Notice: JavaScript is not enabled. Please enable JavaScript to view this site.
Skip to main content
Open Announcement
Facebook
Instagram
X
Contact Us
中文
Share To
WeChat
Facebook
X
Weibo
LinkedIn
Email
Threads
Line
Whatsapp
Copy Link
Open Search Area
News & Events
Events
Past Events
Plan Your Visit
Hours, Admission & Direction
360º Virtual Tour
Online Booking System for Guided Tours
Education
Dynamic Earth
Earth Evolution
Reconstruct Geological History
The present is the key to the past
Relative Age
Index Fossils
Absolute Age
Solar System Formation
Solar System Formation
Meteorites
Our Unique Earth
Habitable Earth
Archean
Origin of the Earth's Crust
Origin of the Continents
The Oldest Rock from China
The Earliest Atmosphere & Hydrosphere
The Earliest Life on Earth
Proterozoic
The Onset of Plate Tectonics
Extensive Carbonate Platforms
Stromatolites
Dawn of Multicellular Life
Early Paleozoic
Early Paleozoic Sea
Early Paleozoic Geosphere
Early Paleozoic Climate
Early Paleozoic Biosphere
Late Paleozoic
Late Paleozoic Geosphere
Oxygen of the Atmosphere
Life moves onto Land
Diversification of early seedless vascular plants
Diversification of early seed vascular plants
Diversification of Marine Life
Mesozoic
The Breakup of Supercontinent Pangea
The Age of Reptiles
Dinosaur World
Cenozoic
Shaping the Present
Continents in Collision
Earth Materials
Minerals
Minerals Properties
Minerals Color
Variation of Quartz
Mineral Pseudomorphs
Mineral Uses
Rocks
Out of Solution
Volcanic Products
Rock Cycle
Geological History of Hong Kong
Minerals
Rocks and Fossils
Structures
Museum Collections
Minerals
Native Elements
Sulphides & Sulphosalts
Oxides & Hydroxides
Carbonates
Halides
Nitrates & Borates
Sulphates, Molybdates & Tungstates
Phosphates, Arsenates & Vanadates
Silicates
Nesosilicates
Sorosilicates
Cyclosilicates
Inosilicates
Phyllosilicates
Tectosilicates
Rocks
Igneous Rocks
Sedimentary Rocks
Biogenic Sedimentary Rocks
Clastic Sedimentary Rocks
Sedimentary Structures
Metamorphic Rocks
Fossils
Others
Loan Services
Support Us
Friends of Museum
Volunteer
Survey
About Us
Mission & Introduction
Dr. Stephen Hui
Museum Development
Our People
Register for Guided Tour
Register for Guided Tour
Open Announcement Section
Open Menu
Museum Location, Exhibition, Education, Collections, and more...
Search
Close Search Box
Close
Facebook
Instagram
X
中文
Share This Page To
WeChat
Facebook
X
Weibo
LinkedIn
Email
Threads
Line
Whatsapp
Copy Link
Open Search Box
News & Events
Events
Past Events
Plan Your Visit
Hours, Admission & Direction
360º Virtual Tour
Online Booking System for Guided Tours
Education
Dynamic Earth
Earth Evolution
Reconstruct Geological History
The present is the key to the past
Relative Age
Index Fossils
Absolute Age
Solar System Formation
Solar System Formation
Meteorites
Our Unique Earth
Habitable Earth
Archean
Origin of the Earth's Crust
Origin of the Continents
The Oldest Rock from China
The Earliest Atmosphere & Hydrosphere
The Earliest Life on Earth
Proterozoic
The Onset of Plate Tectonics
Extensive Carbonate Platforms
Stromatolites
Dawn of Multicellular Life
Early Paleozoic
Early Paleozoic Sea
Early Paleozoic Geosphere
Early Paleozoic Climate
Early Paleozoic Biosphere
Late Paleozoic
Late Paleozoic Geosphere
Oxygen of the Atmosphere
Life moves onto Land
Diversification of early seedless vascular plants
Diversification of early seed vascular plants
Diversification of Marine Life
Mesozoic
The Breakup of Supercontinent Pangea
The Age of Reptiles
Dinosaur World
Cenozoic
Shaping the Present
Continents in Collision
Earth Materials
Minerals
Minerals Properties
Minerals Color
Variation of Quartz
Mineral Pseudomorphs
Mineral Uses
Rocks
Out of Solution
Volcanic Products
Rock Cycle
Geological History of Hong Kong
Minerals
Rocks and Fossils
Structures
Museum Collections
Minerals
Native Elements
Sulphides & Sulphosalts
Oxides & Hydroxides
Carbonates
Halides
Nitrates & Borates
Sulphates, Molybdates & Tungstates
Phosphates, Arsenates & Vanadates
Silicates
Nesosilicates
Sorosilicates
Cyclosilicates
Inosilicates
Phyllosilicates
Tectosilicates
Rocks
Igneous Rocks
Sedimentary Rocks
Biogenic Sedimentary Rocks
Clastic Sedimentary Rocks
Sedimentary Structures
Metamorphic Rocks
Fossils
Others
Loan Services
Support Us
Friends of Museum
Volunteer
Survey
About Us
Mission & Introduction
Dr. Stephen Hui
Museum Development
Our People
Home
Education
Geological History of Hong Kong
Minerals
Minerals
Explore More
Education
Dynamic Earth
Earth Evolution
Reconstruct Geological History
The present is the key to the past
Relative Age
Index Fossils
Absolute Age
Solar System Formation
Solar System Formation
Meteorites
Our Unique Earth
Habitable Earth
Archean
Origin of the Earth's Crust
Origin of the Continents
The Oldest Rock from China
The Earliest Atmosphere & Hydrosphere
The Earliest Life on Earth
Proterozoic
The Onset of Plate Tectonics
Extensive Carbonate Platforms
Stromatolites
Dawn of Multicellular Life
Early Paleozoic
Early Paleozoic Sea
Early Paleozoic Geosphere
Early Paleozoic Climate
Early Paleozoic Biosphere
Late Paleozoic
Late Paleozoic Geosphere
Oxygen of the Atmosphere
Life moves onto Land
Diversification of early seedless vascular plants
Diversification of early seed vascular plants
Diversification of Marine Life
Mesozoic
The Breakup of Supercontinent Pangea
The Age of Reptiles
Dinosaur World
Cenozoic
Shaping the Present
Continents in Collision
Earth Materials
Minerals
Minerals Properties
Minerals Color
Variation of Quartz
Mineral Pseudomorphs
Mineral Uses
Rocks
Out of Solution
Volcanic Products
Rock Cycle
Geological History of Hong Kong
Minerals
Rocks and Fossils
Structures
Home
Education
Geological History of Hong Kong
Minerals
Coming Soon…