{"title":"澳大利亚新南威尔士州蓝山石英砂岩中的铁泉、环境变化、加速风化和洞穴发育:初步研究","authors":"Jill Rowling","doi":"10.12657/landfana-043-001","DOIUrl":null,"url":null,"abstract":"After a series of extreme weather events (drought, bushfires and floods), iron flocs were seen at ephemeral springs in quartz sandstone in the Blue Mountains National Park, New South Wales, Australia. Naturally burnt areas allowed better viewing of small sandstone caves. This paper discusses some of the processes operating within the quartz sandstone, leading to the attractive and unusual shapes, and how extreme weather led to the mobilisation and redeposition of iron minerals.","PeriodicalId":30719,"journal":{"name":"Landform Analysis","volume":"52 8","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2024-04-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Iron springs, environmental changes, accelerated weathering and cave development in quartz sandstone in the Blue Mountains, New South Wales, Australia: preliminary studies\",\"authors\":\"Jill Rowling\",\"doi\":\"10.12657/landfana-043-001\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"After a series of extreme weather events (drought, bushfires and floods), iron flocs were seen at ephemeral springs in quartz sandstone in the Blue Mountains National Park, New South Wales, Australia. Naturally burnt areas allowed better viewing of small sandstone caves. This paper discusses some of the processes operating within the quartz sandstone, leading to the attractive and unusual shapes, and how extreme weather led to the mobilisation and redeposition of iron minerals.\",\"PeriodicalId\":30719,\"journal\":{\"name\":\"Landform Analysis\",\"volume\":\"52 8\",\"pages\":\"\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2024-04-05\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Landform Analysis\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.12657/landfana-043-001\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Landform Analysis","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.12657/landfana-043-001","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Iron springs, environmental changes, accelerated weathering and cave development in quartz sandstone in the Blue Mountains, New South Wales, Australia: preliminary studies
After a series of extreme weather events (drought, bushfires and floods), iron flocs were seen at ephemeral springs in quartz sandstone in the Blue Mountains National Park, New South Wales, Australia. Naturally burnt areas allowed better viewing of small sandstone caves. This paper discusses some of the processes operating within the quartz sandstone, leading to the attractive and unusual shapes, and how extreme weather led to the mobilisation and redeposition of iron minerals.