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Tweed-Moreton

Tweed-Moreton is a science topic covered in the lgStudy science library. This page brings together a partial reference excerpt, illustrations, worked examples, real-world applications and a short study plan, so you can understand Tweed-Moreton rather than just read about it. In short: Tweed–Moreton, also known as the Central Eastern Shelf Transition, is a marine biogeographic region of eastern Australia. The region includes the coastal and estuarine waters from just north of the Baffle Creek estuary in Queensland to north of Nambucca Heads in New South Wales.

Tweed-Moreton — main illustration
Tweed-Moreton — illustration

Key takeaways

  • Tweed-Moreton belongs to science; place it in that map before memorising details.
  • Learn the definition first, then one example that makes the definition concrete.
  • Connect Tweed-Moreton to a quantity you can measure, compute or draw — that is where exam questions come from.
  • Reproduce the core statement of Tweed-Moreton from memory before moving on to harder problems.

Reference excerpt

Tweed–Moreton, also known as the Central Eastern Shelf Transition, is a marine biogeographic region of eastern Australia. The region includes the coastal and estuarine waters from just north of the Baffle Creek estuary in Queensland to north of Nambucca Heads in New South Wales. It extends from the shore to the edge of the narrow continental shelf, with an area of 46,484 km2. It is a transition zone between the tropical waters of the northeastern Australian coast (Northeast Shelf Province) and the warm temperate seas of the central eastern Australian coast (Manning-Hawkesbury or Central Eastern Shelf Province). It is defined as both a bioregional province and meso-scale bioregion in the Integrated Marine and Coastal Regionalisation of Australia (IMCRA). and as a marine ecoregion in the Marine Ecoregions of the World system developed by the World Wide Fund for Nature (WWF).

Oceanography Coastal ocean circulation is dominated by the main stream of the East Australian Current. It runs southwards parallel to the shore, moving tropical Coral Sea waters into the temperate continental shelf waters. Localised centres of upwelling occur during springtime on a 40-day cycle off Evans Head (29°17’S). When upwelling is active it increases nutrient levels five- to ten-fold over normal values. The region is characterised by extensive sandy beaches punctuated by rocky headlands. There are extensive coastal estuaries behind sand islands, and offshore barrier islands. Beaches and sediments are generally of terrestrial origin. Tides range from 1 to 3 metres. Typical wave breaker heights are between 1.4 and 3.0 metres. Wave energy generally peaks in July, with a secondary peak during February in the New South Wales (southern) section.

Ecology Tweed–Moreton is near the southern limit of hard corals, with 60 coral genera in the north and fewer than 50 in the south. Sandstone outcrops form the substrate for reef faunas. These include the offshore Flinders Reef and fringing reefs at Hervey Bay. The New South Wales portion has two distinctive species assemblages of temperate reef fishes, echinoderms, and gastropods, and a single distinctive species assemblage of hermatypic corals and bivalves. The region has a distinctive assemblage of algal species. There is a significant difference in occurrences of seagrass species from north to south along the coast. The offshore benthic fauna is not well known. Low closed to open mangrove forest communities are found along sheltered coasts and rivers. There are eight mangrove tree species and three mangrove understorey species in the Queensland portion, along with 14 species of saltmarsh plants. Mangrove development and species diversity is lower in the New South Wales portion.

Protected areas Protected marine areas include Great Sandy Biosphere Reserve, Moreton Bay Marine Park, Cape Byron Marine Park, Richmond River Nature Reserve, and Solitary Islands Marine Park.

References

Illustrations

Tweed-Moreton: location of the Tweed–Moreton marine ecoregion
location of the Tweed–Moreton marine ecoregion

Worked examples

Example 1 — a first encounter with Tweed-Moreton

Start with the simplest possible case. Write down what Tweed-Moreton claims or describes in one sentence, then invent the smallest concrete situation in which that sentence is true. In science, the smallest case is usually a single object, a single equation or a single measurement. Check that every symbol or term in your sentence has a meaning in that case.

Example 2 — changing one variable

Take the situation from Example 1 and change exactly one quantity: double it, halve it, or set it to zero. Predict what should happen to Tweed-Moreton before you calculate. Comparing your prediction with the result is the fastest way to find out whether you understand the idea or only the words.

Example 3 — an exam-style question

Typical questions about Tweed-Moreton ask you to (a) state it precisely, (b) apply it to given data, and (c) explain a limitation. Practise writing all three answers in under five minutes; the third part is what separates a full-mark answer from an average one.

Applications of Tweed-Moreton

In research
Tweed-Moreton appears in science research whenever the underlying quantities have to be modelled precisely. Papers usually cite it as a starting assumption and then explore where it breaks down.
In technology and industry
Engineering practice reuses Tweed-Moreton in design rules, simulations and safety margins. Knowing the idea lets you read a specification sheet and understand why the numbers look the way they do.
In the classroom
Tweed-Moreton is common in secondary-school and first-year university syllabi. It links to neighbouring topics Biogeography of New South Wales, Biogeography of Queensland, Ecoregions of Australia, so understanding it makes those chapters shorter.
In everyday life
Look for Tweed-Moreton outside the textbook — in sport, cooking, traffic, electronics or the sky above you. An example you found yourself is remembered far longer than one you were given.
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How to study Tweed-Moreton in 20 minutes

  1. Read the reference excerpt below once, without taking notes.
  2. Close the page and write down what Tweed-Moreton means in your own words.
  3. Compare your version with the excerpt and mark what you missed.
  4. Work through the three examples above with pen and paper.
  5. Explain Tweed-Moreton out loud to somebody else — or to Teacher Smith in the lgStudy chat.

Frequently asked questions

What is Tweed-Moreton in simple terms?

Tweed–Moreton, also known as the Central Eastern Shelf Transition, is a marine biogeographic region of eastern Australia. The region includes the coastal and estuarine waters from just north of the Baffle Creek estuary in Queensland to north of Nambucca Heads in New South Wales.

Why does Tweed-Moreton matter?

Because it connects several science ideas at once: it gives you a definition you can apply, a quantity you can calculate, and a way to check whether a result is plausible.

How should I study Tweed-Moreton?

Read the excerpt, restate it from memory, then work through the examples and applications listed on this page. The five-step study plan above takes about twenty minutes.

What does this page cover?

It gives you a compact reference excerpt plus original lgStudy explanations, examples, applications and study material on Tweed-Moreton.

Tags

  • Biogeography of New South Wales
  • Biogeography of Queensland
  • Ecoregions of Australia
  • IMCRA meso-scale bioregions
  • IMCRA provincial bioregions
  • Marine ecoregions
  • Temperate Australasia

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