Classification
| Element |
Detail |
| Category |
Wave Mobilization (Hendrickson Method) |
| Subcategory |
Level II — deep/specific |
| FOMTRAC |
Supports PCs 3.2a-3.2n (integrated soft tissue approach), 3.2o (joint mobilization integration) |
| Fritz method |
Combination: compression + shaking (deep oscillation into specific structures) |
Purpose
- Release deep fascial restrictions and interfascicular torsion at the level of individual muscles and their investing fascia
- Integrate oscillating soft tissue work with MET and joint mobilization for comprehensive orthopedic treatment
- Address specific adhesions and fascial binding between deep tissue layers that Level I does not reach
- Reduce deep muscle hypertonicity through oscillation rather than sustained ischemic compression
Mechanism
Level II applies the same wave-generated oscillation as Level I but directs it into deeper tissue layers with more focused contact (thumbs, fingertips, forearm, or elbow). The deeper oscillation produces rhythmic shearing between the epimysium of individual muscles and the perimysium surrounding fascicles, addressing interfascicular torsion — the twisting and binding of fascial layers that occurs with chronic overuse, injury, or immobility. The oscillating force is more effective at separating adhered fascial planes than sustained static pressure because the rhythmic input continuously disrupts adhesive cross-links while simultaneously producing thixotropic ground substance changes. In the Hendrickson Method, Level II is not used in isolation — it integrates with MET (to neurologically release muscle holding patterns) and joint mobilization (to restore accessory joint movement), creating a synergistic treatment approach.
Indications
- Specific deep fascial restrictions identified during assessment or Level I treatment
- Chronic tendinopathy and tendon adhesions
- Deep muscle hypertonicity unresponsive to Swedish techniques
- Post-surgical adhesions (subacute and chronic stages)
- Orthopedic conditions requiring integrated soft tissue and joint mobilization
- Scar tissue remodeling at deep tissue levels
- Chronic myofascial pain with identified deep fascial restriction
Contraindications
- Acute inflammation in the target tissue
- Acute muscle tear or tendon rupture (deep oscillation stresses healing tissue)
- Anticoagulant therapy — modify depth; the focused pressure increases bruising risk
- Nerve entrapment in the target area — deep oscillation near compressed nerves may aggravate symptoms
- Malignancy in the treatment area
- Open wounds or skin infections over the treatment area
- Osteoporosis — use caution with deep pressure near fragile bone
Effects
Immediate:
- Separation of adhered fascial planes through rhythmic shearing
- Thixotropic changes in deep fascial ground substance
- Reduction in deep muscle hypertonicity via mechanoreceptor stimulation
- Improved inter-layer glide between deep fascial structures
- Traumatic hyperemia at the specific treatment site (similar to friction but distributed over a slightly larger area)
Cumulative (repeated application over sessions):
- Progressive release of deep fascial restrictions and scar tissue
- Restored glide between muscle compartments
- Improved joint mechanics when combined with joint mobilization
- Functional ROM gains that are maintained because both soft tissue and joint components are addressed simultaneously
Risks and Side Effects
- Post-treatment soreness (24-48 hours) — more common than with Level I due to deeper forces
- Bruising in clients on anticoagulants or with fragile vasculature
- Nerve irritation if applied directly over a nerve trunk without adequate anatomical awareness
- Temporary increase in symptoms before improvement (healing response)
Expected Outcomes
Short-term (immediate session): Palpable release of specific deep fascial restrictions. Improved ROM at the associated joint. Reduced deep muscle tenderness. Client reports feeling that a previously "stuck" area now moves more freely.
Medium-term (over 4-6 sessions): Progressive and sustained improvements in tissue mobility and joint ROM. Resolution or significant reduction of chronic adhesions and deep fascial restrictions. Functional improvement in activities limited by the restriction.
Execution
1. Begin with Level I in the target region to warm the superficial layer and reduce guarding (3-5 minutes).
2. Transition to Level II by narrowing your contact surface — move from full palm to thumbs, fingertips, forearm, or elbow as appropriate for the target structure.
3. Maintain the wave. The oscillation still originates from your lower body. The only change is the depth and specificity of contact — the rhythm and wave quality remain the same.
4. Sink into the target structure gradually over several oscillation cycles. Do not drive directly to depth — let the tissue invite you deeper as it releases.
5. Oscillate at the specific structure for 30-60 seconds, then assess for tissue change (softening, improved glide).
6. Integrate with MET: After releasing a fascial restriction, apply MET to the associated muscle to address any neurological holding pattern. Then return to Level II to further deepen the release.
7. Integrate with joint mobilization: After soft tissue and MET work, mobilize the associated joint to restore accessory movement. The sequence (Level II → MET → joint mobilization) addresses all three components of restriction: fascial, muscular, and articular.
8. Reassess ROM and tissue quality after the integrated sequence.
Lubricant: Minimal or none — deeper work requires better tissue coupling than lubricated surfaces provide.
Breathing: Instruct the client to exhale as you sink deeper. Coordinate depth with the exhalation phase.
Parameters
| Parameter |
Range |
Clinical Reasoning |
| Depth |
Moderate to deep (specific fascial layer / muscle) |
Targets deep fascia, epimysium, perimysium — structures Level I does not reach |
| Contact surface |
Thumbs, fingertips, forearm, elbow |
Narrower contact concentrates force into specific structures |
| Rate |
1-2 oscillations/sec |
Same as Level I — maintain the wave quality |
| Duration |
30-60 sec per specific site |
Sufficient for deep thixotropic and adhesion-breaking effects |
| Integration |
Combined with MET and joint mobilization |
The Hendrickson Method treats the full restriction pattern, not just one component |
Clinical Notes
- Common error: Losing the wave quality when going deeper. When therapists increase depth, they tend to abandon the oscillation and revert to sustained static pressure — at that point, it is no longer wave mobilization. Maintain the rhythm regardless of depth.
- Common error: Skipping Level I and going directly to Level II. The superficial layer must be released first — otherwise, the deeper oscillation cannot reach its target effectively, and the client's guarding will resist the deeper work.
- What to feel for: A distinct "unlocking" sensation as adhered fascial layers separate — the tissue suddenly becomes more mobile under your hands and the oscillation transmits more freely through the tissue.
- When to stop: If the client reports sharp or radiating pain (possible nerve involvement). If the tissue does not respond after 60 seconds of sustained oscillation (the restriction may be structural rather than fascial).
- Clinical pearl: The Level I → Level II → MET → joint mobilization integration sequence is the core of the Hendrickson Method and represents one of the most efficient treatment approaches in orthopedic massage. Each component builds on the previous — fascial release creates slack for MET, MET reduces muscle holding for joint mobilization, and joint mobilization restores the movement that maintains all the soft tissue gains. When you treat all three components in sequence, the results are greater and more lasting than treating any component in isolation.
Verbal Script
> "Now I'm going to work more specifically into the [muscle/structure] with the same oscillating technique but at a deeper level. You'll feel more focused pressure — it should be firm but not sharp. Let me know your comfort level. Breathe out as I work deeper."
Distinguishing Features
| Feature |
Wave Mobilization Level II |
Wave Mobilization Level I |
| Depth |
Moderate to deep (deep fascia, specific muscles) |
Superficial (skin and superficial fascia) |
| Contact surface |
Focused — thumbs, fingertips, forearm, elbow |
Broad — full palm |
| Target |
Specific structures (individual muscles, tendons, deep adhesions) |
General superficial fascial layer |
| Integration |
Combined with MET and joint mobilization |
Standalone or as preparation for Level II |
| Post-treatment soreness |
Likely (24-48 hours) |
Unlikely |
| Duration per site |
30-60 sec per specific structure |
3-5 min per broad region |
The key distinction: Level II is deeper, more specific, and integrates with MET and joint mobilization as part of a comprehensive orthopedic approach. Level I is superficial, broad, and primarily used for general fascial release and relaxation. Level I prepares the tissue for Level II.
Key Takeaways
- Level II applies the same wave-generated oscillation as Level I but at greater depth with more focused contact, targeting deep fascial restrictions and specific muscle adhesions
- Always begin with Level I to warm and release the superficial layer before progressing to Level II
- The Hendrickson Method integrates Level II with MET and joint mobilization in sequence — this combined approach addresses fascial, muscular, and articular components of restriction simultaneously
- Maintain the wave quality even at depth — if the oscillation stops and becomes sustained static pressure, it is no longer wave mobilization
- Distinguished from Level I by depth, specificity, and integration with other techniques