Counting matching models…
A simple block model showing a normal fault. It has a removable core for stimulating additional discussions during the class. We use them in our GEOL101 labs and Geological Field Techniques classes. This is one of eight models used by…
A simple block model showing a reverse fault. It has a removable core for stimulating additional discussions during the class. We use them in our GEOL101 labs and Geological Field Techniques classes. This is one of eight models used by…
All geology photos need to have a scale. The model contains 1 cm square blocks inside a 1 mm wide frame. A circle with a 1 cm diameter is also included in the design. A keychain hole makes it easy to carry the scale. The front face of the…
A simple block model showing a plunging fold. This is one of eight models used by students during a GEOL 101 structural geology laboratory module. We also use them in our Geological Field Techniques class. These models would typically…
A simple block model showing a geological fold. Depending on how you hold it in your hand, you can show and antiform or a synform. It has a removable core for stimulating additional discussions during the class. We use them in our GEOL101…
Apparent dip is the inclination of geologic beds as seen from any vertical plane not perpendicular to the strike of the geologic beds. This block model shows an inclined marker bed appears on five different vertical faces that are not…
A geological unit with uniform thickness can have variable outcrop widths depending on the dip of the unit and the topography. This block model demonstrates these relationships. This block model shows the intersection of an inclined…
A simple geologic block model showing an inclined marker bed. The block contains two faces that are cut perpendicular to the strike of the marker bed. These are the surfaces on which true dip can be measured. Use this model together with…
When geological contacts cross valleys or hilltops, the contacts are bent. The direction and amount of bending depends on the slope of the valley and the dip of the contact. This is one of six models that demonstrate the “Rule of V's”.…
A simple block model showing inclined bedding. It has a removable core for stimulating additional discussions during the class. We use them in our GEOL101 labs and Geological Field Techniques classes. This is one of eight models used by…
When geological contacts cross valleys or hilltops, the contacts are bent. The direction and amount of bending depends on the slope of the valley and the dip of the contact. This is one of six models that demonstrate the “Rule of V's”.…
Visualizing the orientation of geological planes in the subsurface can be tricky for students as they are expected to extrapolate from one-dimensional data (e.g. borehole depths). We commonly use depth data from three boreholes to…
When geological contacts cross valleys or hilltops, the contacts are bent. The direction and amount of bending depends on the slope of the valley and the dip of the contact. This is one of six models that demonstrate the “Rule of V's”.…
A simple block model showing horizontal bedding. It has a removable core for stimulating additional discussions during the class. We use them in our GEOL101 labs and Geological Field Techniques classes. This is one of eight models used by…
A simple block model showing a dextral fault. It has a removable core for stimulating additional discussions during the class. We use them in our GEOL101 labs and Geological Field Techniques classes. This is one of eight models used by…
A simple block model showing a sinistral fault. It has a removable core for stimulating additional discussions during the class. We use them in our GEOL101 labs and Geological Field Techniques classes. This is one of eight models used by…
When geological contacts cross valleys or hilltops, the contacts are bent. The direction and amount of bending depends on the slope of the valley and the dip of the contact. This is one of six models that demonstrate the “Rule of V's”.…
When geological contacts cross valleys or hilltops, the contacts are bent. The direction and amount of bending depends on the slope of the valley and the dip of the contact. This is one of six models that demonstrate the “Rule of V's”.…
When geological contacts cross valleys or hilltops, the contacts are bent. The direction and amount of bending depends on the slope of the valley and the dip of the contact. This is one of six models that demonstrate the “Rule of V's”.…
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