1. Clay mineral type Kaolinite have Gibbsite: Silicate mineral structure of .d.1:2a.1:12. Laterites soils isb.2:1c.2:2C. sandb. Transported3. Glaciers or their meltwaters transported sediment such asa. Residuald. None of themа. Tillb. waterc. Alluviumd. Non of them4. The hydration processes of rocks can transform the Anhydrite (CaSO4) to.....a. Sodium chlorideb. Gypsumc. Potassium Carbonated. Clay Minerals.weathering is the activities of organisms, including plants, burrowing animals and humanc. Physical5.b. Biological6. Material moved downhill by gravity is called..b. Colluviuma. Chemicald. Non of thema. Alluviumc. glacial driftd. Loess...is solid with very high density materials with an average density 17 gm/cm³.c. Inner core7.a. Outer coreb. Manteld. Crest8. The outer solid earth envelope up to 100 km is called.....b. Atmospherea. Hydrospherec. Lithosphered. Biosphere9. Feldspar mineral is froma. Non Silicate10. Tetragonal System: It consists..Group.b. Clay mineralc. Silicated. Magmamutually perpendicular axes.с.4а. 2b.1d. 3

We are not supposed to answer more than 3 questions. Still, I am answering 5 questions. I hope they…

Clay mineral type Kaolinite have Gibbsite: Silicate mineral structure of a.1:1 b.2:1 с.2:2 d.1:2 Laterites soils is C. sand b. Transported Glaciers or their meltwaters transported sediment such as a. Residual d. None of them ...... а. Till b. water c. Alluvium d. Non of them The hydration processes of rocks can transform the Anhydrite (CASO4) to....... a. Sodium chloride b. Gypsum c. Potassium Carbonate d. Clay Minerals .weathering is the activities of organisms, including plants, burrowing animals and human c. Physical a. Chemical b. Biological d. Non of them

Clay mineral type Kaolinite have Gibbsite: Silicate mineral structure of a.1:1 b.2:1 с.2:2 d.1:2 Laterites soils is C. sand b. Transported Glaciers or their meltwaters transported sediment such as a. Residual d. None of them ...... а. Till b. water c. Alluvium d. Non of them The hydration processes of rocks can transform the Anhydrite (CASO4) to....... a. Sodium chloride b. Gypsum c. Potassium Carbonate d. Clay Minerals .weathering is the activities of organisms, including plants, burrowing animals and human c. Physical a. Chemical b. Biological d. Non of them

Structural Analysis

6th Edition

ISBN:9781337630931

Author:KASSIMALI, Aslam.

Publisher:KASSIMALI, Aslam.

Chapter2: Loads On Structures

Section: Chapter Questions

Problem 1P

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Concept explainers

Pricing Excavation and Backfill

Backfill, in construction, is the activity of returning the soil and gravel that are removed during building construction or using them again to toughen and support the foundation of the building or any other structural component.

Question

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1. Clay mineral type Kaolinite have Gibbsite: Silicate mineral structure of .
d.1:2
a.1:1
2. Laterites soils is
b.2:1
c.2:2
C. sand
b. Transported
3. Glaciers or their meltwaters transported sediment such as
a. Residual
d. None of them
а. Till
b. water
c. Alluvium
d. Non of them
4. The hydration processes of rocks can transform the Anhydrite (CaSO4) to.....
a. Sodium chloride
b. Gypsum
c. Potassium Carbonate
d. Clay Minerals
.weathering is the activities of organisms, including plants, burrowing animals and human
c. Physical
5.
b. Biological
6. Material moved downhill by gravity is called..
b. Colluvium
a. Chemical
d. Non of them
a. Alluvium
c. glacial drift
d. Loess
...is solid with very high density materials with an average density 17 gm/cm³.
c. Inner core
7.
a. Outer core
b. Mantel
d. Crest
8. The outer solid earth envelope up to 100 km is called.....
b. Atmosphere
a. Hydrosphere
c. Lithosphere
d. Biosphere
9. Feldspar mineral is from
a. Non Silicate
10. Tetragonal System: It consists
..Group.
b. Clay mineral
c. Silicate
d. Magma
mutually perpendicular axes.
с.4
а. 2
b.1
d. 3

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