Xinglong town. In Xinglong Town, Wanning City, Xinglong Town is about 21 kilometers away from Wanning City. There are chicken coconut, coffee, Indonesian restaurants and other delicacies. There are so many hotels in the town that it is convenient to eat, live and play.

Huanke 1921 Boutique B&B is located at No.21 Zhongshan Road, Longhua District, Haikou City. The overall color is white, combined with Nanyang elements, giving off a strong Nanyang atmosphere. The owner has collected a large number of historical collections. There are cultural centers, bookstores and food streets around, so you can visit them anyway. It is also very pleasant to sit on the balcony and look at the starry sky at night and have a cup of coffee to talk about old things.

Wanning lives in Lantian Fishing Village with few good people and low prices. Lantian Fishing Village, located in Dong 'ao Town, Wanning City, Hainan Province, is a coastal village characterized by fishery production. Fishing village has the historical background of the revolutionary old Soviet area. In recent years, with convenient transportation and beautiful environment, it has given full play to its own resource advantages and vigorously developed rural tourism.

Geology:

The geological basement of Wanning City is composed of ancient sandstone-shale retrogressive rock series (slate, schist, phyllite and quartzite), Mesozoic magmatic rocks (granite and gabbro), coastal Quaternary loose layers and river alluvial strata. The parent rocks of western, southwestern mountainous areas and central hills and platforms are granite, and the low hilly platforms and coastal residual hills in the north are metamorphic rocks.

The west and southwest are located in the periphery of Qiongzhong granite mountain in Hainan Island, and the main structural direction of the Lower Paleozoic is northeast, which has been greatly subsided along this direction and deposited Cambrian Ordovician and Silurian strata. In the middle and late Caledonian movement, folds occurred, accompanied by large-scale acid magma intrusion.

due to metasomatism, mixed rock series (granite and gabbro) were formed, and other strata only appeared at the edge in the Lower Paleozoic. Due to the rising of the crust, the process of denudation is intensified, and the overlying strata are denuded completely, which makes the granite body enter the stage of geomorphic development.