Abstract Geomorphological diversity is part of geodiversity. Study and evaluation of geodiversity, including geomorphological diversity, is often conducted in uplands and mountains, despite the fact that lowland areas are of equal importance. This paper evaluates geomorphological diversity in a small area of the Polish Lowland, using a variety of methods that have been applied in recent times for evaluating geodiversity, and presents the results on maps. By comparing these maps and analyzing the correlation coefficients of the results obtained, it was possible to identify the two methods that were best suited to indicating areas with the greatest geomorphological diversity in the lowlands. These two methods are least affected by the choice of elementary fields and data classification methods applied. The study identified the two areas with the greatest relief diversity and showed that they distinctly differ from one another. They demonstrate the major influence of processes, not only on the topographic parameters and landform types, but above all on identifying and defining total geomorphological diversity. These methods, which can be used to identify the areas with the greatest total geomorphological diversity, could readily be used in applied studies relating to abiotic ecosystem services and landscape management.

中文翻译：

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波兰低地（托伦盆地和海乌姆诺湖区）地貌多样性评估方法的结果比较

摘要 地貌多样性是地貌多样性的一部分。尽管低地地区同样重要，但对包括地貌多样性在内的地质多样性的研究和评估通常在高地和山区进行。本文使用最近用于评估地质多样性的各种方法来评估波兰低地的一小块区域的地貌多样性，并在地图上呈现结果。通过比较这些地图并分析所得结果的相关系数，可以确定最适合指示低地地貌多样性最大区域的两种方法。这两种方法受基本字段的选择和应用的数据分类方法的影响最小。该研究确定了两个具有最大地形多样性的区域，并表明它们彼此明显不同。它们展示了过程的主要影响，不仅对地形参数和地貌类型，而且最重要的是对识别和定义总体地貌多样性的影响。这些方法可用于识别具有最大总地貌多样性的区域，可以很容易地用于与非生物生态系统服务和景观管理相关的应用研究。