Yok Re - North Georgia Realtor

03/17/2026

For those who are unfamiliar with GRAUPEL...

12/22/2025

That’s one way to get people’s attention. 👀🤣

11/17/2025

Good information on buying/running short term rentals in different markets.
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10/20/2025

#5 team in the world!!!
to be a part of The Short Term Shop

10/13/2025

Saw some pretty spectacular cabins today.

09/02/2025

I love Blue Ridge this time of year. 60 in the morning and 80s in the afternoon.

07/29/2025

05/11/2025

I was showing a house yesterday when the earthquake hit. First time I ever experienced it. My client was from California and he acted like it was nothing. It honestly scared the crap out of me. We were on the top floor master when it occurred. All hard floors. EVERYTHING shook. The TVs on the walls, the bed, the dressers, the pictures, bedside tables, everything. It felt like it lasted for 5 seconds, but it was probably less than 2. I thought the hot water heater or furnace had blown. Then it felt like an uneven load in the washing machine on spin cycle x1000. It even sounded like it.

The Southern Appalachian Seismic Zone (SASZ) is a region of relatively low to moderate earthquake activity in the southeastern United States, stretching through parts of eastern Tennessee, northern Georgia, northeastern Alabama, and western North Carolina. Here’s an explanation of the processes involved:

1. Tectonic Setting

The SASZ lies within the interior of the North American Plate, far from any active plate boundaries. Earthquakes here are classified as intraplate earthquakes—they occur within a tectonic plate rather than at its edges.

2. Ancient Geological Structures

The region is underlain by ancient faults and crustal weaknesses that date back hundreds of millions of years to the formation and breakup of supercontinents like Rodinia and Pangaea. These include:
• Thrust faults and folds from the Appalachian mountain-building (Alleghanian orogeny)
• Reactivated fault zones that can slip again under present-day stresses

3. Stress Accumulation and Release

Although not near an active plate boundary, the North American Plate is subject to compressive forces due to:
• Seafloor spreading in the Atlantic
• Collisions along the western margin of the continent

These stresses accumulate in the crust and, over time, reactivate ancient faults. When the stress overcomes the frictional resistance along a fault, it is released as an earthquake.

4. Earthquake Characteristics
• Typically small to moderate in magnitude (usually < M5.0)
• Can still be felt over wide areas due to the dense, old crust of the eastern U.S., which transmits seismic waves efficiently
• Earthquakes are unpredictable and poorly understood, partly due to the complexity of buried structures

01/08/2025

Get ready!

11/11/2024

🇺🇸🇺🇸🇺🇸

10/25/2024

If you’re interested, let me know…

This 5338 square feet Single Family home has 4 bedrooms and 4 bathrooms. It is located at 498 Rock Creek Ct, Cherry Log, GA.