闵园景区面积约６km2。这是一个融自然景观与人文景观为一体的综合型游览区。山庄田园秀美，环境清幽，四季凉爽，空气新鲜，是疗养、度假和读书著作的佳境。景点有龙溪、怪石、竹海、凤凰古松、华严洞和20余座民居式尼庵。
Minyuan Scenic Area with an area of 6 km2 is a comprehensive tourist district where integrates natural landscapes with cultural landscapes. The idyllic scenery can be enjoyed: a fresh and beautiful countryside picture of villages, farming lands, hills, plant vegetation, quiet environment, cool four seasons, and fresh air. It is a good place for health, holiday and reading books. The attractions are Dragon Stream, peculiar stones, sea of bamboos, old phoenix pine, Huayan Cave and over 20 residential-styled nunneries.
天台景区面积约８km2，是九华山地质公园海拔最高的游览区。景区内十王峰为九华山海拔最高的山峰(1344.4m)，天台寺是九华山海拔最高的寺庙(1248m)。天台象形石群(观音石、大鹏听经石、金龟朝北斗、蜡烛峰等)、天台寺庙群(吊桥寺、观音寺、古拜经台、地藏禅林等)和天台摩崖石刻群，构成九华山地质地貌景观与人文景观融合的核心展示区。
Tiantai Scenic Area is the highest tourism area with an area of 8 km2 in Jiuhuashan Geopark. In this scenic area, Shiwang Peak is highest mountain with an altitude of 1344.4 m in Jiuhuashan, and the highest temple is Tiantai Temple with an altitude of 1248 m. The core exhibition area of the integration of geology, geomorphology and culture in Jiuhuashan is composed of three parts, namely, grotesquely-shaped rock group (Kwan-yin Stone, Roc hearing sutras Stone, Golden turtle facing the North Star, Candle Peak, etc.), temple group (Diaoqiao Temple, Kwan-yin Temple, Ancient Baijingtai, Dizang Temple, etc.) and cliff carving group.
九华山地区地壳基底形成于8亿年前；在2.5亿年前，相对稳定的地块隆升成陆；约1.4亿年前因板块碰撞，出现了两期大规模的岩浆入侵活动，形成东亚地区最大的花岗岩岩体，这是稳定地块活化的表现；6500万年前以来，受喜马拉雅造山运动影响，九华山大断裂塑造出壮观的花岗岩断块地貌；数千万年的流水、冰川和构造作用塑造了完整的“峰丘盆”地貌和丰富多彩的生物多样性景观。 The crust basement of Jiuhuashan was formed 800 million years ago. The stable platform uplifted to land 250 million years ago. The intense crustal activity happened with two stages of magmatism in Jiuhuashan area 140 million years ago, and the largest granite rock body in the East Asian was formed, which is sign of the stable continent reactivation. Because of Himalayan movement, Jiuhuashan Grand Fault made splendid fault-block mountains since the 65 million years ago. The complete geomorphologic pattern of mountain-hill-basin and abundant biodiversity were created because of tens of millions of years function of flowing water and glacier and structural activities.
地质遗迹是在地球历史演变过程中，由于内外动力地质作用，形成的地貌景观、地层剖面、地质构造、矿物、岩石、水体景观等遗迹。地质遗迹构成地质公园的主体。 九华山地质公园地质遗迹主要有地质剖面、地质构造、地貌景观与水体景观4大类。
Geosites, such as geomorphologic landscape, stratigraphic profiles, geological structures, minerals, rocks, water landscapes and so on, were formed by internal and external geological agents and witness the historical evolution of the Earth. The geosites in Jiuhuashan Geopark are classified into four categories: geological profile, geological structure, geomorphic landscape and water landscape.