This study aims to identify potential geosites and show existing geosites in a young glacial landscape in northern Poland through a qualitative assessment of the local geoheritage. Three areas of diversified morphology and geology located within the extent of the last Scandinavian Ice Sheet have been selected as the research polygons: the north-eastern part of the Dobrzyń Lake District, the Lower Vistula Valley and the Kashubian Lake District. Three basic abiotic components of the environment have been analysed: geology, terrain relief and hydrology. This research is based on some specific materials including maps and photographs. Methodology of this research includes the inventory, characterization and assessment of selected areas. The final results are proposals for geosites of high educational value in each of the three investigated regions. For the north-eastern part of the Dobrzyń Lake District, the creation of a geopark has been proposed, and the geosites of the Lower Vistula Valley provide the potential for a geotourist footpath to be designed. The Kashubian Lake District is characterised by the occurrence of numerous glacial landforms and sediments as well as high denivelations and a concentration of erratic boulders. Therefore, this region also has the potential to be selected for valuable geosites and the designing of a geotourist footpath.

中文翻译：

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波兰北部冰河后地区的地质遗产—地质旅游的前景

本研究旨在通过对当地地质遗产的定性评估，确定潜在的地理位置，并在波兰北部年轻的冰川景观中显示现有的地理位置。选择了最后一个斯堪的纳维亚冰盖范围内的三个形态和地质分布多样的区域作为研究多边形：杜布赞湖区的东北部，维斯杜拉河下游谷和卡舒比亚湖区。已分析了环境的三个基本非生物成分：地质，地形起伏和水文学。这项研究基于一些特定的材料，包括地图和照片。这项研究的方法论包括对选定区域的清单，特征和评估。最终结果是在三个被调查地区中的每个地区都具有高教育价值的地理位置建议。对于多布赞湖区的东北部，已经提出了建立地质公园的建议，而下维斯杜拉河谷的地理位置为设计地质旅游者的行人路提供了潜力。卡舒边湖区的特征是出现了许多冰川地貌和沉积物，以及高密度化和不规则的巨石集中。因此，该地区也有可能被选为珍贵的地理位置和地质旅游人行道的设计。卡舒边湖区的特征是出现了许多冰川地貌和沉积物，以及高密度化和不规则的巨石集中。因此，该地区也有可能被选为珍贵的地理位置和地质旅游人行道的设计。卡舒边湖区的特征是出现了许多冰川地貌和沉积物，以及高密度化和不规则的巨石集中。因此，该地区也有可能被选为有价值的地理位置和地质旅游人行道的设计。