This education resource comprises earthquake images with background information and descriptions of each image - includes world plate boundaries and earthquake distribution, distribution of earthquakes in Australia and examples of earthquake events, Australia's Seismological Network that is managed by Geoscience Australia, how earthquakes are measured, a case study of Tennant Creek and a map indicating Australia's earthquake hazard. Suitable for primary level Years 5-6 and secondary level Years 7-12.

A comprehensive black and white teachers' guide reviews the history and development of the United Nation's Convention on the Law of the Sea and its application to Australian marine jurisdiction. Case studies on the North West Shelf, Antarctica and Orange Roughy are included. 108 page booklet with student activities and suggested answers. Suitable for secondary geography and science students Years 8-12.

Weathering, erosion and deposition are all around us. Without these processes we would not have our mountains, river valleys, sandy beaches or even the soil in which we grow our food. This booklet outlines the processes of weathering, erosion and deposition for the information of teachers and students. Inlcudes case studies about the formation of many Australian landforms such as Uluru, the Warrumbungles and the Bungle Bungles. The booklet also includes reproducible student activities that provide students with fun and easy ways to learn about the processes that shape the Earth. - 50 page booklet - 8 student activities - suggested answers A comprehensive resource to introduce your students to the concept of regolith, an important way of looking at, and mapping, the landscape. Suitable for primary Years 5-6 and secondary Years 7-12.

A booklet that explains scale, distances, directions, map projections, latitude and longitude, grid references, legends and contours. Utilises the Rockhampton 1:100,000 topographic map for examples. Student activities included.

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Did you know that landslides kill more people in Australia than earthquakes. Using these activities, encourage your students to understand landslide hazards and how to reduce their own risks. This education resource consists of: - 44 page booklet - 11 reproducible activitities - suggested answers Please note: this booklet does not contain teacher notes. Suitable for secondary levels 7-12

Part-page article on matters relating to Australian stratigraphy. This column discusses what constitutes a publication for the purpose of establishing and formalising stratigrphic units. ISSN: 0312 4711

Codes, guidelines, and standard practices for naming and describing Australian stratigraphic units have been discussed for more than 60 years since the Australian and New Zealand Association for the Advancement of Science (ANZAAS) set up a Research Committee on Stratigraphic Nomenclature in 1946. Like today's Australian Stratigraphy Commission, its aims were 'to encourage the orderly use of names and definitions for stratigraphic units'. .......

Kakadu and Nitmiluk (Katherine Gorge) National Parks are unique in Australia in terms of their diversity of geological, cultural and biological values. Both parks are renowned for sandstone plateaus with spectacular gorges and escarpments, and contain some of the oldest and finest collections of Aboriginal rock art in the world. The parks support a remarkable abundance and variety of plants and animals, many of them rare or not found anywhere else. Kakadu is also famous for its extensive wetlands and is one of the few World Heritage areas listed for both its natural and cultural values. This guidebook has been written by experts from the Australian Geological Survey Organisation, Northern Territory Geological Survey, Environment Australia, Parks Australia, and the Parks and Wildlife Commission of the Northern Territory. Written for the non-specialist, the guidebook provides a concise and authoritative account of the rocks, landforms, plants, animals, Aboriginal culture and exploration history of the Kakadu and Nitmiluk National Parks. There is also information on places to visit, walking trails, camping facilities, commercial tours and helpful hints on getting the most from your visit.

Moreton Bay (MB) is a large (~1800 square km), stressed (with recent outbreaks of the cyanobacteria Lyngbia majscula), sub-tropical estuary which receives urban and rural runoff from a large catchment. Silicon is an essential nutrient for diatomaceous phytoplankton growth in coastal ecosystems. BSi (biogenic silicon) in surface sediments, pore water DSi (dissolved silicate, SiO4--) and benthic DSi fluxes were used as tracers of the formation and degradation of organic matter (OM) in MB. This work has implications for N & P cycling, water quality and eutrophication. BSi, TOC (both up to 2 wt%), TN & TP and diatom sterol biomarkers were all highest in the muddy sediments of western MB that is ~65% of the bay's area. We found that diatoms dominated OM cycling in western MB, and the benthic DSi flux accounted for ~80% of the pelagic productivity. Our conceptual model is that diatoms being heavy (because of their Si content) sink rapidly to the sediments where their biomass-N (OM-N) was denitrified to N2 and lost to the atmosphere with an efficiency of about 50%. Approximately 60% of OM-P, subsequent to degradation, remained trapped within the sediment. Diatoms therefore are an important vector to repeatedly deliver river-borne N & P to their respective sinks. However, diatomaceous OM contributed only about 20% of the OM input to the marine sands of eastern MB, about 34% of the bay's area. The principal OM input to the sandy sediments was attributed to benthic photosynthesis and N-fixation with rates of N-fixation (estimated from pore water DIN gradients) at 1.5 - 3.5 mmol m-2d-1. OM was rapidly and efficiently degraded (principally by O2), with little net accumulation and burial in sediments. N was denitrified efficiently (~100%). DIP must have been recycled rapidly in the top few cm's of the sandy sediments to support N-fixation. A whole-bay silicate budget indicated that: 1. DSi fluxes through the western margin of MB were about 4- fold those in eastern MB. 2. Pelagic diatom productivity was supported (approximately) by the benthic fluxes of DSi. 3. The DSi inventory was recycled through diatomaceous phytoplankton in about 15 days. 4. The export of DSi to the sea was about the same as the combined terrestrial and small marine inputs.