2015), Queensland Government
Terrestrial Ecosystem Research Network
Commonwealth Scientific and Industrial Research Organisation
Department of Environment and Primary Industries (2013-2015), Victorian Government
Department of Agriculture and Food (2006-2017), Western Australian Government
Contact Point
Malone, Brendan
Publisher
Terrestrial Ecosystem Research Network
Malone, B., & Searle, R. (2020). Improvements to the Australian national soil thickness map using an integrated data mining approach. Geoderma, 377, 114579. https://doi.org/10.1016/J.GEODERMA.2020.114579
Export to DCATExport to BibTeXExport to EndNote/Zotero
Terrestrial Ecosystem Research Network
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Creative Commons Attribution 4.0 International Licence
https://creativecommons.org/licenses/by/4.0/
TERN services are provided on an "as-is" and "as available" basis. Users use any TERN services at their discretion and risk. They will be solely responsible for any damage or loss whatsoever that results from such use including use of any data obtained through TERN and any analysis performed using the TERN infrastructure.
Web links to and from external, third party websites should not be construed as implying any relationships with and/or endorsement of the external site or its content by TERN.

Please advise any work or publications that use this data via the online form at https://www.tern.org.au/research-publications/#reporting 
Please cite this dataset as {Author} ({PublicationYear}). {Title}. {Version, as appropriate}. Terrestrial Ecosystem Research Network. Dataset. {Identifier}. 

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