The dimensions of geotourism with a spotlight on geodiversity in a subdued landscape

David Newsome, Philip Ladd
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引用次数: 3

Abstract

Landscapes of high relief are often favoured tourist destinations and at the same time display complex geomorphology that may be the result of diverse geology summarised into the concept of geodiversity. In contrast areas of subdued landscape, while topographically unappealing, may also be geodiverse but need careful explanation and promotion to attract the geotourist. The mid-west of Western Australia is an area of low relief with a long history of weathering, ostensibly of little interest to visitors, is underlain by a diverse geology that is displayed in an incised landscape where erosion by rivers and the ocean displays geodiversity in attractive detail. The mid-west of Western Australia is the result of sedimentary basin formation during the separation of the Gondwanan Indian plate from the western edge of the Archean Yilgarn granitic craton. A plutonic Precambrian basement is overlain by Ordovician sediments comprising the Tumblagooda sandstone and then Permian and younger Mesozoic rocks, often capped with a complex weathered regolith. Geology is exposed in the Murchison and Irwin River valleys where interpretive signs explain the origin of the landscape and sequences of rock. Extensive weathering products from the Tertiary period, such as laterite and sandplains, provide opportunities to explain processes such as deep weathering, mobilisation and re-deposition of sediments that are integral to the development of landscapes in general. We thus provide a conceptual understanding of the nexus between tourism and geodiversity via the applied science of geotourism in a predominantly subdued landscape. We make the point that there is a general lack of attention paid to regolith in the geotourism literature, hence we have provided a relatively detailed account of a large expanse of sandplain that occurs in the study area. Furthermore, regolith geodiversity has not been investigated in the context of its wider geotourism potential and while this case study is preliminary in its wider scope, we provide a platform for further research.

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地质旅游的维度,聚焦于柔和景观中的地质多样性
高浮雕景观往往是受欢迎的旅游目的地,同时也显示出复杂的地貌,这可能是地质多样性的结果,概括为地质多样性的概念。相比之下,那些地势较低的地区,虽然地形不吸引人,但也可能具有地质多样性,但需要仔细的解释和宣传,以吸引地质旅游者。西澳大利亚的中西部是一个有着悠久风化历史的低起伏地区,表面上游客对它不感兴趣,但它的基础是一个多样化的地质,在河流和海洋的侵蚀下,它在一个迷人的细节上展示了地质多样性。西澳大利亚中西部是冈瓦南印度板块与太古宙伊尔冈花岗岩克拉通西缘分离过程中沉积盆地形成的结果。深成型前寒武纪基底被奥陶系沉积物覆盖,这些沉积物包括翻滚古达砂岩,然后是二叠纪和更年轻的中生代岩石,通常被复杂的风化层覆盖。默奇森和埃尔文河谷的地质情况是显而易见的,在那里,解释性的标志解释了景观的起源和岩石的序列。第三纪的大量风化产物,如红土和沙平原,为解释深层风化、沉积物的动员和再沉积等过程提供了机会,这些过程对景观的发展是不可或缺的。因此,我们提供了一个概念性的理解旅游和地质多样性之间的联系,通过应用科学的地质旅游在一个主要是柔和的景观。我们指出,在地质旅游文献中普遍缺乏对风化层的关注,因此我们提供了一个相对详细的研究区域内大片沙平原的描述。此外,风化层地质多样性还没有在其更广泛的地质旅游潜力的背景下进行调查,虽然这个案例研究是初步的,在更广泛的范围内,我们为进一步的研究提供了一个平台。
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来源期刊
International Journal of Geoheritage and Parks
International Journal of Geoheritage and Parks Social Sciences-Urban Studies
CiteScore
6.70
自引率
0.00%
发文量
43
审稿时长
72 days
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