Types of Chemical Weathering n 1 Spheroidal Weathering














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Types of Chemical Weathering n 1. Spheroidal Weathering球狀風化 n 2. Honeycomb Weathering蜂窩狀風化

1. Spheroidal Weathering What? n It is a type of chemical weathering caused by acidic rainwater

1. Spheroidal Weathering Where? n It is common in hot and humid areas. n It takes place in well-jointed and exposed rocks such as granite.

Photograph of Spheroidal Weathering in granite, Cheung Chau

1. Spheroidal Weathering How to form? n Rainwater absorbs carbon dioxide in the atmosphere and form a mild carbonic acid. n It falls on the ground and seeps into the joints of the rocks. n Chemical processes such as oxidation, hydration and solution occur. n These processes start on the land surface and along the joints and then work into the inner part.

1. Spheroidal Weathering n In time, large rectangular granite blocks are reduced to small and round boulders (corestones) and at last to fine weathered particles n When large part of weathered layers are removed by wind or rain, corestones are exposed on the ground and called tors

Corestones岩心 / Tors石塔 Photograph of corestones exposed in a bay northeast of Sham Chung

2. Honeycomb. Weathering What? n It is a type of chemical weathering caused by acidic rainwater and salt spray. n It is a kind of selective weathering選擇 性風化or differential weathering差別風 化

2. Honeycomb Weathering Where? n It is found in coastal area of Hong Kong. n It is common in rocks with minerals of different resistance.

Human Head Rock in Cheung Chau (an example of honeycomb weathering)

2. Honeycomb Weathering How to form? n Rocks contain minerals of differential resistance. n Less resistant minerals are easily weathered. (1) n Some minerals may react with sea water. n Sea water may act like sea spray. 海水噴灑

2. Honeycomb Weathering (2) n Rainwater absorbs carbon dioxide in the atmosphere and form a mild carbonic acid. n Rainwater react with some minerals e. g. feldspar / mica

Process of honeycomb weathering

2. Honeycomb Weathering n Selective weathering takes place. n The chemical processes of solution, oxidation, hydration and hydrolysis act on the rock surface. n The rock structure is weaken. n Some minerals e. g. feldspar are dissolved. n Holes, hollows / pits / cavities are left on the rock.