Difficulty: Easy
Correct Answer: Silica, giving rise to the term sial
Explanation:
Introduction / Context:
Geographers and earth scientists often describe the structure of the Earth crust using simple compositional models. The continental crust, or continental mass, is described as being rich in silica and alumina, which together are sometimes abbreviated as sial. The oceanic crust, in contrast, is richer in silica and magnesium, abbreviated as sima. This question asks you to recall the main mineral constituents of the continental mass and identify the oxide that is paired with alumina in this description.
Given Data / Assumptions:
Concept / Approach:
The upper part of the continental crust is dominated by rocks rich in silica (silicon dioxide) and alumina (aluminium oxide). The term sial comes from combining the symbols of silicon and aluminium, representing these dominant elements. These rocks are generally light in colour and low in density compared with the denser basaltic rocks of the oceanic crust. Iron oxide is more closely associated with the denser sima layer and with mafic rocks. Water and oxygen are important in other contexts but do not form the main solid mineral framework of the continental mass. Therefore, silica is the correct component that, together with alumina, characterises the continental crust.
Step-by-Step Solution:
Step 1: Recall that the continental crust is often described as sial because it is rich in silica and alumina.
Step 2: Identify silica as silicon dioxide, represented by the element silicon in the abbreviation sial.
Step 3: Recognise that alumina stands for aluminium oxide, and together these oxides form the basis of many continental crust rocks.
Step 4: Note that iron oxide is significant in denser rocks and the oceanic crust, usually referred to as sima, rich in silica and magnesium.
Step 5: Understand that water and free oxygen, although important, are not described as the main mineral constituents of the solid continental mass.
Step 6: Conclude that silica is the oxide paired with alumina and select it as the correct answer.
Verification / Alternative check:
Geography and geology textbooks consistently describe the upper continental crust as being composed mainly of granitic and related rocks, which are rich in silica and alumina. The term sial is used to refer to this silica and aluminium rich composition. In contrast, the oceanic crust is typically basaltic, with more magnesium and iron bearing minerals, grouped under sima. These descriptive models, though simplified, are standard in school level discussions and confirm that silica plus alumina are the key constituents of the continental mass.
Why Other Options Are Wrong:
Iron oxide is not the primary partner to alumina in defining the continental crust; instead it is more emphasised in descriptions of the denser sima layer and mafic rocks. Water, while present in pores and as groundwater, is not the main solid mineral constituent and therefore does not belong in this pair. Oxygen is a major element in the Earth crust but is typically considered as part of oxides such as silica and alumina rather than as a separate mineral constituent in this specific context. Thus, these options do not accurately describe the simplified composition model used in the question.
Common Pitfalls:
Students sometimes mix up sial and sima, confusing which combination of elements applies to continental versus oceanic crust. Another pitfall is to think of water as a main crust component because of oceans and groundwater, failing to distinguish between the solid crust and the hydrosphere. To avoid these errors, remember that sial stands for silica and alumina in the lighter continental crust, while sima refers to silica and magnesium in the denser oceanic crust. This simple mnemonic helps keep the compositional models clear for exam questions.
Final Answer:
The main mineral constituents of the continental mass are silica, giving rise to the term sial, and alumina.
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